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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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GEOLOGIA E GEOMORFOLOGIA
1
Prof Fabiano Magdaleno
CEFET 2010
2) Composiccedilatildeo interna da Terra
1) Formaccedilatildeo da Terra
3) Agentes formadores do relevo
4) Estruturas geoloacutegicas
5) Feiccedilotildees do relevo brasileiro
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Formaccedilatildeo do planeta Terra
+ou- 46 bilhotildees de anos atraacutes
ldquoOrigem Quenterdquo
Nuvens de gasesquentes em rotaccedilatildeo que
foram se esfriando
ldquoOrigem por agregaccedilatildeordquo
Poeira coacutesmica se agregouaquecendo-se depois por meiode violentas reaccedilotildees quiacutemicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Composiccedilatildeo interna da Terra
CrostaDescontinuidade de Mohorovicic
Manto
Descontinuidade de Gutenberg
Nuacutecleo externoNuacutecleo interno
Correntes de Convecccedilatildeo
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Agentes formadores do relevo
Agentes internosTectonismo
Epirogecircnese
Orogecircnese
Abalos Siacutesmicos
Vulcanismo
Agentes externos
Intemperismo
Erosatildeo
PluvialFluvial
EoacutelicaMarinhaGlacial
Antroacutepica
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Estruturas Geoloacutegicas
1) Escudos Cristalinos ou CraacutetonsDobramentos antigos (do Preacute-Cambriano) que sofreram intensa e prolongada accedilatildeo
erosiva Satildeo estaacuteveis geologicamente e formados por rochas magmaacuteticas emetamoacuterficas Nessas aacutereas encontram-se os recursos minerais metaacutelicos (ouroprata alumiacutenio ferro etc)
2) Bacias Sedimentares
Satildeo aacutereas cocircncavas formadas por espessos pacotes de rochas sedimentares quechegam a ultrapassar 5000 m Nessas aacutereas encontram-se os minerais de origemfoacutessil (Carvatildeo mineral petroacuteleo diamante e xisto betuminoso)
3) Dobramentos Modernos
Dobras originadas do choque das placas tectocircnicas em periacuteodo geoloacutegico recenteCorrespondem aos terrenos mais elevados da superfiacutecie terrestre Possuem grandecomplexidade rochosa e estrutural geradas por efeitos de dobramentosacompanhados de intrusotildees vulcanismo abalos siacutesmicos e falhamentos Satildeoterrenos instaacuteveis As grandes cadeias orogeneacuteticas encontram-sepreferencialmente nas bordas dos continentes (Exemplos Cordilheira dos AndesHimalaia Rochosas etc) Natildeo existem no Brasil
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Escala Geoloacutegica do Tempo
Comparaccedilatildeo
Evoluccedilatildeoestrutural da
Terra
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Intemperismo
Processos naturais de desagregaccedilatildeo (fiacutesico) edecomposiccedilatildeo (quiacutemico) de rochas e solos preacute-existentes
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Agentes internos
bullTambeacutem chamados de agentes endoacutegenos satildeoresponsaacuteveis pela criaccedilatildeo do relevo (geram as
partes altas e baixas)bullOriginam-se da crosta da Terra ou do manto(camada localizada abaixo da crosta)
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Agentes externos
bullTambeacutem chamados de agentes exoacutegenosmodelam a superfiacutecie terrestre
bullAtuam a superfiacutecie terrestre
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Escala Richter
Criada pelo sismoacutelogo norte-americano Charles Francis Richter a escala para medir
a energia liberada pelos tremores de terra passou a ser usada em 1935 A escalaRichter varia de zero a 9 graus0 ndash Tremor equivalente ao choque produzido por um homem de estatura normal aosaltar de uma cadeira para o chatildeo1 ndash Tremor sentido apenas por instrumentos cientiacuteficos2 ndash Tremor sentido por algumas pessoas e animais
3 ndash Tremor sentido por muitas pessoas4 ndash Tremor sentido por todas as pessoas5 ndash Algumas construccedilotildees satildeo destruiacutedas6 ndash Estruturas balanccedilam e paredes caem7 ndash Construccedilotildees satildeo destruiacutedas e pessoas morrem
8 ndash Calamidade todas as construccedilotildees sofrem danos e muitas satildeo completamentedestruiacutedas9 ndash Cataacutestrofe as construccedilotildees satildeo completamente destruiacutedas como se arrasadas poruma bomba nuclear e haacute mudanccedila aparente na paisagem
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Terremotos ocorridos em 1999
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Orogecircnesebull Pressatildeo horizontal exercida pelas placas tectocircnicas que
origina dobras eou falhasbull Eacute um processo geologicamente raacutepido que causa grandes
deformaccedilotildees na Crosta
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Epirogecircnese
bull
Pressatildeo vertical exercida pelo magma como resposta aoaliacutevio de carga ou ao aumento de peso que geramovimento no sentido vertical (ascendente eoudescendente) de vastas aacutereas continentais sem perturbar
geologicamente a estrutura dos blocos afetadosbull Eacute um processo lento que natildeo gera deformaccedilotildees na crostabull Ex Fiordes na Escandinaacuteviabull Causam movimentos do niacutevel do mar que satildeo chamados
eustaacuteticos podendo ser do tipo transgressatildeo (avanccedilo domar sobre o continente) ou regressatildeo (recuo)
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bull Eacute a parte externa consolidada da Terra constituiacuteda de rochas
(agregados naturais de um ou mais minerais)bull Nas regiotildees continentais eacute formada por duas zonas a superior
denominada Sial (graccedilas agrave predominacircncia de rochas graniacuteticasricas em siliacutecio e alumiacutenio) e a zona inferior na qual se supotildee a
predominacircncia de siliacutecio e magneacutesio de onde vem o nome deSima
bull Sua espessura varia de 5 a 90 km
bull Estaacute dividida em vaacuterias partes chamadas Placas Tectocircnicas quese movimentam lateralmente independentes umas das outrasdevido as Correntes de Convecccedilatildeo
bull Estaacute equilibrada sobre o Manto segundo o princiacutepio da Isostasia
Crosta Terrestre
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Isostasia
bull Estado de equiliacutebrio dos
blocos continentais siaacutelicosque flutuam no substratomais denso do manto
bull Quanto mais alto for obloco maior seraacute a sua raiz
mergulhada
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Movimentaccedilatildeo das Placas Tectocircnicas
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Exemplos de Dobramentos Modernos
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Divergente
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bullTriacircngulo de Afar Eritreacuteia -Aacutefrica
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Tangencial ou transformante ou transcorrente
bull Falha de Santo Andreacute - EUA
bull A Placa do Pacifico tem se movido a uma velocidade meacutedia de 5 cmano
bull nos uacuteltimos 10 milhotildees de anos
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bull
Formaccedilatildeoda lha deSurtsey naIslacircndia em
1963
bullVulcanismo
bullRelevo formado por 6
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bullTimanfaya Lanzarote- Ilhas Canaacuterias
bull Relevo formado por 6
bull anos de erupccedilatildeo
F d d N h A i eacutel V l acirc i
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bullFernando de Noronha Arquipeacutelago Vulcacircnico
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A t aacuteli
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Austraacutelia
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Faleacutesia
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bullErosatildeo Diferencial
bullNiacuteveis com maior
cimentaccedilatildeo
bullShip Rock NovoMeacutexico antigo
cone vulcacircnico
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bull Milhotildees de anos de erosatildeo glacial e eoacutelica esculpiram
os profundos vales e os precipiacutecios
bull Badlands Dakota do Sul (EUA)
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bullSerra Pelada 1983
bullSerra Pelada atual
Placas Tectocircnicas
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Placas Tectocircnicas
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Ciclo das rochas
Rocha Magmaacutetica
Rocha Metamoacuterfica
Rocha Sedimentar
Magma
Erosatildeo e Sedimentaccedilatildeo
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Rochas Magmaacuteticas ou Iacutegneas
bullFormadas pelo resfriamento e solidificaccedilatildeo do magma dentro dacrosta terrestre em profundidade (intrusivas) ou em superfiacutecie(extrusiva)
bullExemplos Granito (intrusiva) Basalto (extrusiva) etc
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Derrame basaacuteltico em Torres- RS
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Rochas Sedimentares
bull Formada a partir de material originado da destruiccedilatildeo erosivade qualquer tipo de rocha material este que deveraacute sertransportado e depositado em um dos muitos ambientes de
sedimentaccedilatildeo da superfiacutecie terrestrebull Na maioria das vezes apresenta-se estratificada
bull Exemplos Argilito arenito siltitoetc
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Rochas Metamoacuterficas
bull Formadas por alteraccedilotildees nas antigas condiccedilotildees de
temperatura e pressatildeo das rochas magmaacuteticas ousedimentares que geram instabilidade dosminerais preacute-existentes
bull Dependendo do caso poderaacute ou natildeo mudar acomposiccedilatildeo mineraloacutegica mas a textura mudaobrigatoriamente
bull Exemplos Quartzito (derivada do metamorfismodo arenito) Maacutermore (proveacutem do Calcaacuterio ou doDolomito) Gnaisse (muito parecida com oGranito) etc
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Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
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Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
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Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
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Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
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Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
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Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
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Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
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Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
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Classificaccedilatildeo de Jurandyr Ross
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ldquoMares de morrosrdquo
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ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
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ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
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Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
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Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
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Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
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Co ve ge te
Formaccedilatildeo do petroacuteleo
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ccedil p
Formaccedilatildeo do carvatildeo mineral
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ccedil
Estaacutegios do carvatildeo mineral
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g
E t atilde d atilde i l P d atilde d atilde t l
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Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Formaccedilatildeo do planeta Terra
+ou- 46 bilhotildees de anos atraacutes
ldquoOrigem Quenterdquo
Nuvens de gasesquentes em rotaccedilatildeo que
foram se esfriando
ldquoOrigem por agregaccedilatildeordquo
Poeira coacutesmica se agregouaquecendo-se depois por meiode violentas reaccedilotildees quiacutemicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 371
Composiccedilatildeo interna da Terra
CrostaDescontinuidade de Mohorovicic
Manto
Descontinuidade de Gutenberg
Nuacutecleo externoNuacutecleo interno
Correntes de Convecccedilatildeo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Agentes formadores do relevo
Agentes internosTectonismo
Epirogecircnese
Orogecircnese
Abalos Siacutesmicos
Vulcanismo
Agentes externos
Intemperismo
Erosatildeo
PluvialFluvial
EoacutelicaMarinhaGlacial
Antroacutepica
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Estruturas Geoloacutegicas
1) Escudos Cristalinos ou CraacutetonsDobramentos antigos (do Preacute-Cambriano) que sofreram intensa e prolongada accedilatildeo
erosiva Satildeo estaacuteveis geologicamente e formados por rochas magmaacuteticas emetamoacuterficas Nessas aacutereas encontram-se os recursos minerais metaacutelicos (ouroprata alumiacutenio ferro etc)
2) Bacias Sedimentares
Satildeo aacutereas cocircncavas formadas por espessos pacotes de rochas sedimentares quechegam a ultrapassar 5000 m Nessas aacutereas encontram-se os minerais de origemfoacutessil (Carvatildeo mineral petroacuteleo diamante e xisto betuminoso)
3) Dobramentos Modernos
Dobras originadas do choque das placas tectocircnicas em periacuteodo geoloacutegico recenteCorrespondem aos terrenos mais elevados da superfiacutecie terrestre Possuem grandecomplexidade rochosa e estrutural geradas por efeitos de dobramentosacompanhados de intrusotildees vulcanismo abalos siacutesmicos e falhamentos Satildeoterrenos instaacuteveis As grandes cadeias orogeneacuteticas encontram-sepreferencialmente nas bordas dos continentes (Exemplos Cordilheira dos AndesHimalaia Rochosas etc) Natildeo existem no Brasil
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Escala Geoloacutegica do Tempo
Comparaccedilatildeo
Evoluccedilatildeoestrutural da
Terra
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Intemperismo
Processos naturais de desagregaccedilatildeo (fiacutesico) edecomposiccedilatildeo (quiacutemico) de rochas e solos preacute-existentes
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Agentes internos
bullTambeacutem chamados de agentes endoacutegenos satildeoresponsaacuteveis pela criaccedilatildeo do relevo (geram as
partes altas e baixas)bullOriginam-se da crosta da Terra ou do manto(camada localizada abaixo da crosta)
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Agentes externos
bullTambeacutem chamados de agentes exoacutegenosmodelam a superfiacutecie terrestre
bullAtuam a superfiacutecie terrestre
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Escala Richter
Criada pelo sismoacutelogo norte-americano Charles Francis Richter a escala para medir
a energia liberada pelos tremores de terra passou a ser usada em 1935 A escalaRichter varia de zero a 9 graus0 ndash Tremor equivalente ao choque produzido por um homem de estatura normal aosaltar de uma cadeira para o chatildeo1 ndash Tremor sentido apenas por instrumentos cientiacuteficos2 ndash Tremor sentido por algumas pessoas e animais
3 ndash Tremor sentido por muitas pessoas4 ndash Tremor sentido por todas as pessoas5 ndash Algumas construccedilotildees satildeo destruiacutedas6 ndash Estruturas balanccedilam e paredes caem7 ndash Construccedilotildees satildeo destruiacutedas e pessoas morrem
8 ndash Calamidade todas as construccedilotildees sofrem danos e muitas satildeo completamentedestruiacutedas9 ndash Cataacutestrofe as construccedilotildees satildeo completamente destruiacutedas como se arrasadas poruma bomba nuclear e haacute mudanccedila aparente na paisagem
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Terremotos ocorridos em 1999
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Orogecircnesebull Pressatildeo horizontal exercida pelas placas tectocircnicas que
origina dobras eou falhasbull Eacute um processo geologicamente raacutepido que causa grandes
deformaccedilotildees na Crosta
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Epirogecircnese
bull
Pressatildeo vertical exercida pelo magma como resposta aoaliacutevio de carga ou ao aumento de peso que geramovimento no sentido vertical (ascendente eoudescendente) de vastas aacutereas continentais sem perturbar
geologicamente a estrutura dos blocos afetadosbull Eacute um processo lento que natildeo gera deformaccedilotildees na crostabull Ex Fiordes na Escandinaacuteviabull Causam movimentos do niacutevel do mar que satildeo chamados
eustaacuteticos podendo ser do tipo transgressatildeo (avanccedilo domar sobre o continente) ou regressatildeo (recuo)
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bull Eacute a parte externa consolidada da Terra constituiacuteda de rochas
(agregados naturais de um ou mais minerais)bull Nas regiotildees continentais eacute formada por duas zonas a superior
denominada Sial (graccedilas agrave predominacircncia de rochas graniacuteticasricas em siliacutecio e alumiacutenio) e a zona inferior na qual se supotildee a
predominacircncia de siliacutecio e magneacutesio de onde vem o nome deSima
bull Sua espessura varia de 5 a 90 km
bull Estaacute dividida em vaacuterias partes chamadas Placas Tectocircnicas quese movimentam lateralmente independentes umas das outrasdevido as Correntes de Convecccedilatildeo
bull Estaacute equilibrada sobre o Manto segundo o princiacutepio da Isostasia
Crosta Terrestre
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Isostasia
bull Estado de equiliacutebrio dos
blocos continentais siaacutelicosque flutuam no substratomais denso do manto
bull Quanto mais alto for obloco maior seraacute a sua raiz
mergulhada
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Movimentaccedilatildeo das Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1971
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Exemplos de Dobramentos Modernos
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Divergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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bullTriacircngulo de Afar Eritreacuteia -Aacutefrica
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Tangencial ou transformante ou transcorrente
bull Falha de Santo Andreacute - EUA
bull A Placa do Pacifico tem se movido a uma velocidade meacutedia de 5 cmano
bull nos uacuteltimos 10 milhotildees de anos
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bull
Formaccedilatildeoda lha deSurtsey naIslacircndia em
1963
bullVulcanismo
bullRelevo formado por 6
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bullTimanfaya Lanzarote- Ilhas Canaacuterias
bull Relevo formado por 6
bull anos de erupccedilatildeo
F d d N h A i eacutel V l acirc i
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bullFernando de Noronha Arquipeacutelago Vulcacircnico
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A t aacuteli
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Austraacutelia
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Faleacutesia
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bullErosatildeo Diferencial
bullNiacuteveis com maior
cimentaccedilatildeo
bullShip Rock NovoMeacutexico antigo
cone vulcacircnico
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bull Milhotildees de anos de erosatildeo glacial e eoacutelica esculpiram
os profundos vales e os precipiacutecios
bull Badlands Dakota do Sul (EUA)
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bullSerra Pelada 1983
bullSerra Pelada atual
Placas Tectocircnicas
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Placas Tectocircnicas
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Ciclo das rochas
Rocha Magmaacutetica
Rocha Metamoacuterfica
Rocha Sedimentar
Magma
Erosatildeo e Sedimentaccedilatildeo
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Rochas Magmaacuteticas ou Iacutegneas
bullFormadas pelo resfriamento e solidificaccedilatildeo do magma dentro dacrosta terrestre em profundidade (intrusivas) ou em superfiacutecie(extrusiva)
bullExemplos Granito (intrusiva) Basalto (extrusiva) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Derrame basaacuteltico em Torres- RS
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Rochas Sedimentares
bull Formada a partir de material originado da destruiccedilatildeo erosivade qualquer tipo de rocha material este que deveraacute sertransportado e depositado em um dos muitos ambientes de
sedimentaccedilatildeo da superfiacutecie terrestrebull Na maioria das vezes apresenta-se estratificada
bull Exemplos Argilito arenito siltitoetc
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Rochas Metamoacuterficas
bull Formadas por alteraccedilotildees nas antigas condiccedilotildees de
temperatura e pressatildeo das rochas magmaacuteticas ousedimentares que geram instabilidade dosminerais preacute-existentes
bull Dependendo do caso poderaacute ou natildeo mudar acomposiccedilatildeo mineraloacutegica mas a textura mudaobrigatoriamente
bull Exemplos Quartzito (derivada do metamorfismodo arenito) Maacutermore (proveacutem do Calcaacuterio ou doDolomito) Gnaisse (muito parecida com oGranito) etc
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Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
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Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
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Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
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Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
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Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
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Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
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Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
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Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
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Classificaccedilatildeo de Jurandyr Ross
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ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
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ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
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Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Composiccedilatildeo interna da Terra
CrostaDescontinuidade de Mohorovicic
Manto
Descontinuidade de Gutenberg
Nuacutecleo externoNuacutecleo interno
Correntes de Convecccedilatildeo
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Agentes formadores do relevo
Agentes internosTectonismo
Epirogecircnese
Orogecircnese
Abalos Siacutesmicos
Vulcanismo
Agentes externos
Intemperismo
Erosatildeo
PluvialFluvial
EoacutelicaMarinhaGlacial
Antroacutepica
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Estruturas Geoloacutegicas
1) Escudos Cristalinos ou CraacutetonsDobramentos antigos (do Preacute-Cambriano) que sofreram intensa e prolongada accedilatildeo
erosiva Satildeo estaacuteveis geologicamente e formados por rochas magmaacuteticas emetamoacuterficas Nessas aacutereas encontram-se os recursos minerais metaacutelicos (ouroprata alumiacutenio ferro etc)
2) Bacias Sedimentares
Satildeo aacutereas cocircncavas formadas por espessos pacotes de rochas sedimentares quechegam a ultrapassar 5000 m Nessas aacutereas encontram-se os minerais de origemfoacutessil (Carvatildeo mineral petroacuteleo diamante e xisto betuminoso)
3) Dobramentos Modernos
Dobras originadas do choque das placas tectocircnicas em periacuteodo geoloacutegico recenteCorrespondem aos terrenos mais elevados da superfiacutecie terrestre Possuem grandecomplexidade rochosa e estrutural geradas por efeitos de dobramentosacompanhados de intrusotildees vulcanismo abalos siacutesmicos e falhamentos Satildeoterrenos instaacuteveis As grandes cadeias orogeneacuteticas encontram-sepreferencialmente nas bordas dos continentes (Exemplos Cordilheira dos AndesHimalaia Rochosas etc) Natildeo existem no Brasil
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Escala Geoloacutegica do Tempo
Comparaccedilatildeo
Evoluccedilatildeoestrutural da
Terra
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Intemperismo
Processos naturais de desagregaccedilatildeo (fiacutesico) edecomposiccedilatildeo (quiacutemico) de rochas e solos preacute-existentes
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Agentes internos
bullTambeacutem chamados de agentes endoacutegenos satildeoresponsaacuteveis pela criaccedilatildeo do relevo (geram as
partes altas e baixas)bullOriginam-se da crosta da Terra ou do manto(camada localizada abaixo da crosta)
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Agentes externos
bullTambeacutem chamados de agentes exoacutegenosmodelam a superfiacutecie terrestre
bullAtuam a superfiacutecie terrestre
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Escala Richter
Criada pelo sismoacutelogo norte-americano Charles Francis Richter a escala para medir
a energia liberada pelos tremores de terra passou a ser usada em 1935 A escalaRichter varia de zero a 9 graus0 ndash Tremor equivalente ao choque produzido por um homem de estatura normal aosaltar de uma cadeira para o chatildeo1 ndash Tremor sentido apenas por instrumentos cientiacuteficos2 ndash Tremor sentido por algumas pessoas e animais
3 ndash Tremor sentido por muitas pessoas4 ndash Tremor sentido por todas as pessoas5 ndash Algumas construccedilotildees satildeo destruiacutedas6 ndash Estruturas balanccedilam e paredes caem7 ndash Construccedilotildees satildeo destruiacutedas e pessoas morrem
8 ndash Calamidade todas as construccedilotildees sofrem danos e muitas satildeo completamentedestruiacutedas9 ndash Cataacutestrofe as construccedilotildees satildeo completamente destruiacutedas como se arrasadas poruma bomba nuclear e haacute mudanccedila aparente na paisagem
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Terremotos ocorridos em 1999
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Orogecircnesebull Pressatildeo horizontal exercida pelas placas tectocircnicas que
origina dobras eou falhasbull Eacute um processo geologicamente raacutepido que causa grandes
deformaccedilotildees na Crosta
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Epirogecircnese
bull
Pressatildeo vertical exercida pelo magma como resposta aoaliacutevio de carga ou ao aumento de peso que geramovimento no sentido vertical (ascendente eoudescendente) de vastas aacutereas continentais sem perturbar
geologicamente a estrutura dos blocos afetadosbull Eacute um processo lento que natildeo gera deformaccedilotildees na crostabull Ex Fiordes na Escandinaacuteviabull Causam movimentos do niacutevel do mar que satildeo chamados
eustaacuteticos podendo ser do tipo transgressatildeo (avanccedilo domar sobre o continente) ou regressatildeo (recuo)
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bull Eacute a parte externa consolidada da Terra constituiacuteda de rochas
(agregados naturais de um ou mais minerais)bull Nas regiotildees continentais eacute formada por duas zonas a superior
denominada Sial (graccedilas agrave predominacircncia de rochas graniacuteticasricas em siliacutecio e alumiacutenio) e a zona inferior na qual se supotildee a
predominacircncia de siliacutecio e magneacutesio de onde vem o nome deSima
bull Sua espessura varia de 5 a 90 km
bull Estaacute dividida em vaacuterias partes chamadas Placas Tectocircnicas quese movimentam lateralmente independentes umas das outrasdevido as Correntes de Convecccedilatildeo
bull Estaacute equilibrada sobre o Manto segundo o princiacutepio da Isostasia
Crosta Terrestre
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Isostasia
bull Estado de equiliacutebrio dos
blocos continentais siaacutelicosque flutuam no substratomais denso do manto
bull Quanto mais alto for obloco maior seraacute a sua raiz
mergulhada
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Movimentaccedilatildeo das Placas Tectocircnicas
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Exemplos de Dobramentos Modernos
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Divergente
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bullTriacircngulo de Afar Eritreacuteia -Aacutefrica
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Tangencial ou transformante ou transcorrente
bull Falha de Santo Andreacute - EUA
bull A Placa do Pacifico tem se movido a uma velocidade meacutedia de 5 cmano
bull nos uacuteltimos 10 milhotildees de anos
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bull
Formaccedilatildeoda lha deSurtsey naIslacircndia em
1963
bullVulcanismo
bullRelevo formado por 6
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bullTimanfaya Lanzarote- Ilhas Canaacuterias
bull Relevo formado por 6
bull anos de erupccedilatildeo
F d d N h A i eacutel V l acirc i
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bullFernando de Noronha Arquipeacutelago Vulcacircnico
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A t aacuteli
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Austraacutelia
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Faleacutesia
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bullErosatildeo Diferencial
bullNiacuteveis com maior
cimentaccedilatildeo
bullShip Rock NovoMeacutexico antigo
cone vulcacircnico
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bull Milhotildees de anos de erosatildeo glacial e eoacutelica esculpiram
os profundos vales e os precipiacutecios
bull Badlands Dakota do Sul (EUA)
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bullSerra Pelada 1983
bullSerra Pelada atual
Placas Tectocircnicas
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Placas Tectocircnicas
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Ciclo das rochas
Rocha Magmaacutetica
Rocha Metamoacuterfica
Rocha Sedimentar
Magma
Erosatildeo e Sedimentaccedilatildeo
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Rochas Magmaacuteticas ou Iacutegneas
bullFormadas pelo resfriamento e solidificaccedilatildeo do magma dentro dacrosta terrestre em profundidade (intrusivas) ou em superfiacutecie(extrusiva)
bullExemplos Granito (intrusiva) Basalto (extrusiva) etc
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Derrame basaacuteltico em Torres- RS
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Rochas Sedimentares
bull Formada a partir de material originado da destruiccedilatildeo erosivade qualquer tipo de rocha material este que deveraacute sertransportado e depositado em um dos muitos ambientes de
sedimentaccedilatildeo da superfiacutecie terrestrebull Na maioria das vezes apresenta-se estratificada
bull Exemplos Argilito arenito siltitoetc
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Rochas Metamoacuterficas
bull Formadas por alteraccedilotildees nas antigas condiccedilotildees de
temperatura e pressatildeo das rochas magmaacuteticas ousedimentares que geram instabilidade dosminerais preacute-existentes
bull Dependendo do caso poderaacute ou natildeo mudar acomposiccedilatildeo mineraloacutegica mas a textura mudaobrigatoriamente
bull Exemplos Quartzito (derivada do metamorfismodo arenito) Maacutermore (proveacutem do Calcaacuterio ou doDolomito) Gnaisse (muito parecida com oGranito) etc
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Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
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Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
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Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
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Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
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Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
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Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
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Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
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Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
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Classificaccedilatildeo de Jurandyr Ross
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ldquoMares de morrosrdquo
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ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
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ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
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Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
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Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
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httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
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Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
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Co ve ge te
Formaccedilatildeo do petroacuteleo
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ccedil p
Formaccedilatildeo do carvatildeo mineral
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ccedil
Estaacutegios do carvatildeo mineral
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g
E t atilde d atilde i l P d atilde d atilde t l
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Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
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Agentes formadores do relevo
Agentes internosTectonismo
Epirogecircnese
Orogecircnese
Abalos Siacutesmicos
Vulcanismo
Agentes externos
Intemperismo
Erosatildeo
PluvialFluvial
EoacutelicaMarinhaGlacial
Antroacutepica
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Estruturas Geoloacutegicas
1) Escudos Cristalinos ou CraacutetonsDobramentos antigos (do Preacute-Cambriano) que sofreram intensa e prolongada accedilatildeo
erosiva Satildeo estaacuteveis geologicamente e formados por rochas magmaacuteticas emetamoacuterficas Nessas aacutereas encontram-se os recursos minerais metaacutelicos (ouroprata alumiacutenio ferro etc)
2) Bacias Sedimentares
Satildeo aacutereas cocircncavas formadas por espessos pacotes de rochas sedimentares quechegam a ultrapassar 5000 m Nessas aacutereas encontram-se os minerais de origemfoacutessil (Carvatildeo mineral petroacuteleo diamante e xisto betuminoso)
3) Dobramentos Modernos
Dobras originadas do choque das placas tectocircnicas em periacuteodo geoloacutegico recenteCorrespondem aos terrenos mais elevados da superfiacutecie terrestre Possuem grandecomplexidade rochosa e estrutural geradas por efeitos de dobramentosacompanhados de intrusotildees vulcanismo abalos siacutesmicos e falhamentos Satildeoterrenos instaacuteveis As grandes cadeias orogeneacuteticas encontram-sepreferencialmente nas bordas dos continentes (Exemplos Cordilheira dos AndesHimalaia Rochosas etc) Natildeo existem no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Escala Geoloacutegica do Tempo
Comparaccedilatildeo
Evoluccedilatildeoestrutural da
Terra
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Intemperismo
Processos naturais de desagregaccedilatildeo (fiacutesico) edecomposiccedilatildeo (quiacutemico) de rochas e solos preacute-existentes
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Agentes internos
bullTambeacutem chamados de agentes endoacutegenos satildeoresponsaacuteveis pela criaccedilatildeo do relevo (geram as
partes altas e baixas)bullOriginam-se da crosta da Terra ou do manto(camada localizada abaixo da crosta)
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Agentes externos
bullTambeacutem chamados de agentes exoacutegenosmodelam a superfiacutecie terrestre
bullAtuam a superfiacutecie terrestre
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Escala Richter
Criada pelo sismoacutelogo norte-americano Charles Francis Richter a escala para medir
a energia liberada pelos tremores de terra passou a ser usada em 1935 A escalaRichter varia de zero a 9 graus0 ndash Tremor equivalente ao choque produzido por um homem de estatura normal aosaltar de uma cadeira para o chatildeo1 ndash Tremor sentido apenas por instrumentos cientiacuteficos2 ndash Tremor sentido por algumas pessoas e animais
3 ndash Tremor sentido por muitas pessoas4 ndash Tremor sentido por todas as pessoas5 ndash Algumas construccedilotildees satildeo destruiacutedas6 ndash Estruturas balanccedilam e paredes caem7 ndash Construccedilotildees satildeo destruiacutedas e pessoas morrem
8 ndash Calamidade todas as construccedilotildees sofrem danos e muitas satildeo completamentedestruiacutedas9 ndash Cataacutestrofe as construccedilotildees satildeo completamente destruiacutedas como se arrasadas poruma bomba nuclear e haacute mudanccedila aparente na paisagem
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Terremotos ocorridos em 1999
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Orogecircnesebull Pressatildeo horizontal exercida pelas placas tectocircnicas que
origina dobras eou falhasbull Eacute um processo geologicamente raacutepido que causa grandes
deformaccedilotildees na Crosta
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Epirogecircnese
bull
Pressatildeo vertical exercida pelo magma como resposta aoaliacutevio de carga ou ao aumento de peso que geramovimento no sentido vertical (ascendente eoudescendente) de vastas aacutereas continentais sem perturbar
geologicamente a estrutura dos blocos afetadosbull Eacute um processo lento que natildeo gera deformaccedilotildees na crostabull Ex Fiordes na Escandinaacuteviabull Causam movimentos do niacutevel do mar que satildeo chamados
eustaacuteticos podendo ser do tipo transgressatildeo (avanccedilo domar sobre o continente) ou regressatildeo (recuo)
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bull Eacute a parte externa consolidada da Terra constituiacuteda de rochas
(agregados naturais de um ou mais minerais)bull Nas regiotildees continentais eacute formada por duas zonas a superior
denominada Sial (graccedilas agrave predominacircncia de rochas graniacuteticasricas em siliacutecio e alumiacutenio) e a zona inferior na qual se supotildee a
predominacircncia de siliacutecio e magneacutesio de onde vem o nome deSima
bull Sua espessura varia de 5 a 90 km
bull Estaacute dividida em vaacuterias partes chamadas Placas Tectocircnicas quese movimentam lateralmente independentes umas das outrasdevido as Correntes de Convecccedilatildeo
bull Estaacute equilibrada sobre o Manto segundo o princiacutepio da Isostasia
Crosta Terrestre
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Isostasia
bull Estado de equiliacutebrio dos
blocos continentais siaacutelicosque flutuam no substratomais denso do manto
bull Quanto mais alto for obloco maior seraacute a sua raiz
mergulhada
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Movimentaccedilatildeo das Placas Tectocircnicas
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Exemplos de Dobramentos Modernos
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Divergente
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bullTriacircngulo de Afar Eritreacuteia -Aacutefrica
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Tangencial ou transformante ou transcorrente
bull Falha de Santo Andreacute - EUA
bull A Placa do Pacifico tem se movido a uma velocidade meacutedia de 5 cmano
bull nos uacuteltimos 10 milhotildees de anos
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bull
Formaccedilatildeoda lha deSurtsey naIslacircndia em
1963
bullVulcanismo
bullRelevo formado por 6
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bullTimanfaya Lanzarote- Ilhas Canaacuterias
bull Relevo formado por 6
bull anos de erupccedilatildeo
F d d N h A i eacutel V l acirc i
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bullFernando de Noronha Arquipeacutelago Vulcacircnico
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A t aacuteli
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Austraacutelia
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Faleacutesia
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bullErosatildeo Diferencial
bullNiacuteveis com maior
cimentaccedilatildeo
bullShip Rock NovoMeacutexico antigo
cone vulcacircnico
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bull Milhotildees de anos de erosatildeo glacial e eoacutelica esculpiram
os profundos vales e os precipiacutecios
bull Badlands Dakota do Sul (EUA)
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bullSerra Pelada 1983
bullSerra Pelada atual
Placas Tectocircnicas
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Placas Tectocircnicas
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Ciclo das rochas
Rocha Magmaacutetica
Rocha Metamoacuterfica
Rocha Sedimentar
Magma
Erosatildeo e Sedimentaccedilatildeo
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Rochas Magmaacuteticas ou Iacutegneas
bullFormadas pelo resfriamento e solidificaccedilatildeo do magma dentro dacrosta terrestre em profundidade (intrusivas) ou em superfiacutecie(extrusiva)
bullExemplos Granito (intrusiva) Basalto (extrusiva) etc
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Derrame basaacuteltico em Torres- RS
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Rochas Sedimentares
bull Formada a partir de material originado da destruiccedilatildeo erosivade qualquer tipo de rocha material este que deveraacute sertransportado e depositado em um dos muitos ambientes de
sedimentaccedilatildeo da superfiacutecie terrestrebull Na maioria das vezes apresenta-se estratificada
bull Exemplos Argilito arenito siltitoetc
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Rochas Metamoacuterficas
bull Formadas por alteraccedilotildees nas antigas condiccedilotildees de
temperatura e pressatildeo das rochas magmaacuteticas ousedimentares que geram instabilidade dosminerais preacute-existentes
bull Dependendo do caso poderaacute ou natildeo mudar acomposiccedilatildeo mineraloacutegica mas a textura mudaobrigatoriamente
bull Exemplos Quartzito (derivada do metamorfismodo arenito) Maacutermore (proveacutem do Calcaacuterio ou doDolomito) Gnaisse (muito parecida com oGranito) etc
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Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
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Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
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Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
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Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
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Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
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Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
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Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
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Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
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Classificaccedilatildeo de Jurandyr Ross
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ldquoMares de morrosrdquo
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ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
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ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
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Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
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Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
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Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
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Co ve ge te
Formaccedilatildeo do petroacuteleo
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ccedil p
Formaccedilatildeo do carvatildeo mineral
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ccedil
Estaacutegios do carvatildeo mineral
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g
E t atilde d atilde i l P d atilde d atilde t l
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Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
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Estruturas Geoloacutegicas
1) Escudos Cristalinos ou CraacutetonsDobramentos antigos (do Preacute-Cambriano) que sofreram intensa e prolongada accedilatildeo
erosiva Satildeo estaacuteveis geologicamente e formados por rochas magmaacuteticas emetamoacuterficas Nessas aacutereas encontram-se os recursos minerais metaacutelicos (ouroprata alumiacutenio ferro etc)
2) Bacias Sedimentares
Satildeo aacutereas cocircncavas formadas por espessos pacotes de rochas sedimentares quechegam a ultrapassar 5000 m Nessas aacutereas encontram-se os minerais de origemfoacutessil (Carvatildeo mineral petroacuteleo diamante e xisto betuminoso)
3) Dobramentos Modernos
Dobras originadas do choque das placas tectocircnicas em periacuteodo geoloacutegico recenteCorrespondem aos terrenos mais elevados da superfiacutecie terrestre Possuem grandecomplexidade rochosa e estrutural geradas por efeitos de dobramentosacompanhados de intrusotildees vulcanismo abalos siacutesmicos e falhamentos Satildeoterrenos instaacuteveis As grandes cadeias orogeneacuteticas encontram-sepreferencialmente nas bordas dos continentes (Exemplos Cordilheira dos AndesHimalaia Rochosas etc) Natildeo existem no Brasil
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Escala Geoloacutegica do Tempo
Comparaccedilatildeo
Evoluccedilatildeoestrutural da
Terra
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Intemperismo
Processos naturais de desagregaccedilatildeo (fiacutesico) edecomposiccedilatildeo (quiacutemico) de rochas e solos preacute-existentes
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Agentes internos
bullTambeacutem chamados de agentes endoacutegenos satildeoresponsaacuteveis pela criaccedilatildeo do relevo (geram as
partes altas e baixas)bullOriginam-se da crosta da Terra ou do manto(camada localizada abaixo da crosta)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Agentes externos
bullTambeacutem chamados de agentes exoacutegenosmodelam a superfiacutecie terrestre
bullAtuam a superfiacutecie terrestre
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1271
Escala Richter
Criada pelo sismoacutelogo norte-americano Charles Francis Richter a escala para medir
a energia liberada pelos tremores de terra passou a ser usada em 1935 A escalaRichter varia de zero a 9 graus0 ndash Tremor equivalente ao choque produzido por um homem de estatura normal aosaltar de uma cadeira para o chatildeo1 ndash Tremor sentido apenas por instrumentos cientiacuteficos2 ndash Tremor sentido por algumas pessoas e animais
3 ndash Tremor sentido por muitas pessoas4 ndash Tremor sentido por todas as pessoas5 ndash Algumas construccedilotildees satildeo destruiacutedas6 ndash Estruturas balanccedilam e paredes caem7 ndash Construccedilotildees satildeo destruiacutedas e pessoas morrem
8 ndash Calamidade todas as construccedilotildees sofrem danos e muitas satildeo completamentedestruiacutedas9 ndash Cataacutestrofe as construccedilotildees satildeo completamente destruiacutedas como se arrasadas poruma bomba nuclear e haacute mudanccedila aparente na paisagem
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1371
Terremotos ocorridos em 1999
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Orogecircnesebull Pressatildeo horizontal exercida pelas placas tectocircnicas que
origina dobras eou falhasbull Eacute um processo geologicamente raacutepido que causa grandes
deformaccedilotildees na Crosta
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httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1571
Epirogecircnese
bull
Pressatildeo vertical exercida pelo magma como resposta aoaliacutevio de carga ou ao aumento de peso que geramovimento no sentido vertical (ascendente eoudescendente) de vastas aacutereas continentais sem perturbar
geologicamente a estrutura dos blocos afetadosbull Eacute um processo lento que natildeo gera deformaccedilotildees na crostabull Ex Fiordes na Escandinaacuteviabull Causam movimentos do niacutevel do mar que satildeo chamados
eustaacuteticos podendo ser do tipo transgressatildeo (avanccedilo domar sobre o continente) ou regressatildeo (recuo)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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bull Eacute a parte externa consolidada da Terra constituiacuteda de rochas
(agregados naturais de um ou mais minerais)bull Nas regiotildees continentais eacute formada por duas zonas a superior
denominada Sial (graccedilas agrave predominacircncia de rochas graniacuteticasricas em siliacutecio e alumiacutenio) e a zona inferior na qual se supotildee a
predominacircncia de siliacutecio e magneacutesio de onde vem o nome deSima
bull Sua espessura varia de 5 a 90 km
bull Estaacute dividida em vaacuterias partes chamadas Placas Tectocircnicas quese movimentam lateralmente independentes umas das outrasdevido as Correntes de Convecccedilatildeo
bull Estaacute equilibrada sobre o Manto segundo o princiacutepio da Isostasia
Crosta Terrestre
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Isostasia
bull Estado de equiliacutebrio dos
blocos continentais siaacutelicosque flutuam no substratomais denso do manto
bull Quanto mais alto for obloco maior seraacute a sua raiz
mergulhada
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Movimentaccedilatildeo das Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1971
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Exemplos de Dobramentos Modernos
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Divergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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bullTriacircngulo de Afar Eritreacuteia -Aacutefrica
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Tangencial ou transformante ou transcorrente
bull Falha de Santo Andreacute - EUA
bull A Placa do Pacifico tem se movido a uma velocidade meacutedia de 5 cmano
bull nos uacuteltimos 10 milhotildees de anos
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bull
Formaccedilatildeoda lha deSurtsey naIslacircndia em
1963
bullVulcanismo
bullRelevo formado por 6
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bullTimanfaya Lanzarote- Ilhas Canaacuterias
bull Relevo formado por 6
bull anos de erupccedilatildeo
F d d N h A i eacutel V l acirc i
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bullFernando de Noronha Arquipeacutelago Vulcacircnico
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A t aacuteli
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Austraacutelia
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Faleacutesia
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bullErosatildeo Diferencial
bullNiacuteveis com maior
cimentaccedilatildeo
bullShip Rock NovoMeacutexico antigo
cone vulcacircnico
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bull Milhotildees de anos de erosatildeo glacial e eoacutelica esculpiram
os profundos vales e os precipiacutecios
bull Badlands Dakota do Sul (EUA)
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bullSerra Pelada 1983
bullSerra Pelada atual
Placas Tectocircnicas
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Placas Tectocircnicas
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Ciclo das rochas
Rocha Magmaacutetica
Rocha Metamoacuterfica
Rocha Sedimentar
Magma
Erosatildeo e Sedimentaccedilatildeo
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Rochas Magmaacuteticas ou Iacutegneas
bullFormadas pelo resfriamento e solidificaccedilatildeo do magma dentro dacrosta terrestre em profundidade (intrusivas) ou em superfiacutecie(extrusiva)
bullExemplos Granito (intrusiva) Basalto (extrusiva) etc
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Derrame basaacuteltico em Torres- RS
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Rochas Sedimentares
bull Formada a partir de material originado da destruiccedilatildeo erosivade qualquer tipo de rocha material este que deveraacute sertransportado e depositado em um dos muitos ambientes de
sedimentaccedilatildeo da superfiacutecie terrestrebull Na maioria das vezes apresenta-se estratificada
bull Exemplos Argilito arenito siltitoetc
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httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4171
Rochas Metamoacuterficas
bull Formadas por alteraccedilotildees nas antigas condiccedilotildees de
temperatura e pressatildeo das rochas magmaacuteticas ousedimentares que geram instabilidade dosminerais preacute-existentes
bull Dependendo do caso poderaacute ou natildeo mudar acomposiccedilatildeo mineraloacutegica mas a textura mudaobrigatoriamente
bull Exemplos Quartzito (derivada do metamorfismodo arenito) Maacutermore (proveacutem do Calcaacuterio ou doDolomito) Gnaisse (muito parecida com oGranito) etc
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Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
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Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
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Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
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Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
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Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
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Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
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Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
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Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
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Classificaccedilatildeo de Jurandyr Ross
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ldquoMares de morrosrdquo
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ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
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ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
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Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
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Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
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Co ve ge te
Formaccedilatildeo do petroacuteleo
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ccedil p
Formaccedilatildeo do carvatildeo mineral
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ccedil
Estaacutegios do carvatildeo mineral
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g
E t atilde d atilde i l P d atilde d atilde t l
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Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
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Escala Geoloacutegica do Tempo
Comparaccedilatildeo
Evoluccedilatildeoestrutural da
Terra
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Intemperismo
Processos naturais de desagregaccedilatildeo (fiacutesico) edecomposiccedilatildeo (quiacutemico) de rochas e solos preacute-existentes
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Agentes internos
bullTambeacutem chamados de agentes endoacutegenos satildeoresponsaacuteveis pela criaccedilatildeo do relevo (geram as
partes altas e baixas)bullOriginam-se da crosta da Terra ou do manto(camada localizada abaixo da crosta)
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Agentes externos
bullTambeacutem chamados de agentes exoacutegenosmodelam a superfiacutecie terrestre
bullAtuam a superfiacutecie terrestre
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Escala Richter
Criada pelo sismoacutelogo norte-americano Charles Francis Richter a escala para medir
a energia liberada pelos tremores de terra passou a ser usada em 1935 A escalaRichter varia de zero a 9 graus0 ndash Tremor equivalente ao choque produzido por um homem de estatura normal aosaltar de uma cadeira para o chatildeo1 ndash Tremor sentido apenas por instrumentos cientiacuteficos2 ndash Tremor sentido por algumas pessoas e animais
3 ndash Tremor sentido por muitas pessoas4 ndash Tremor sentido por todas as pessoas5 ndash Algumas construccedilotildees satildeo destruiacutedas6 ndash Estruturas balanccedilam e paredes caem7 ndash Construccedilotildees satildeo destruiacutedas e pessoas morrem
8 ndash Calamidade todas as construccedilotildees sofrem danos e muitas satildeo completamentedestruiacutedas9 ndash Cataacutestrofe as construccedilotildees satildeo completamente destruiacutedas como se arrasadas poruma bomba nuclear e haacute mudanccedila aparente na paisagem
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Terremotos ocorridos em 1999
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Orogecircnesebull Pressatildeo horizontal exercida pelas placas tectocircnicas que
origina dobras eou falhasbull Eacute um processo geologicamente raacutepido que causa grandes
deformaccedilotildees na Crosta
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1571
Epirogecircnese
bull
Pressatildeo vertical exercida pelo magma como resposta aoaliacutevio de carga ou ao aumento de peso que geramovimento no sentido vertical (ascendente eoudescendente) de vastas aacutereas continentais sem perturbar
geologicamente a estrutura dos blocos afetadosbull Eacute um processo lento que natildeo gera deformaccedilotildees na crostabull Ex Fiordes na Escandinaacuteviabull Causam movimentos do niacutevel do mar que satildeo chamados
eustaacuteticos podendo ser do tipo transgressatildeo (avanccedilo domar sobre o continente) ou regressatildeo (recuo)
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httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1671
bull Eacute a parte externa consolidada da Terra constituiacuteda de rochas
(agregados naturais de um ou mais minerais)bull Nas regiotildees continentais eacute formada por duas zonas a superior
denominada Sial (graccedilas agrave predominacircncia de rochas graniacuteticasricas em siliacutecio e alumiacutenio) e a zona inferior na qual se supotildee a
predominacircncia de siliacutecio e magneacutesio de onde vem o nome deSima
bull Sua espessura varia de 5 a 90 km
bull Estaacute dividida em vaacuterias partes chamadas Placas Tectocircnicas quese movimentam lateralmente independentes umas das outrasdevido as Correntes de Convecccedilatildeo
bull Estaacute equilibrada sobre o Manto segundo o princiacutepio da Isostasia
Crosta Terrestre
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1771
Isostasia
bull Estado de equiliacutebrio dos
blocos continentais siaacutelicosque flutuam no substratomais denso do manto
bull Quanto mais alto for obloco maior seraacute a sua raiz
mergulhada
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1871
Movimentaccedilatildeo das Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2271
Exemplos de Dobramentos Modernos
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2371
Divergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2471
bullTriacircngulo de Afar Eritreacuteia -Aacutefrica
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httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2571
Tangencial ou transformante ou transcorrente
bull Falha de Santo Andreacute - EUA
bull A Placa do Pacifico tem se movido a uma velocidade meacutedia de 5 cmano
bull nos uacuteltimos 10 milhotildees de anos
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2671
bull
Formaccedilatildeoda lha deSurtsey naIslacircndia em
1963
bullVulcanismo
bullRelevo formado por 6
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httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2771
bullTimanfaya Lanzarote- Ilhas Canaacuterias
bull Relevo formado por 6
bull anos de erupccedilatildeo
F d d N h A i eacutel V l acirc i
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bullFernando de Noronha Arquipeacutelago Vulcacircnico
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A t aacuteli
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Austraacutelia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3171
Faleacutesia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3271
bullErosatildeo Diferencial
bullNiacuteveis com maior
cimentaccedilatildeo
bullShip Rock NovoMeacutexico antigo
cone vulcacircnico
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httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3371
bull Milhotildees de anos de erosatildeo glacial e eoacutelica esculpiram
os profundos vales e os precipiacutecios
bull Badlands Dakota do Sul (EUA)
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httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3471
bullSerra Pelada 1983
bullSerra Pelada atual
Placas Tectocircnicas
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Placas Tectocircnicas
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Ciclo das rochas
Rocha Magmaacutetica
Rocha Metamoacuterfica
Rocha Sedimentar
Magma
Erosatildeo e Sedimentaccedilatildeo
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httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3871
Rochas Magmaacuteticas ou Iacutegneas
bullFormadas pelo resfriamento e solidificaccedilatildeo do magma dentro dacrosta terrestre em profundidade (intrusivas) ou em superfiacutecie(extrusiva)
bullExemplos Granito (intrusiva) Basalto (extrusiva) etc
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httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3971
Derrame basaacuteltico em Torres- RS
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httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4071
Rochas Sedimentares
bull Formada a partir de material originado da destruiccedilatildeo erosivade qualquer tipo de rocha material este que deveraacute sertransportado e depositado em um dos muitos ambientes de
sedimentaccedilatildeo da superfiacutecie terrestrebull Na maioria das vezes apresenta-se estratificada
bull Exemplos Argilito arenito siltitoetc
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httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4171
Rochas Metamoacuterficas
bull Formadas por alteraccedilotildees nas antigas condiccedilotildees de
temperatura e pressatildeo das rochas magmaacuteticas ousedimentares que geram instabilidade dosminerais preacute-existentes
bull Dependendo do caso poderaacute ou natildeo mudar acomposiccedilatildeo mineraloacutegica mas a textura mudaobrigatoriamente
bull Exemplos Quartzito (derivada do metamorfismodo arenito) Maacutermore (proveacutem do Calcaacuterio ou doDolomito) Gnaisse (muito parecida com oGranito) etc
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httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4271
Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
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Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
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Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
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Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
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Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
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Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
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httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
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Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
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Classificaccedilatildeo de Jurandyr Ross
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
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httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
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Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 771
Escala Geoloacutegica do Tempo
Comparaccedilatildeo
Evoluccedilatildeoestrutural da
Terra
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Intemperismo
Processos naturais de desagregaccedilatildeo (fiacutesico) edecomposiccedilatildeo (quiacutemico) de rochas e solos preacute-existentes
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Agentes internos
bullTambeacutem chamados de agentes endoacutegenos satildeoresponsaacuteveis pela criaccedilatildeo do relevo (geram as
partes altas e baixas)bullOriginam-se da crosta da Terra ou do manto(camada localizada abaixo da crosta)
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httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1171
Agentes externos
bullTambeacutem chamados de agentes exoacutegenosmodelam a superfiacutecie terrestre
bullAtuam a superfiacutecie terrestre
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httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1271
Escala Richter
Criada pelo sismoacutelogo norte-americano Charles Francis Richter a escala para medir
a energia liberada pelos tremores de terra passou a ser usada em 1935 A escalaRichter varia de zero a 9 graus0 ndash Tremor equivalente ao choque produzido por um homem de estatura normal aosaltar de uma cadeira para o chatildeo1 ndash Tremor sentido apenas por instrumentos cientiacuteficos2 ndash Tremor sentido por algumas pessoas e animais
3 ndash Tremor sentido por muitas pessoas4 ndash Tremor sentido por todas as pessoas5 ndash Algumas construccedilotildees satildeo destruiacutedas6 ndash Estruturas balanccedilam e paredes caem7 ndash Construccedilotildees satildeo destruiacutedas e pessoas morrem
8 ndash Calamidade todas as construccedilotildees sofrem danos e muitas satildeo completamentedestruiacutedas9 ndash Cataacutestrofe as construccedilotildees satildeo completamente destruiacutedas como se arrasadas poruma bomba nuclear e haacute mudanccedila aparente na paisagem
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Terremotos ocorridos em 1999
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Orogecircnesebull Pressatildeo horizontal exercida pelas placas tectocircnicas que
origina dobras eou falhasbull Eacute um processo geologicamente raacutepido que causa grandes
deformaccedilotildees na Crosta
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Epirogecircnese
bull
Pressatildeo vertical exercida pelo magma como resposta aoaliacutevio de carga ou ao aumento de peso que geramovimento no sentido vertical (ascendente eoudescendente) de vastas aacutereas continentais sem perturbar
geologicamente a estrutura dos blocos afetadosbull Eacute um processo lento que natildeo gera deformaccedilotildees na crostabull Ex Fiordes na Escandinaacuteviabull Causam movimentos do niacutevel do mar que satildeo chamados
eustaacuteticos podendo ser do tipo transgressatildeo (avanccedilo domar sobre o continente) ou regressatildeo (recuo)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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bull Eacute a parte externa consolidada da Terra constituiacuteda de rochas
(agregados naturais de um ou mais minerais)bull Nas regiotildees continentais eacute formada por duas zonas a superior
denominada Sial (graccedilas agrave predominacircncia de rochas graniacuteticasricas em siliacutecio e alumiacutenio) e a zona inferior na qual se supotildee a
predominacircncia de siliacutecio e magneacutesio de onde vem o nome deSima
bull Sua espessura varia de 5 a 90 km
bull Estaacute dividida em vaacuterias partes chamadas Placas Tectocircnicas quese movimentam lateralmente independentes umas das outrasdevido as Correntes de Convecccedilatildeo
bull Estaacute equilibrada sobre o Manto segundo o princiacutepio da Isostasia
Crosta Terrestre
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httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1771
Isostasia
bull Estado de equiliacutebrio dos
blocos continentais siaacutelicosque flutuam no substratomais denso do manto
bull Quanto mais alto for obloco maior seraacute a sua raiz
mergulhada
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Movimentaccedilatildeo das Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2271
Exemplos de Dobramentos Modernos
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2371
Divergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2471
bullTriacircngulo de Afar Eritreacuteia -Aacutefrica
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2571
Tangencial ou transformante ou transcorrente
bull Falha de Santo Andreacute - EUA
bull A Placa do Pacifico tem se movido a uma velocidade meacutedia de 5 cmano
bull nos uacuteltimos 10 milhotildees de anos
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2671
bull
Formaccedilatildeoda lha deSurtsey naIslacircndia em
1963
bullVulcanismo
bullRelevo formado por 6
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2771
bullTimanfaya Lanzarote- Ilhas Canaacuterias
bull Relevo formado por 6
bull anos de erupccedilatildeo
F d d N h A i eacutel V l acirc i
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2871
bullFernando de Noronha Arquipeacutelago Vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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A t aacuteli
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Austraacutelia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3171
Faleacutesia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3271
bullErosatildeo Diferencial
bullNiacuteveis com maior
cimentaccedilatildeo
bullShip Rock NovoMeacutexico antigo
cone vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3371
bull Milhotildees de anos de erosatildeo glacial e eoacutelica esculpiram
os profundos vales e os precipiacutecios
bull Badlands Dakota do Sul (EUA)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3471
bullSerra Pelada 1983
bullSerra Pelada atual
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3571
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Ciclo das rochas
Rocha Magmaacutetica
Rocha Metamoacuterfica
Rocha Sedimentar
Magma
Erosatildeo e Sedimentaccedilatildeo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3871
Rochas Magmaacuteticas ou Iacutegneas
bullFormadas pelo resfriamento e solidificaccedilatildeo do magma dentro dacrosta terrestre em profundidade (intrusivas) ou em superfiacutecie(extrusiva)
bullExemplos Granito (intrusiva) Basalto (extrusiva) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3971
Derrame basaacuteltico em Torres- RS
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4071
Rochas Sedimentares
bull Formada a partir de material originado da destruiccedilatildeo erosivade qualquer tipo de rocha material este que deveraacute sertransportado e depositado em um dos muitos ambientes de
sedimentaccedilatildeo da superfiacutecie terrestrebull Na maioria das vezes apresenta-se estratificada
bull Exemplos Argilito arenito siltitoetc
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httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4171
Rochas Metamoacuterficas
bull Formadas por alteraccedilotildees nas antigas condiccedilotildees de
temperatura e pressatildeo das rochas magmaacuteticas ousedimentares que geram instabilidade dosminerais preacute-existentes
bull Dependendo do caso poderaacute ou natildeo mudar acomposiccedilatildeo mineraloacutegica mas a textura mudaobrigatoriamente
bull Exemplos Quartzito (derivada do metamorfismodo arenito) Maacutermore (proveacutem do Calcaacuterio ou doDolomito) Gnaisse (muito parecida com oGranito) etc
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httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4271
Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
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Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
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httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4471
Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
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httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4571
Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
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httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4671
Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4771
Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4971
Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
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Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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g
E t atilde d atilde i l P d atilde d atilde t l
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Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Intemperismo
Processos naturais de desagregaccedilatildeo (fiacutesico) edecomposiccedilatildeo (quiacutemico) de rochas e solos preacute-existentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Agentes internos
bullTambeacutem chamados de agentes endoacutegenos satildeoresponsaacuteveis pela criaccedilatildeo do relevo (geram as
partes altas e baixas)bullOriginam-se da crosta da Terra ou do manto(camada localizada abaixo da crosta)
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httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1171
Agentes externos
bullTambeacutem chamados de agentes exoacutegenosmodelam a superfiacutecie terrestre
bullAtuam a superfiacutecie terrestre
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1271
Escala Richter
Criada pelo sismoacutelogo norte-americano Charles Francis Richter a escala para medir
a energia liberada pelos tremores de terra passou a ser usada em 1935 A escalaRichter varia de zero a 9 graus0 ndash Tremor equivalente ao choque produzido por um homem de estatura normal aosaltar de uma cadeira para o chatildeo1 ndash Tremor sentido apenas por instrumentos cientiacuteficos2 ndash Tremor sentido por algumas pessoas e animais
3 ndash Tremor sentido por muitas pessoas4 ndash Tremor sentido por todas as pessoas5 ndash Algumas construccedilotildees satildeo destruiacutedas6 ndash Estruturas balanccedilam e paredes caem7 ndash Construccedilotildees satildeo destruiacutedas e pessoas morrem
8 ndash Calamidade todas as construccedilotildees sofrem danos e muitas satildeo completamentedestruiacutedas9 ndash Cataacutestrofe as construccedilotildees satildeo completamente destruiacutedas como se arrasadas poruma bomba nuclear e haacute mudanccedila aparente na paisagem
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1371
Terremotos ocorridos em 1999
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Orogecircnesebull Pressatildeo horizontal exercida pelas placas tectocircnicas que
origina dobras eou falhasbull Eacute um processo geologicamente raacutepido que causa grandes
deformaccedilotildees na Crosta
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1571
Epirogecircnese
bull
Pressatildeo vertical exercida pelo magma como resposta aoaliacutevio de carga ou ao aumento de peso que geramovimento no sentido vertical (ascendente eoudescendente) de vastas aacutereas continentais sem perturbar
geologicamente a estrutura dos blocos afetadosbull Eacute um processo lento que natildeo gera deformaccedilotildees na crostabull Ex Fiordes na Escandinaacuteviabull Causam movimentos do niacutevel do mar que satildeo chamados
eustaacuteticos podendo ser do tipo transgressatildeo (avanccedilo domar sobre o continente) ou regressatildeo (recuo)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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bull Eacute a parte externa consolidada da Terra constituiacuteda de rochas
(agregados naturais de um ou mais minerais)bull Nas regiotildees continentais eacute formada por duas zonas a superior
denominada Sial (graccedilas agrave predominacircncia de rochas graniacuteticasricas em siliacutecio e alumiacutenio) e a zona inferior na qual se supotildee a
predominacircncia de siliacutecio e magneacutesio de onde vem o nome deSima
bull Sua espessura varia de 5 a 90 km
bull Estaacute dividida em vaacuterias partes chamadas Placas Tectocircnicas quese movimentam lateralmente independentes umas das outrasdevido as Correntes de Convecccedilatildeo
bull Estaacute equilibrada sobre o Manto segundo o princiacutepio da Isostasia
Crosta Terrestre
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Isostasia
bull Estado de equiliacutebrio dos
blocos continentais siaacutelicosque flutuam no substratomais denso do manto
bull Quanto mais alto for obloco maior seraacute a sua raiz
mergulhada
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Movimentaccedilatildeo das Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2271
Exemplos de Dobramentos Modernos
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Divergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2471
bullTriacircngulo de Afar Eritreacuteia -Aacutefrica
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2571
Tangencial ou transformante ou transcorrente
bull Falha de Santo Andreacute - EUA
bull A Placa do Pacifico tem se movido a uma velocidade meacutedia de 5 cmano
bull nos uacuteltimos 10 milhotildees de anos
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2671
bull
Formaccedilatildeoda lha deSurtsey naIslacircndia em
1963
bullVulcanismo
bullRelevo formado por 6
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2771
bullTimanfaya Lanzarote- Ilhas Canaacuterias
bull Relevo formado por 6
bull anos de erupccedilatildeo
F d d N h A i eacutel V l acirc i
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2871
bullFernando de Noronha Arquipeacutelago Vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2971
A t aacuteli
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3071
Austraacutelia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3171
Faleacutesia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3271
bullErosatildeo Diferencial
bullNiacuteveis com maior
cimentaccedilatildeo
bullShip Rock NovoMeacutexico antigo
cone vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3371
bull Milhotildees de anos de erosatildeo glacial e eoacutelica esculpiram
os profundos vales e os precipiacutecios
bull Badlands Dakota do Sul (EUA)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3471
bullSerra Pelada 1983
bullSerra Pelada atual
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3571
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3771
Ciclo das rochas
Rocha Magmaacutetica
Rocha Metamoacuterfica
Rocha Sedimentar
Magma
Erosatildeo e Sedimentaccedilatildeo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3871
Rochas Magmaacuteticas ou Iacutegneas
bullFormadas pelo resfriamento e solidificaccedilatildeo do magma dentro dacrosta terrestre em profundidade (intrusivas) ou em superfiacutecie(extrusiva)
bullExemplos Granito (intrusiva) Basalto (extrusiva) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3971
Derrame basaacuteltico em Torres- RS
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4071
Rochas Sedimentares
bull Formada a partir de material originado da destruiccedilatildeo erosivade qualquer tipo de rocha material este que deveraacute sertransportado e depositado em um dos muitos ambientes de
sedimentaccedilatildeo da superfiacutecie terrestrebull Na maioria das vezes apresenta-se estratificada
bull Exemplos Argilito arenito siltitoetc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4171
Rochas Metamoacuterficas
bull Formadas por alteraccedilotildees nas antigas condiccedilotildees de
temperatura e pressatildeo das rochas magmaacuteticas ousedimentares que geram instabilidade dosminerais preacute-existentes
bull Dependendo do caso poderaacute ou natildeo mudar acomposiccedilatildeo mineraloacutegica mas a textura mudaobrigatoriamente
bull Exemplos Quartzito (derivada do metamorfismodo arenito) Maacutermore (proveacutem do Calcaacuterio ou doDolomito) Gnaisse (muito parecida com oGranito) etc
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Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
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Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
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Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
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httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4571
Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4671
Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4771
Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
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httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
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Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
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Classificaccedilatildeo de Jurandyr Ross
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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ldquoMares de morrosrdquo
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ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
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ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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g
E t atilde d atilde i l P d atilde d atilde t l
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Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
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Agentes internos
bullTambeacutem chamados de agentes endoacutegenos satildeoresponsaacuteveis pela criaccedilatildeo do relevo (geram as
partes altas e baixas)bullOriginam-se da crosta da Terra ou do manto(camada localizada abaixo da crosta)
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Agentes externos
bullTambeacutem chamados de agentes exoacutegenosmodelam a superfiacutecie terrestre
bullAtuam a superfiacutecie terrestre
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Escala Richter
Criada pelo sismoacutelogo norte-americano Charles Francis Richter a escala para medir
a energia liberada pelos tremores de terra passou a ser usada em 1935 A escalaRichter varia de zero a 9 graus0 ndash Tremor equivalente ao choque produzido por um homem de estatura normal aosaltar de uma cadeira para o chatildeo1 ndash Tremor sentido apenas por instrumentos cientiacuteficos2 ndash Tremor sentido por algumas pessoas e animais
3 ndash Tremor sentido por muitas pessoas4 ndash Tremor sentido por todas as pessoas5 ndash Algumas construccedilotildees satildeo destruiacutedas6 ndash Estruturas balanccedilam e paredes caem7 ndash Construccedilotildees satildeo destruiacutedas e pessoas morrem
8 ndash Calamidade todas as construccedilotildees sofrem danos e muitas satildeo completamentedestruiacutedas9 ndash Cataacutestrofe as construccedilotildees satildeo completamente destruiacutedas como se arrasadas poruma bomba nuclear e haacute mudanccedila aparente na paisagem
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Terremotos ocorridos em 1999
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Orogecircnesebull Pressatildeo horizontal exercida pelas placas tectocircnicas que
origina dobras eou falhasbull Eacute um processo geologicamente raacutepido que causa grandes
deformaccedilotildees na Crosta
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httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1571
Epirogecircnese
bull
Pressatildeo vertical exercida pelo magma como resposta aoaliacutevio de carga ou ao aumento de peso que geramovimento no sentido vertical (ascendente eoudescendente) de vastas aacutereas continentais sem perturbar
geologicamente a estrutura dos blocos afetadosbull Eacute um processo lento que natildeo gera deformaccedilotildees na crostabull Ex Fiordes na Escandinaacuteviabull Causam movimentos do niacutevel do mar que satildeo chamados
eustaacuteticos podendo ser do tipo transgressatildeo (avanccedilo domar sobre o continente) ou regressatildeo (recuo)
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bull Eacute a parte externa consolidada da Terra constituiacuteda de rochas
(agregados naturais de um ou mais minerais)bull Nas regiotildees continentais eacute formada por duas zonas a superior
denominada Sial (graccedilas agrave predominacircncia de rochas graniacuteticasricas em siliacutecio e alumiacutenio) e a zona inferior na qual se supotildee a
predominacircncia de siliacutecio e magneacutesio de onde vem o nome deSima
bull Sua espessura varia de 5 a 90 km
bull Estaacute dividida em vaacuterias partes chamadas Placas Tectocircnicas quese movimentam lateralmente independentes umas das outrasdevido as Correntes de Convecccedilatildeo
bull Estaacute equilibrada sobre o Manto segundo o princiacutepio da Isostasia
Crosta Terrestre
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Isostasia
bull Estado de equiliacutebrio dos
blocos continentais siaacutelicosque flutuam no substratomais denso do manto
bull Quanto mais alto for obloco maior seraacute a sua raiz
mergulhada
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Movimentaccedilatildeo das Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Exemplos de Dobramentos Modernos
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Divergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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bullTriacircngulo de Afar Eritreacuteia -Aacutefrica
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2571
Tangencial ou transformante ou transcorrente
bull Falha de Santo Andreacute - EUA
bull A Placa do Pacifico tem se movido a uma velocidade meacutedia de 5 cmano
bull nos uacuteltimos 10 milhotildees de anos
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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bull
Formaccedilatildeoda lha deSurtsey naIslacircndia em
1963
bullVulcanismo
bullRelevo formado por 6
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bullTimanfaya Lanzarote- Ilhas Canaacuterias
bull Relevo formado por 6
bull anos de erupccedilatildeo
F d d N h A i eacutel V l acirc i
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bullFernando de Noronha Arquipeacutelago Vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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A t aacuteli
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Austraacutelia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Faleacutesia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3271
bullErosatildeo Diferencial
bullNiacuteveis com maior
cimentaccedilatildeo
bullShip Rock NovoMeacutexico antigo
cone vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3371
bull Milhotildees de anos de erosatildeo glacial e eoacutelica esculpiram
os profundos vales e os precipiacutecios
bull Badlands Dakota do Sul (EUA)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3471
bullSerra Pelada 1983
bullSerra Pelada atual
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3571
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3771
Ciclo das rochas
Rocha Magmaacutetica
Rocha Metamoacuterfica
Rocha Sedimentar
Magma
Erosatildeo e Sedimentaccedilatildeo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3871
Rochas Magmaacuteticas ou Iacutegneas
bullFormadas pelo resfriamento e solidificaccedilatildeo do magma dentro dacrosta terrestre em profundidade (intrusivas) ou em superfiacutecie(extrusiva)
bullExemplos Granito (intrusiva) Basalto (extrusiva) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3971
Derrame basaacuteltico em Torres- RS
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4071
Rochas Sedimentares
bull Formada a partir de material originado da destruiccedilatildeo erosivade qualquer tipo de rocha material este que deveraacute sertransportado e depositado em um dos muitos ambientes de
sedimentaccedilatildeo da superfiacutecie terrestrebull Na maioria das vezes apresenta-se estratificada
bull Exemplos Argilito arenito siltitoetc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4171
Rochas Metamoacuterficas
bull Formadas por alteraccedilotildees nas antigas condiccedilotildees de
temperatura e pressatildeo das rochas magmaacuteticas ousedimentares que geram instabilidade dosminerais preacute-existentes
bull Dependendo do caso poderaacute ou natildeo mudar acomposiccedilatildeo mineraloacutegica mas a textura mudaobrigatoriamente
bull Exemplos Quartzito (derivada do metamorfismodo arenito) Maacutermore (proveacutem do Calcaacuterio ou doDolomito) Gnaisse (muito parecida com oGranito) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4271
Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4371
Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4471
Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4571
Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4671
Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4771
Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1071
Agentes internos
bullTambeacutem chamados de agentes endoacutegenos satildeoresponsaacuteveis pela criaccedilatildeo do relevo (geram as
partes altas e baixas)bullOriginam-se da crosta da Terra ou do manto(camada localizada abaixo da crosta)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Agentes externos
bullTambeacutem chamados de agentes exoacutegenosmodelam a superfiacutecie terrestre
bullAtuam a superfiacutecie terrestre
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1271
Escala Richter
Criada pelo sismoacutelogo norte-americano Charles Francis Richter a escala para medir
a energia liberada pelos tremores de terra passou a ser usada em 1935 A escalaRichter varia de zero a 9 graus0 ndash Tremor equivalente ao choque produzido por um homem de estatura normal aosaltar de uma cadeira para o chatildeo1 ndash Tremor sentido apenas por instrumentos cientiacuteficos2 ndash Tremor sentido por algumas pessoas e animais
3 ndash Tremor sentido por muitas pessoas4 ndash Tremor sentido por todas as pessoas5 ndash Algumas construccedilotildees satildeo destruiacutedas6 ndash Estruturas balanccedilam e paredes caem7 ndash Construccedilotildees satildeo destruiacutedas e pessoas morrem
8 ndash Calamidade todas as construccedilotildees sofrem danos e muitas satildeo completamentedestruiacutedas9 ndash Cataacutestrofe as construccedilotildees satildeo completamente destruiacutedas como se arrasadas poruma bomba nuclear e haacute mudanccedila aparente na paisagem
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1371
Terremotos ocorridos em 1999
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Orogecircnesebull Pressatildeo horizontal exercida pelas placas tectocircnicas que
origina dobras eou falhasbull Eacute um processo geologicamente raacutepido que causa grandes
deformaccedilotildees na Crosta
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1571
Epirogecircnese
bull
Pressatildeo vertical exercida pelo magma como resposta aoaliacutevio de carga ou ao aumento de peso que geramovimento no sentido vertical (ascendente eoudescendente) de vastas aacutereas continentais sem perturbar
geologicamente a estrutura dos blocos afetadosbull Eacute um processo lento que natildeo gera deformaccedilotildees na crostabull Ex Fiordes na Escandinaacuteviabull Causam movimentos do niacutevel do mar que satildeo chamados
eustaacuteticos podendo ser do tipo transgressatildeo (avanccedilo domar sobre o continente) ou regressatildeo (recuo)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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bull Eacute a parte externa consolidada da Terra constituiacuteda de rochas
(agregados naturais de um ou mais minerais)bull Nas regiotildees continentais eacute formada por duas zonas a superior
denominada Sial (graccedilas agrave predominacircncia de rochas graniacuteticasricas em siliacutecio e alumiacutenio) e a zona inferior na qual se supotildee a
predominacircncia de siliacutecio e magneacutesio de onde vem o nome deSima
bull Sua espessura varia de 5 a 90 km
bull Estaacute dividida em vaacuterias partes chamadas Placas Tectocircnicas quese movimentam lateralmente independentes umas das outrasdevido as Correntes de Convecccedilatildeo
bull Estaacute equilibrada sobre o Manto segundo o princiacutepio da Isostasia
Crosta Terrestre
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Isostasia
bull Estado de equiliacutebrio dos
blocos continentais siaacutelicosque flutuam no substratomais denso do manto
bull Quanto mais alto for obloco maior seraacute a sua raiz
mergulhada
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Movimentaccedilatildeo das Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Exemplos de Dobramentos Modernos
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Divergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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bullTriacircngulo de Afar Eritreacuteia -Aacutefrica
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Tangencial ou transformante ou transcorrente
bull Falha de Santo Andreacute - EUA
bull A Placa do Pacifico tem se movido a uma velocidade meacutedia de 5 cmano
bull nos uacuteltimos 10 milhotildees de anos
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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bull
Formaccedilatildeoda lha deSurtsey naIslacircndia em
1963
bullVulcanismo
bullRelevo formado por 6
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bullTimanfaya Lanzarote- Ilhas Canaacuterias
bull Relevo formado por 6
bull anos de erupccedilatildeo
F d d N h A i eacutel V l acirc i
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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bullFernando de Noronha Arquipeacutelago Vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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A t aacuteli
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Austraacutelia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Faleacutesia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3271
bullErosatildeo Diferencial
bullNiacuteveis com maior
cimentaccedilatildeo
bullShip Rock NovoMeacutexico antigo
cone vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3371
bull Milhotildees de anos de erosatildeo glacial e eoacutelica esculpiram
os profundos vales e os precipiacutecios
bull Badlands Dakota do Sul (EUA)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3471
bullSerra Pelada 1983
bullSerra Pelada atual
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3571
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3771
Ciclo das rochas
Rocha Magmaacutetica
Rocha Metamoacuterfica
Rocha Sedimentar
Magma
Erosatildeo e Sedimentaccedilatildeo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3871
Rochas Magmaacuteticas ou Iacutegneas
bullFormadas pelo resfriamento e solidificaccedilatildeo do magma dentro dacrosta terrestre em profundidade (intrusivas) ou em superfiacutecie(extrusiva)
bullExemplos Granito (intrusiva) Basalto (extrusiva) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3971
Derrame basaacuteltico em Torres- RS
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4071
Rochas Sedimentares
bull Formada a partir de material originado da destruiccedilatildeo erosivade qualquer tipo de rocha material este que deveraacute sertransportado e depositado em um dos muitos ambientes de
sedimentaccedilatildeo da superfiacutecie terrestrebull Na maioria das vezes apresenta-se estratificada
bull Exemplos Argilito arenito siltitoetc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4171
Rochas Metamoacuterficas
bull Formadas por alteraccedilotildees nas antigas condiccedilotildees de
temperatura e pressatildeo das rochas magmaacuteticas ousedimentares que geram instabilidade dosminerais preacute-existentes
bull Dependendo do caso poderaacute ou natildeo mudar acomposiccedilatildeo mineraloacutegica mas a textura mudaobrigatoriamente
bull Exemplos Quartzito (derivada do metamorfismodo arenito) Maacutermore (proveacutem do Calcaacuterio ou doDolomito) Gnaisse (muito parecida com oGranito) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4271
Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4371
Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4471
Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4571
Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4671
Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4771
Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4971
Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5071
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5271
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5371
ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1171
Agentes externos
bullTambeacutem chamados de agentes exoacutegenosmodelam a superfiacutecie terrestre
bullAtuam a superfiacutecie terrestre
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1271
Escala Richter
Criada pelo sismoacutelogo norte-americano Charles Francis Richter a escala para medir
a energia liberada pelos tremores de terra passou a ser usada em 1935 A escalaRichter varia de zero a 9 graus0 ndash Tremor equivalente ao choque produzido por um homem de estatura normal aosaltar de uma cadeira para o chatildeo1 ndash Tremor sentido apenas por instrumentos cientiacuteficos2 ndash Tremor sentido por algumas pessoas e animais
3 ndash Tremor sentido por muitas pessoas4 ndash Tremor sentido por todas as pessoas5 ndash Algumas construccedilotildees satildeo destruiacutedas6 ndash Estruturas balanccedilam e paredes caem7 ndash Construccedilotildees satildeo destruiacutedas e pessoas morrem
8 ndash Calamidade todas as construccedilotildees sofrem danos e muitas satildeo completamentedestruiacutedas9 ndash Cataacutestrofe as construccedilotildees satildeo completamente destruiacutedas como se arrasadas poruma bomba nuclear e haacute mudanccedila aparente na paisagem
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1371
Terremotos ocorridos em 1999
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1471
Orogecircnesebull Pressatildeo horizontal exercida pelas placas tectocircnicas que
origina dobras eou falhasbull Eacute um processo geologicamente raacutepido que causa grandes
deformaccedilotildees na Crosta
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1571
Epirogecircnese
bull
Pressatildeo vertical exercida pelo magma como resposta aoaliacutevio de carga ou ao aumento de peso que geramovimento no sentido vertical (ascendente eoudescendente) de vastas aacutereas continentais sem perturbar
geologicamente a estrutura dos blocos afetadosbull Eacute um processo lento que natildeo gera deformaccedilotildees na crostabull Ex Fiordes na Escandinaacuteviabull Causam movimentos do niacutevel do mar que satildeo chamados
eustaacuteticos podendo ser do tipo transgressatildeo (avanccedilo domar sobre o continente) ou regressatildeo (recuo)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1671
bull Eacute a parte externa consolidada da Terra constituiacuteda de rochas
(agregados naturais de um ou mais minerais)bull Nas regiotildees continentais eacute formada por duas zonas a superior
denominada Sial (graccedilas agrave predominacircncia de rochas graniacuteticasricas em siliacutecio e alumiacutenio) e a zona inferior na qual se supotildee a
predominacircncia de siliacutecio e magneacutesio de onde vem o nome deSima
bull Sua espessura varia de 5 a 90 km
bull Estaacute dividida em vaacuterias partes chamadas Placas Tectocircnicas quese movimentam lateralmente independentes umas das outrasdevido as Correntes de Convecccedilatildeo
bull Estaacute equilibrada sobre o Manto segundo o princiacutepio da Isostasia
Crosta Terrestre
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1771
Isostasia
bull Estado de equiliacutebrio dos
blocos continentais siaacutelicosque flutuam no substratomais denso do manto
bull Quanto mais alto for obloco maior seraacute a sua raiz
mergulhada
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1871
Movimentaccedilatildeo das Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2271
Exemplos de Dobramentos Modernos
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2371
Divergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2471
bullTriacircngulo de Afar Eritreacuteia -Aacutefrica
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2571
Tangencial ou transformante ou transcorrente
bull Falha de Santo Andreacute - EUA
bull A Placa do Pacifico tem se movido a uma velocidade meacutedia de 5 cmano
bull nos uacuteltimos 10 milhotildees de anos
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2671
bull
Formaccedilatildeoda lha deSurtsey naIslacircndia em
1963
bullVulcanismo
bullRelevo formado por 6
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2771
bullTimanfaya Lanzarote- Ilhas Canaacuterias
bull Relevo formado por 6
bull anos de erupccedilatildeo
F d d N h A i eacutel V l acirc i
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2871
bullFernando de Noronha Arquipeacutelago Vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2971
A t aacuteli
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3071
Austraacutelia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3171
Faleacutesia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3271
bullErosatildeo Diferencial
bullNiacuteveis com maior
cimentaccedilatildeo
bullShip Rock NovoMeacutexico antigo
cone vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3371
bull Milhotildees de anos de erosatildeo glacial e eoacutelica esculpiram
os profundos vales e os precipiacutecios
bull Badlands Dakota do Sul (EUA)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3471
bullSerra Pelada 1983
bullSerra Pelada atual
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3571
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3771
Ciclo das rochas
Rocha Magmaacutetica
Rocha Metamoacuterfica
Rocha Sedimentar
Magma
Erosatildeo e Sedimentaccedilatildeo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3871
Rochas Magmaacuteticas ou Iacutegneas
bullFormadas pelo resfriamento e solidificaccedilatildeo do magma dentro dacrosta terrestre em profundidade (intrusivas) ou em superfiacutecie(extrusiva)
bullExemplos Granito (intrusiva) Basalto (extrusiva) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3971
Derrame basaacuteltico em Torres- RS
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4071
Rochas Sedimentares
bull Formada a partir de material originado da destruiccedilatildeo erosivade qualquer tipo de rocha material este que deveraacute sertransportado e depositado em um dos muitos ambientes de
sedimentaccedilatildeo da superfiacutecie terrestrebull Na maioria das vezes apresenta-se estratificada
bull Exemplos Argilito arenito siltitoetc
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httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4171
Rochas Metamoacuterficas
bull Formadas por alteraccedilotildees nas antigas condiccedilotildees de
temperatura e pressatildeo das rochas magmaacuteticas ousedimentares que geram instabilidade dosminerais preacute-existentes
bull Dependendo do caso poderaacute ou natildeo mudar acomposiccedilatildeo mineraloacutegica mas a textura mudaobrigatoriamente
bull Exemplos Quartzito (derivada do metamorfismodo arenito) Maacutermore (proveacutem do Calcaacuterio ou doDolomito) Gnaisse (muito parecida com oGranito) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4271
Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4371
Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4471
Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4571
Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4671
Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4771
Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4971
Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5071
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5271
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5371
ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1271
Escala Richter
Criada pelo sismoacutelogo norte-americano Charles Francis Richter a escala para medir
a energia liberada pelos tremores de terra passou a ser usada em 1935 A escalaRichter varia de zero a 9 graus0 ndash Tremor equivalente ao choque produzido por um homem de estatura normal aosaltar de uma cadeira para o chatildeo1 ndash Tremor sentido apenas por instrumentos cientiacuteficos2 ndash Tremor sentido por algumas pessoas e animais
3 ndash Tremor sentido por muitas pessoas4 ndash Tremor sentido por todas as pessoas5 ndash Algumas construccedilotildees satildeo destruiacutedas6 ndash Estruturas balanccedilam e paredes caem7 ndash Construccedilotildees satildeo destruiacutedas e pessoas morrem
8 ndash Calamidade todas as construccedilotildees sofrem danos e muitas satildeo completamentedestruiacutedas9 ndash Cataacutestrofe as construccedilotildees satildeo completamente destruiacutedas como se arrasadas poruma bomba nuclear e haacute mudanccedila aparente na paisagem
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1371
Terremotos ocorridos em 1999
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1471
Orogecircnesebull Pressatildeo horizontal exercida pelas placas tectocircnicas que
origina dobras eou falhasbull Eacute um processo geologicamente raacutepido que causa grandes
deformaccedilotildees na Crosta
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1571
Epirogecircnese
bull
Pressatildeo vertical exercida pelo magma como resposta aoaliacutevio de carga ou ao aumento de peso que geramovimento no sentido vertical (ascendente eoudescendente) de vastas aacutereas continentais sem perturbar
geologicamente a estrutura dos blocos afetadosbull Eacute um processo lento que natildeo gera deformaccedilotildees na crostabull Ex Fiordes na Escandinaacuteviabull Causam movimentos do niacutevel do mar que satildeo chamados
eustaacuteticos podendo ser do tipo transgressatildeo (avanccedilo domar sobre o continente) ou regressatildeo (recuo)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1671
bull Eacute a parte externa consolidada da Terra constituiacuteda de rochas
(agregados naturais de um ou mais minerais)bull Nas regiotildees continentais eacute formada por duas zonas a superior
denominada Sial (graccedilas agrave predominacircncia de rochas graniacuteticasricas em siliacutecio e alumiacutenio) e a zona inferior na qual se supotildee a
predominacircncia de siliacutecio e magneacutesio de onde vem o nome deSima
bull Sua espessura varia de 5 a 90 km
bull Estaacute dividida em vaacuterias partes chamadas Placas Tectocircnicas quese movimentam lateralmente independentes umas das outrasdevido as Correntes de Convecccedilatildeo
bull Estaacute equilibrada sobre o Manto segundo o princiacutepio da Isostasia
Crosta Terrestre
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1771
Isostasia
bull Estado de equiliacutebrio dos
blocos continentais siaacutelicosque flutuam no substratomais denso do manto
bull Quanto mais alto for obloco maior seraacute a sua raiz
mergulhada
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1871
Movimentaccedilatildeo das Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2271
Exemplos de Dobramentos Modernos
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2371
Divergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2471
bullTriacircngulo de Afar Eritreacuteia -Aacutefrica
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2571
Tangencial ou transformante ou transcorrente
bull Falha de Santo Andreacute - EUA
bull A Placa do Pacifico tem se movido a uma velocidade meacutedia de 5 cmano
bull nos uacuteltimos 10 milhotildees de anos
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2671
bull
Formaccedilatildeoda lha deSurtsey naIslacircndia em
1963
bullVulcanismo
bullRelevo formado por 6
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2771
bullTimanfaya Lanzarote- Ilhas Canaacuterias
bull Relevo formado por 6
bull anos de erupccedilatildeo
F d d N h A i eacutel V l acirc i
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2871
bullFernando de Noronha Arquipeacutelago Vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2971
A t aacuteli
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3071
Austraacutelia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3171
Faleacutesia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3271
bullErosatildeo Diferencial
bullNiacuteveis com maior
cimentaccedilatildeo
bullShip Rock NovoMeacutexico antigo
cone vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3371
bull Milhotildees de anos de erosatildeo glacial e eoacutelica esculpiram
os profundos vales e os precipiacutecios
bull Badlands Dakota do Sul (EUA)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3471
bullSerra Pelada 1983
bullSerra Pelada atual
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3571
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3771
Ciclo das rochas
Rocha Magmaacutetica
Rocha Metamoacuterfica
Rocha Sedimentar
Magma
Erosatildeo e Sedimentaccedilatildeo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3871
Rochas Magmaacuteticas ou Iacutegneas
bullFormadas pelo resfriamento e solidificaccedilatildeo do magma dentro dacrosta terrestre em profundidade (intrusivas) ou em superfiacutecie(extrusiva)
bullExemplos Granito (intrusiva) Basalto (extrusiva) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3971
Derrame basaacuteltico em Torres- RS
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4071
Rochas Sedimentares
bull Formada a partir de material originado da destruiccedilatildeo erosivade qualquer tipo de rocha material este que deveraacute sertransportado e depositado em um dos muitos ambientes de
sedimentaccedilatildeo da superfiacutecie terrestrebull Na maioria das vezes apresenta-se estratificada
bull Exemplos Argilito arenito siltitoetc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4171
Rochas Metamoacuterficas
bull Formadas por alteraccedilotildees nas antigas condiccedilotildees de
temperatura e pressatildeo das rochas magmaacuteticas ousedimentares que geram instabilidade dosminerais preacute-existentes
bull Dependendo do caso poderaacute ou natildeo mudar acomposiccedilatildeo mineraloacutegica mas a textura mudaobrigatoriamente
bull Exemplos Quartzito (derivada do metamorfismodo arenito) Maacutermore (proveacutem do Calcaacuterio ou doDolomito) Gnaisse (muito parecida com oGranito) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4271
Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4371
Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4471
Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4571
Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4671
Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4771
Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4971
Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5071
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5271
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1371
Terremotos ocorridos em 1999
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1471
Orogecircnesebull Pressatildeo horizontal exercida pelas placas tectocircnicas que
origina dobras eou falhasbull Eacute um processo geologicamente raacutepido que causa grandes
deformaccedilotildees na Crosta
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1571
Epirogecircnese
bull
Pressatildeo vertical exercida pelo magma como resposta aoaliacutevio de carga ou ao aumento de peso que geramovimento no sentido vertical (ascendente eoudescendente) de vastas aacutereas continentais sem perturbar
geologicamente a estrutura dos blocos afetadosbull Eacute um processo lento que natildeo gera deformaccedilotildees na crostabull Ex Fiordes na Escandinaacuteviabull Causam movimentos do niacutevel do mar que satildeo chamados
eustaacuteticos podendo ser do tipo transgressatildeo (avanccedilo domar sobre o continente) ou regressatildeo (recuo)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1671
bull Eacute a parte externa consolidada da Terra constituiacuteda de rochas
(agregados naturais de um ou mais minerais)bull Nas regiotildees continentais eacute formada por duas zonas a superior
denominada Sial (graccedilas agrave predominacircncia de rochas graniacuteticasricas em siliacutecio e alumiacutenio) e a zona inferior na qual se supotildee a
predominacircncia de siliacutecio e magneacutesio de onde vem o nome deSima
bull Sua espessura varia de 5 a 90 km
bull Estaacute dividida em vaacuterias partes chamadas Placas Tectocircnicas quese movimentam lateralmente independentes umas das outrasdevido as Correntes de Convecccedilatildeo
bull Estaacute equilibrada sobre o Manto segundo o princiacutepio da Isostasia
Crosta Terrestre
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1771
Isostasia
bull Estado de equiliacutebrio dos
blocos continentais siaacutelicosque flutuam no substratomais denso do manto
bull Quanto mais alto for obloco maior seraacute a sua raiz
mergulhada
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1871
Movimentaccedilatildeo das Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2271
Exemplos de Dobramentos Modernos
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2371
Divergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2471
bullTriacircngulo de Afar Eritreacuteia -Aacutefrica
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2571
Tangencial ou transformante ou transcorrente
bull Falha de Santo Andreacute - EUA
bull A Placa do Pacifico tem se movido a uma velocidade meacutedia de 5 cmano
bull nos uacuteltimos 10 milhotildees de anos
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2671
bull
Formaccedilatildeoda lha deSurtsey naIslacircndia em
1963
bullVulcanismo
bullRelevo formado por 6
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2771
bullTimanfaya Lanzarote- Ilhas Canaacuterias
bull Relevo formado por 6
bull anos de erupccedilatildeo
F d d N h A i eacutel V l acirc i
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2871
bullFernando de Noronha Arquipeacutelago Vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2971
A t aacuteli
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3071
Austraacutelia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3171
Faleacutesia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3271
bullErosatildeo Diferencial
bullNiacuteveis com maior
cimentaccedilatildeo
bullShip Rock NovoMeacutexico antigo
cone vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3371
bull Milhotildees de anos de erosatildeo glacial e eoacutelica esculpiram
os profundos vales e os precipiacutecios
bull Badlands Dakota do Sul (EUA)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3471
bullSerra Pelada 1983
bullSerra Pelada atual
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3571
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3771
Ciclo das rochas
Rocha Magmaacutetica
Rocha Metamoacuterfica
Rocha Sedimentar
Magma
Erosatildeo e Sedimentaccedilatildeo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3871
Rochas Magmaacuteticas ou Iacutegneas
bullFormadas pelo resfriamento e solidificaccedilatildeo do magma dentro dacrosta terrestre em profundidade (intrusivas) ou em superfiacutecie(extrusiva)
bullExemplos Granito (intrusiva) Basalto (extrusiva) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3971
Derrame basaacuteltico em Torres- RS
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4071
Rochas Sedimentares
bull Formada a partir de material originado da destruiccedilatildeo erosivade qualquer tipo de rocha material este que deveraacute sertransportado e depositado em um dos muitos ambientes de
sedimentaccedilatildeo da superfiacutecie terrestrebull Na maioria das vezes apresenta-se estratificada
bull Exemplos Argilito arenito siltitoetc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4171
Rochas Metamoacuterficas
bull Formadas por alteraccedilotildees nas antigas condiccedilotildees de
temperatura e pressatildeo das rochas magmaacuteticas ousedimentares que geram instabilidade dosminerais preacute-existentes
bull Dependendo do caso poderaacute ou natildeo mudar acomposiccedilatildeo mineraloacutegica mas a textura mudaobrigatoriamente
bull Exemplos Quartzito (derivada do metamorfismodo arenito) Maacutermore (proveacutem do Calcaacuterio ou doDolomito) Gnaisse (muito parecida com oGranito) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4271
Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4371
Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4471
Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4571
Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4671
Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4771
Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4971
Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5071
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5271
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5371
ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1471
Orogecircnesebull Pressatildeo horizontal exercida pelas placas tectocircnicas que
origina dobras eou falhasbull Eacute um processo geologicamente raacutepido que causa grandes
deformaccedilotildees na Crosta
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1571
Epirogecircnese
bull
Pressatildeo vertical exercida pelo magma como resposta aoaliacutevio de carga ou ao aumento de peso que geramovimento no sentido vertical (ascendente eoudescendente) de vastas aacutereas continentais sem perturbar
geologicamente a estrutura dos blocos afetadosbull Eacute um processo lento que natildeo gera deformaccedilotildees na crostabull Ex Fiordes na Escandinaacuteviabull Causam movimentos do niacutevel do mar que satildeo chamados
eustaacuteticos podendo ser do tipo transgressatildeo (avanccedilo domar sobre o continente) ou regressatildeo (recuo)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1671
bull Eacute a parte externa consolidada da Terra constituiacuteda de rochas
(agregados naturais de um ou mais minerais)bull Nas regiotildees continentais eacute formada por duas zonas a superior
denominada Sial (graccedilas agrave predominacircncia de rochas graniacuteticasricas em siliacutecio e alumiacutenio) e a zona inferior na qual se supotildee a
predominacircncia de siliacutecio e magneacutesio de onde vem o nome deSima
bull Sua espessura varia de 5 a 90 km
bull Estaacute dividida em vaacuterias partes chamadas Placas Tectocircnicas quese movimentam lateralmente independentes umas das outrasdevido as Correntes de Convecccedilatildeo
bull Estaacute equilibrada sobre o Manto segundo o princiacutepio da Isostasia
Crosta Terrestre
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1771
Isostasia
bull Estado de equiliacutebrio dos
blocos continentais siaacutelicosque flutuam no substratomais denso do manto
bull Quanto mais alto for obloco maior seraacute a sua raiz
mergulhada
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1871
Movimentaccedilatildeo das Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2271
Exemplos de Dobramentos Modernos
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2371
Divergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2471
bullTriacircngulo de Afar Eritreacuteia -Aacutefrica
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2571
Tangencial ou transformante ou transcorrente
bull Falha de Santo Andreacute - EUA
bull A Placa do Pacifico tem se movido a uma velocidade meacutedia de 5 cmano
bull nos uacuteltimos 10 milhotildees de anos
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2671
bull
Formaccedilatildeoda lha deSurtsey naIslacircndia em
1963
bullVulcanismo
bullRelevo formado por 6
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2771
bullTimanfaya Lanzarote- Ilhas Canaacuterias
bull Relevo formado por 6
bull anos de erupccedilatildeo
F d d N h A i eacutel V l acirc i
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2871
bullFernando de Noronha Arquipeacutelago Vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2971
A t aacuteli
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3071
Austraacutelia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3171
Faleacutesia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3271
bullErosatildeo Diferencial
bullNiacuteveis com maior
cimentaccedilatildeo
bullShip Rock NovoMeacutexico antigo
cone vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3371
bull Milhotildees de anos de erosatildeo glacial e eoacutelica esculpiram
os profundos vales e os precipiacutecios
bull Badlands Dakota do Sul (EUA)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3471
bullSerra Pelada 1983
bullSerra Pelada atual
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3571
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3771
Ciclo das rochas
Rocha Magmaacutetica
Rocha Metamoacuterfica
Rocha Sedimentar
Magma
Erosatildeo e Sedimentaccedilatildeo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3871
Rochas Magmaacuteticas ou Iacutegneas
bullFormadas pelo resfriamento e solidificaccedilatildeo do magma dentro dacrosta terrestre em profundidade (intrusivas) ou em superfiacutecie(extrusiva)
bullExemplos Granito (intrusiva) Basalto (extrusiva) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3971
Derrame basaacuteltico em Torres- RS
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4071
Rochas Sedimentares
bull Formada a partir de material originado da destruiccedilatildeo erosivade qualquer tipo de rocha material este que deveraacute sertransportado e depositado em um dos muitos ambientes de
sedimentaccedilatildeo da superfiacutecie terrestrebull Na maioria das vezes apresenta-se estratificada
bull Exemplos Argilito arenito siltitoetc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4171
Rochas Metamoacuterficas
bull Formadas por alteraccedilotildees nas antigas condiccedilotildees de
temperatura e pressatildeo das rochas magmaacuteticas ousedimentares que geram instabilidade dosminerais preacute-existentes
bull Dependendo do caso poderaacute ou natildeo mudar acomposiccedilatildeo mineraloacutegica mas a textura mudaobrigatoriamente
bull Exemplos Quartzito (derivada do metamorfismodo arenito) Maacutermore (proveacutem do Calcaacuterio ou doDolomito) Gnaisse (muito parecida com oGranito) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4271
Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4371
Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4471
Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4571
Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4671
Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4771
Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4971
Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5071
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5271
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5371
ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1571
Epirogecircnese
bull
Pressatildeo vertical exercida pelo magma como resposta aoaliacutevio de carga ou ao aumento de peso que geramovimento no sentido vertical (ascendente eoudescendente) de vastas aacutereas continentais sem perturbar
geologicamente a estrutura dos blocos afetadosbull Eacute um processo lento que natildeo gera deformaccedilotildees na crostabull Ex Fiordes na Escandinaacuteviabull Causam movimentos do niacutevel do mar que satildeo chamados
eustaacuteticos podendo ser do tipo transgressatildeo (avanccedilo domar sobre o continente) ou regressatildeo (recuo)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1671
bull Eacute a parte externa consolidada da Terra constituiacuteda de rochas
(agregados naturais de um ou mais minerais)bull Nas regiotildees continentais eacute formada por duas zonas a superior
denominada Sial (graccedilas agrave predominacircncia de rochas graniacuteticasricas em siliacutecio e alumiacutenio) e a zona inferior na qual se supotildee a
predominacircncia de siliacutecio e magneacutesio de onde vem o nome deSima
bull Sua espessura varia de 5 a 90 km
bull Estaacute dividida em vaacuterias partes chamadas Placas Tectocircnicas quese movimentam lateralmente independentes umas das outrasdevido as Correntes de Convecccedilatildeo
bull Estaacute equilibrada sobre o Manto segundo o princiacutepio da Isostasia
Crosta Terrestre
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1771
Isostasia
bull Estado de equiliacutebrio dos
blocos continentais siaacutelicosque flutuam no substratomais denso do manto
bull Quanto mais alto for obloco maior seraacute a sua raiz
mergulhada
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1871
Movimentaccedilatildeo das Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2271
Exemplos de Dobramentos Modernos
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2371
Divergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2471
bullTriacircngulo de Afar Eritreacuteia -Aacutefrica
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2571
Tangencial ou transformante ou transcorrente
bull Falha de Santo Andreacute - EUA
bull A Placa do Pacifico tem se movido a uma velocidade meacutedia de 5 cmano
bull nos uacuteltimos 10 milhotildees de anos
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2671
bull
Formaccedilatildeoda lha deSurtsey naIslacircndia em
1963
bullVulcanismo
bullRelevo formado por 6
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2771
bullTimanfaya Lanzarote- Ilhas Canaacuterias
bull Relevo formado por 6
bull anos de erupccedilatildeo
F d d N h A i eacutel V l acirc i
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2871
bullFernando de Noronha Arquipeacutelago Vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2971
A t aacuteli
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Austraacutelia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3171
Faleacutesia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3271
bullErosatildeo Diferencial
bullNiacuteveis com maior
cimentaccedilatildeo
bullShip Rock NovoMeacutexico antigo
cone vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3371
bull Milhotildees de anos de erosatildeo glacial e eoacutelica esculpiram
os profundos vales e os precipiacutecios
bull Badlands Dakota do Sul (EUA)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3471
bullSerra Pelada 1983
bullSerra Pelada atual
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3571
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3771
Ciclo das rochas
Rocha Magmaacutetica
Rocha Metamoacuterfica
Rocha Sedimentar
Magma
Erosatildeo e Sedimentaccedilatildeo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3871
Rochas Magmaacuteticas ou Iacutegneas
bullFormadas pelo resfriamento e solidificaccedilatildeo do magma dentro dacrosta terrestre em profundidade (intrusivas) ou em superfiacutecie(extrusiva)
bullExemplos Granito (intrusiva) Basalto (extrusiva) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3971
Derrame basaacuteltico em Torres- RS
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4071
Rochas Sedimentares
bull Formada a partir de material originado da destruiccedilatildeo erosivade qualquer tipo de rocha material este que deveraacute sertransportado e depositado em um dos muitos ambientes de
sedimentaccedilatildeo da superfiacutecie terrestrebull Na maioria das vezes apresenta-se estratificada
bull Exemplos Argilito arenito siltitoetc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4171
Rochas Metamoacuterficas
bull Formadas por alteraccedilotildees nas antigas condiccedilotildees de
temperatura e pressatildeo das rochas magmaacuteticas ousedimentares que geram instabilidade dosminerais preacute-existentes
bull Dependendo do caso poderaacute ou natildeo mudar acomposiccedilatildeo mineraloacutegica mas a textura mudaobrigatoriamente
bull Exemplos Quartzito (derivada do metamorfismodo arenito) Maacutermore (proveacutem do Calcaacuterio ou doDolomito) Gnaisse (muito parecida com oGranito) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4271
Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4371
Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4471
Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4571
Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4671
Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4771
Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4971
Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5071
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5271
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5371
ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1671
bull Eacute a parte externa consolidada da Terra constituiacuteda de rochas
(agregados naturais de um ou mais minerais)bull Nas regiotildees continentais eacute formada por duas zonas a superior
denominada Sial (graccedilas agrave predominacircncia de rochas graniacuteticasricas em siliacutecio e alumiacutenio) e a zona inferior na qual se supotildee a
predominacircncia de siliacutecio e magneacutesio de onde vem o nome deSima
bull Sua espessura varia de 5 a 90 km
bull Estaacute dividida em vaacuterias partes chamadas Placas Tectocircnicas quese movimentam lateralmente independentes umas das outrasdevido as Correntes de Convecccedilatildeo
bull Estaacute equilibrada sobre o Manto segundo o princiacutepio da Isostasia
Crosta Terrestre
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1771
Isostasia
bull Estado de equiliacutebrio dos
blocos continentais siaacutelicosque flutuam no substratomais denso do manto
bull Quanto mais alto for obloco maior seraacute a sua raiz
mergulhada
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1871
Movimentaccedilatildeo das Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2271
Exemplos de Dobramentos Modernos
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2371
Divergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2471
bullTriacircngulo de Afar Eritreacuteia -Aacutefrica
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2571
Tangencial ou transformante ou transcorrente
bull Falha de Santo Andreacute - EUA
bull A Placa do Pacifico tem se movido a uma velocidade meacutedia de 5 cmano
bull nos uacuteltimos 10 milhotildees de anos
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2671
bull
Formaccedilatildeoda lha deSurtsey naIslacircndia em
1963
bullVulcanismo
bullRelevo formado por 6
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2771
bullTimanfaya Lanzarote- Ilhas Canaacuterias
bull Relevo formado por 6
bull anos de erupccedilatildeo
F d d N h A i eacutel V l acirc i
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2871
bullFernando de Noronha Arquipeacutelago Vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2971
A t aacuteli
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3071
Austraacutelia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3171
Faleacutesia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3271
bullErosatildeo Diferencial
bullNiacuteveis com maior
cimentaccedilatildeo
bullShip Rock NovoMeacutexico antigo
cone vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3371
bull Milhotildees de anos de erosatildeo glacial e eoacutelica esculpiram
os profundos vales e os precipiacutecios
bull Badlands Dakota do Sul (EUA)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3471
bullSerra Pelada 1983
bullSerra Pelada atual
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3571
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3771
Ciclo das rochas
Rocha Magmaacutetica
Rocha Metamoacuterfica
Rocha Sedimentar
Magma
Erosatildeo e Sedimentaccedilatildeo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3871
Rochas Magmaacuteticas ou Iacutegneas
bullFormadas pelo resfriamento e solidificaccedilatildeo do magma dentro dacrosta terrestre em profundidade (intrusivas) ou em superfiacutecie(extrusiva)
bullExemplos Granito (intrusiva) Basalto (extrusiva) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3971
Derrame basaacuteltico em Torres- RS
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4071
Rochas Sedimentares
bull Formada a partir de material originado da destruiccedilatildeo erosivade qualquer tipo de rocha material este que deveraacute sertransportado e depositado em um dos muitos ambientes de
sedimentaccedilatildeo da superfiacutecie terrestrebull Na maioria das vezes apresenta-se estratificada
bull Exemplos Argilito arenito siltitoetc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4171
Rochas Metamoacuterficas
bull Formadas por alteraccedilotildees nas antigas condiccedilotildees de
temperatura e pressatildeo das rochas magmaacuteticas ousedimentares que geram instabilidade dosminerais preacute-existentes
bull Dependendo do caso poderaacute ou natildeo mudar acomposiccedilatildeo mineraloacutegica mas a textura mudaobrigatoriamente
bull Exemplos Quartzito (derivada do metamorfismodo arenito) Maacutermore (proveacutem do Calcaacuterio ou doDolomito) Gnaisse (muito parecida com oGranito) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4271
Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4371
Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4471
Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4571
Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4671
Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4771
Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4971
Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5071
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1771
Isostasia
bull Estado de equiliacutebrio dos
blocos continentais siaacutelicosque flutuam no substratomais denso do manto
bull Quanto mais alto for obloco maior seraacute a sua raiz
mergulhada
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1871
Movimentaccedilatildeo das Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2271
Exemplos de Dobramentos Modernos
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2371
Divergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2471
bullTriacircngulo de Afar Eritreacuteia -Aacutefrica
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2571
Tangencial ou transformante ou transcorrente
bull Falha de Santo Andreacute - EUA
bull A Placa do Pacifico tem se movido a uma velocidade meacutedia de 5 cmano
bull nos uacuteltimos 10 milhotildees de anos
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2671
bull
Formaccedilatildeoda lha deSurtsey naIslacircndia em
1963
bullVulcanismo
bullRelevo formado por 6
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2771
bullTimanfaya Lanzarote- Ilhas Canaacuterias
bull Relevo formado por 6
bull anos de erupccedilatildeo
F d d N h A i eacutel V l acirc i
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2871
bullFernando de Noronha Arquipeacutelago Vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2971
A t aacuteli
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3071
Austraacutelia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3171
Faleacutesia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3271
bullErosatildeo Diferencial
bullNiacuteveis com maior
cimentaccedilatildeo
bullShip Rock NovoMeacutexico antigo
cone vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3371
bull Milhotildees de anos de erosatildeo glacial e eoacutelica esculpiram
os profundos vales e os precipiacutecios
bull Badlands Dakota do Sul (EUA)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3471
bullSerra Pelada 1983
bullSerra Pelada atual
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3571
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3771
Ciclo das rochas
Rocha Magmaacutetica
Rocha Metamoacuterfica
Rocha Sedimentar
Magma
Erosatildeo e Sedimentaccedilatildeo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3871
Rochas Magmaacuteticas ou Iacutegneas
bullFormadas pelo resfriamento e solidificaccedilatildeo do magma dentro dacrosta terrestre em profundidade (intrusivas) ou em superfiacutecie(extrusiva)
bullExemplos Granito (intrusiva) Basalto (extrusiva) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3971
Derrame basaacuteltico em Torres- RS
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4071
Rochas Sedimentares
bull Formada a partir de material originado da destruiccedilatildeo erosivade qualquer tipo de rocha material este que deveraacute sertransportado e depositado em um dos muitos ambientes de
sedimentaccedilatildeo da superfiacutecie terrestrebull Na maioria das vezes apresenta-se estratificada
bull Exemplos Argilito arenito siltitoetc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4171
Rochas Metamoacuterficas
bull Formadas por alteraccedilotildees nas antigas condiccedilotildees de
temperatura e pressatildeo das rochas magmaacuteticas ousedimentares que geram instabilidade dosminerais preacute-existentes
bull Dependendo do caso poderaacute ou natildeo mudar acomposiccedilatildeo mineraloacutegica mas a textura mudaobrigatoriamente
bull Exemplos Quartzito (derivada do metamorfismodo arenito) Maacutermore (proveacutem do Calcaacuterio ou doDolomito) Gnaisse (muito parecida com oGranito) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4271
Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4371
Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4471
Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4571
Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4671
Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4771
Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4971
Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5071
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5271
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5371
ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1871
Movimentaccedilatildeo das Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2271
Exemplos de Dobramentos Modernos
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2371
Divergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2471
bullTriacircngulo de Afar Eritreacuteia -Aacutefrica
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2571
Tangencial ou transformante ou transcorrente
bull Falha de Santo Andreacute - EUA
bull A Placa do Pacifico tem se movido a uma velocidade meacutedia de 5 cmano
bull nos uacuteltimos 10 milhotildees de anos
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2671
bull
Formaccedilatildeoda lha deSurtsey naIslacircndia em
1963
bullVulcanismo
bullRelevo formado por 6
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2771
bullTimanfaya Lanzarote- Ilhas Canaacuterias
bull Relevo formado por 6
bull anos de erupccedilatildeo
F d d N h A i eacutel V l acirc i
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2871
bullFernando de Noronha Arquipeacutelago Vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2971
A t aacuteli
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3071
Austraacutelia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3171
Faleacutesia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3271
bullErosatildeo Diferencial
bullNiacuteveis com maior
cimentaccedilatildeo
bullShip Rock NovoMeacutexico antigo
cone vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3371
bull Milhotildees de anos de erosatildeo glacial e eoacutelica esculpiram
os profundos vales e os precipiacutecios
bull Badlands Dakota do Sul (EUA)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3471
bullSerra Pelada 1983
bullSerra Pelada atual
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3571
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3771
Ciclo das rochas
Rocha Magmaacutetica
Rocha Metamoacuterfica
Rocha Sedimentar
Magma
Erosatildeo e Sedimentaccedilatildeo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3871
Rochas Magmaacuteticas ou Iacutegneas
bullFormadas pelo resfriamento e solidificaccedilatildeo do magma dentro dacrosta terrestre em profundidade (intrusivas) ou em superfiacutecie(extrusiva)
bullExemplos Granito (intrusiva) Basalto (extrusiva) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3971
Derrame basaacuteltico em Torres- RS
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4071
Rochas Sedimentares
bull Formada a partir de material originado da destruiccedilatildeo erosivade qualquer tipo de rocha material este que deveraacute sertransportado e depositado em um dos muitos ambientes de
sedimentaccedilatildeo da superfiacutecie terrestrebull Na maioria das vezes apresenta-se estratificada
bull Exemplos Argilito arenito siltitoetc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4171
Rochas Metamoacuterficas
bull Formadas por alteraccedilotildees nas antigas condiccedilotildees de
temperatura e pressatildeo das rochas magmaacuteticas ousedimentares que geram instabilidade dosminerais preacute-existentes
bull Dependendo do caso poderaacute ou natildeo mudar acomposiccedilatildeo mineraloacutegica mas a textura mudaobrigatoriamente
bull Exemplos Quartzito (derivada do metamorfismodo arenito) Maacutermore (proveacutem do Calcaacuterio ou doDolomito) Gnaisse (muito parecida com oGranito) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4271
Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4371
Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4471
Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4571
Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4671
Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4771
Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4971
Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5071
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5271
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5371
ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 1971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2271
Exemplos de Dobramentos Modernos
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2371
Divergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2471
bullTriacircngulo de Afar Eritreacuteia -Aacutefrica
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2571
Tangencial ou transformante ou transcorrente
bull Falha de Santo Andreacute - EUA
bull A Placa do Pacifico tem se movido a uma velocidade meacutedia de 5 cmano
bull nos uacuteltimos 10 milhotildees de anos
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2671
bull
Formaccedilatildeoda lha deSurtsey naIslacircndia em
1963
bullVulcanismo
bullRelevo formado por 6
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2771
bullTimanfaya Lanzarote- Ilhas Canaacuterias
bull Relevo formado por 6
bull anos de erupccedilatildeo
F d d N h A i eacutel V l acirc i
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2871
bullFernando de Noronha Arquipeacutelago Vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2971
A t aacuteli
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3071
Austraacutelia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3171
Faleacutesia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3271
bullErosatildeo Diferencial
bullNiacuteveis com maior
cimentaccedilatildeo
bullShip Rock NovoMeacutexico antigo
cone vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3371
bull Milhotildees de anos de erosatildeo glacial e eoacutelica esculpiram
os profundos vales e os precipiacutecios
bull Badlands Dakota do Sul (EUA)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3471
bullSerra Pelada 1983
bullSerra Pelada atual
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3571
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3771
Ciclo das rochas
Rocha Magmaacutetica
Rocha Metamoacuterfica
Rocha Sedimentar
Magma
Erosatildeo e Sedimentaccedilatildeo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3871
Rochas Magmaacuteticas ou Iacutegneas
bullFormadas pelo resfriamento e solidificaccedilatildeo do magma dentro dacrosta terrestre em profundidade (intrusivas) ou em superfiacutecie(extrusiva)
bullExemplos Granito (intrusiva) Basalto (extrusiva) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3971
Derrame basaacuteltico em Torres- RS
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4071
Rochas Sedimentares
bull Formada a partir de material originado da destruiccedilatildeo erosivade qualquer tipo de rocha material este que deveraacute sertransportado e depositado em um dos muitos ambientes de
sedimentaccedilatildeo da superfiacutecie terrestrebull Na maioria das vezes apresenta-se estratificada
bull Exemplos Argilito arenito siltitoetc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4171
Rochas Metamoacuterficas
bull Formadas por alteraccedilotildees nas antigas condiccedilotildees de
temperatura e pressatildeo das rochas magmaacuteticas ousedimentares que geram instabilidade dosminerais preacute-existentes
bull Dependendo do caso poderaacute ou natildeo mudar acomposiccedilatildeo mineraloacutegica mas a textura mudaobrigatoriamente
bull Exemplos Quartzito (derivada do metamorfismodo arenito) Maacutermore (proveacutem do Calcaacuterio ou doDolomito) Gnaisse (muito parecida com oGranito) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4271
Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4371
Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4471
Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4571
Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4671
Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4771
Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4971
Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5071
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5271
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5371
ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2271
Exemplos de Dobramentos Modernos
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2371
Divergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2471
bullTriacircngulo de Afar Eritreacuteia -Aacutefrica
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2571
Tangencial ou transformante ou transcorrente
bull Falha de Santo Andreacute - EUA
bull A Placa do Pacifico tem se movido a uma velocidade meacutedia de 5 cmano
bull nos uacuteltimos 10 milhotildees de anos
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2671
bull
Formaccedilatildeoda lha deSurtsey naIslacircndia em
1963
bullVulcanismo
bullRelevo formado por 6
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2771
bullTimanfaya Lanzarote- Ilhas Canaacuterias
bull Relevo formado por 6
bull anos de erupccedilatildeo
F d d N h A i eacutel V l acirc i
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2871
bullFernando de Noronha Arquipeacutelago Vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2971
A t aacuteli
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3071
Austraacutelia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3171
Faleacutesia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3271
bullErosatildeo Diferencial
bullNiacuteveis com maior
cimentaccedilatildeo
bullShip Rock NovoMeacutexico antigo
cone vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3371
bull Milhotildees de anos de erosatildeo glacial e eoacutelica esculpiram
os profundos vales e os precipiacutecios
bull Badlands Dakota do Sul (EUA)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3471
bullSerra Pelada 1983
bullSerra Pelada atual
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3571
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3771
Ciclo das rochas
Rocha Magmaacutetica
Rocha Metamoacuterfica
Rocha Sedimentar
Magma
Erosatildeo e Sedimentaccedilatildeo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3871
Rochas Magmaacuteticas ou Iacutegneas
bullFormadas pelo resfriamento e solidificaccedilatildeo do magma dentro dacrosta terrestre em profundidade (intrusivas) ou em superfiacutecie(extrusiva)
bullExemplos Granito (intrusiva) Basalto (extrusiva) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3971
Derrame basaacuteltico em Torres- RS
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4071
Rochas Sedimentares
bull Formada a partir de material originado da destruiccedilatildeo erosivade qualquer tipo de rocha material este que deveraacute sertransportado e depositado em um dos muitos ambientes de
sedimentaccedilatildeo da superfiacutecie terrestrebull Na maioria das vezes apresenta-se estratificada
bull Exemplos Argilito arenito siltitoetc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4171
Rochas Metamoacuterficas
bull Formadas por alteraccedilotildees nas antigas condiccedilotildees de
temperatura e pressatildeo das rochas magmaacuteticas ousedimentares que geram instabilidade dosminerais preacute-existentes
bull Dependendo do caso poderaacute ou natildeo mudar acomposiccedilatildeo mineraloacutegica mas a textura mudaobrigatoriamente
bull Exemplos Quartzito (derivada do metamorfismodo arenito) Maacutermore (proveacutem do Calcaacuterio ou doDolomito) Gnaisse (muito parecida com oGranito) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4271
Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4371
Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4471
Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4571
Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4671
Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4771
Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4971
Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5071
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5271
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5371
ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2271
Exemplos de Dobramentos Modernos
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2371
Divergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2471
bullTriacircngulo de Afar Eritreacuteia -Aacutefrica
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2571
Tangencial ou transformante ou transcorrente
bull Falha de Santo Andreacute - EUA
bull A Placa do Pacifico tem se movido a uma velocidade meacutedia de 5 cmano
bull nos uacuteltimos 10 milhotildees de anos
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2671
bull
Formaccedilatildeoda lha deSurtsey naIslacircndia em
1963
bullVulcanismo
bullRelevo formado por 6
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2771
bullTimanfaya Lanzarote- Ilhas Canaacuterias
bull Relevo formado por 6
bull anos de erupccedilatildeo
F d d N h A i eacutel V l acirc i
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2871
bullFernando de Noronha Arquipeacutelago Vulcacircnico
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A t aacuteli
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Austraacutelia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3171
Faleacutesia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3271
bullErosatildeo Diferencial
bullNiacuteveis com maior
cimentaccedilatildeo
bullShip Rock NovoMeacutexico antigo
cone vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3371
bull Milhotildees de anos de erosatildeo glacial e eoacutelica esculpiram
os profundos vales e os precipiacutecios
bull Badlands Dakota do Sul (EUA)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3471
bullSerra Pelada 1983
bullSerra Pelada atual
Placas Tectocircnicas
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httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3571
Placas Tectocircnicas
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Ciclo das rochas
Rocha Magmaacutetica
Rocha Metamoacuterfica
Rocha Sedimentar
Magma
Erosatildeo e Sedimentaccedilatildeo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3871
Rochas Magmaacuteticas ou Iacutegneas
bullFormadas pelo resfriamento e solidificaccedilatildeo do magma dentro dacrosta terrestre em profundidade (intrusivas) ou em superfiacutecie(extrusiva)
bullExemplos Granito (intrusiva) Basalto (extrusiva) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3971
Derrame basaacuteltico em Torres- RS
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4071
Rochas Sedimentares
bull Formada a partir de material originado da destruiccedilatildeo erosivade qualquer tipo de rocha material este que deveraacute sertransportado e depositado em um dos muitos ambientes de
sedimentaccedilatildeo da superfiacutecie terrestrebull Na maioria das vezes apresenta-se estratificada
bull Exemplos Argilito arenito siltitoetc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4171
Rochas Metamoacuterficas
bull Formadas por alteraccedilotildees nas antigas condiccedilotildees de
temperatura e pressatildeo das rochas magmaacuteticas ousedimentares que geram instabilidade dosminerais preacute-existentes
bull Dependendo do caso poderaacute ou natildeo mudar acomposiccedilatildeo mineraloacutegica mas a textura mudaobrigatoriamente
bull Exemplos Quartzito (derivada do metamorfismodo arenito) Maacutermore (proveacutem do Calcaacuterio ou doDolomito) Gnaisse (muito parecida com oGranito) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4271
Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4371
Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4471
Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4571
Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4671
Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4771
Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4971
Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5071
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2271
Exemplos de Dobramentos Modernos
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2371
Divergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2471
bullTriacircngulo de Afar Eritreacuteia -Aacutefrica
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2571
Tangencial ou transformante ou transcorrente
bull Falha de Santo Andreacute - EUA
bull A Placa do Pacifico tem se movido a uma velocidade meacutedia de 5 cmano
bull nos uacuteltimos 10 milhotildees de anos
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2671
bull
Formaccedilatildeoda lha deSurtsey naIslacircndia em
1963
bullVulcanismo
bullRelevo formado por 6
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2771
bullTimanfaya Lanzarote- Ilhas Canaacuterias
bull Relevo formado por 6
bull anos de erupccedilatildeo
F d d N h A i eacutel V l acirc i
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2871
bullFernando de Noronha Arquipeacutelago Vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2971
A t aacuteli
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3071
Austraacutelia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3171
Faleacutesia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3271
bullErosatildeo Diferencial
bullNiacuteveis com maior
cimentaccedilatildeo
bullShip Rock NovoMeacutexico antigo
cone vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3371
bull Milhotildees de anos de erosatildeo glacial e eoacutelica esculpiram
os profundos vales e os precipiacutecios
bull Badlands Dakota do Sul (EUA)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3471
bullSerra Pelada 1983
bullSerra Pelada atual
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3571
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3771
Ciclo das rochas
Rocha Magmaacutetica
Rocha Metamoacuterfica
Rocha Sedimentar
Magma
Erosatildeo e Sedimentaccedilatildeo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3871
Rochas Magmaacuteticas ou Iacutegneas
bullFormadas pelo resfriamento e solidificaccedilatildeo do magma dentro dacrosta terrestre em profundidade (intrusivas) ou em superfiacutecie(extrusiva)
bullExemplos Granito (intrusiva) Basalto (extrusiva) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3971
Derrame basaacuteltico em Torres- RS
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4071
Rochas Sedimentares
bull Formada a partir de material originado da destruiccedilatildeo erosivade qualquer tipo de rocha material este que deveraacute sertransportado e depositado em um dos muitos ambientes de
sedimentaccedilatildeo da superfiacutecie terrestrebull Na maioria das vezes apresenta-se estratificada
bull Exemplos Argilito arenito siltitoetc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4171
Rochas Metamoacuterficas
bull Formadas por alteraccedilotildees nas antigas condiccedilotildees de
temperatura e pressatildeo das rochas magmaacuteticas ousedimentares que geram instabilidade dosminerais preacute-existentes
bull Dependendo do caso poderaacute ou natildeo mudar acomposiccedilatildeo mineraloacutegica mas a textura mudaobrigatoriamente
bull Exemplos Quartzito (derivada do metamorfismodo arenito) Maacutermore (proveacutem do Calcaacuterio ou doDolomito) Gnaisse (muito parecida com oGranito) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4271
Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4371
Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4471
Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4571
Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4671
Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4771
Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4971
Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5071
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5271
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5371
ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2371
Divergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2471
bullTriacircngulo de Afar Eritreacuteia -Aacutefrica
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2571
Tangencial ou transformante ou transcorrente
bull Falha de Santo Andreacute - EUA
bull A Placa do Pacifico tem se movido a uma velocidade meacutedia de 5 cmano
bull nos uacuteltimos 10 milhotildees de anos
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2671
bull
Formaccedilatildeoda lha deSurtsey naIslacircndia em
1963
bullVulcanismo
bullRelevo formado por 6
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2771
bullTimanfaya Lanzarote- Ilhas Canaacuterias
bull Relevo formado por 6
bull anos de erupccedilatildeo
F d d N h A i eacutel V l acirc i
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2871
bullFernando de Noronha Arquipeacutelago Vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2971
A t aacuteli
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3071
Austraacutelia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3171
Faleacutesia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3271
bullErosatildeo Diferencial
bullNiacuteveis com maior
cimentaccedilatildeo
bullShip Rock NovoMeacutexico antigo
cone vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3371
bull Milhotildees de anos de erosatildeo glacial e eoacutelica esculpiram
os profundos vales e os precipiacutecios
bull Badlands Dakota do Sul (EUA)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3471
bullSerra Pelada 1983
bullSerra Pelada atual
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3571
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3771
Ciclo das rochas
Rocha Magmaacutetica
Rocha Metamoacuterfica
Rocha Sedimentar
Magma
Erosatildeo e Sedimentaccedilatildeo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3871
Rochas Magmaacuteticas ou Iacutegneas
bullFormadas pelo resfriamento e solidificaccedilatildeo do magma dentro dacrosta terrestre em profundidade (intrusivas) ou em superfiacutecie(extrusiva)
bullExemplos Granito (intrusiva) Basalto (extrusiva) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3971
Derrame basaacuteltico em Torres- RS
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4071
Rochas Sedimentares
bull Formada a partir de material originado da destruiccedilatildeo erosivade qualquer tipo de rocha material este que deveraacute sertransportado e depositado em um dos muitos ambientes de
sedimentaccedilatildeo da superfiacutecie terrestrebull Na maioria das vezes apresenta-se estratificada
bull Exemplos Argilito arenito siltitoetc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4171
Rochas Metamoacuterficas
bull Formadas por alteraccedilotildees nas antigas condiccedilotildees de
temperatura e pressatildeo das rochas magmaacuteticas ousedimentares que geram instabilidade dosminerais preacute-existentes
bull Dependendo do caso poderaacute ou natildeo mudar acomposiccedilatildeo mineraloacutegica mas a textura mudaobrigatoriamente
bull Exemplos Quartzito (derivada do metamorfismodo arenito) Maacutermore (proveacutem do Calcaacuterio ou doDolomito) Gnaisse (muito parecida com oGranito) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4271
Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4371
Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4471
Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4571
Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4671
Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4771
Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4971
Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5071
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5271
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5371
ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2471
bullTriacircngulo de Afar Eritreacuteia -Aacutefrica
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2571
Tangencial ou transformante ou transcorrente
bull Falha de Santo Andreacute - EUA
bull A Placa do Pacifico tem se movido a uma velocidade meacutedia de 5 cmano
bull nos uacuteltimos 10 milhotildees de anos
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2671
bull
Formaccedilatildeoda lha deSurtsey naIslacircndia em
1963
bullVulcanismo
bullRelevo formado por 6
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2771
bullTimanfaya Lanzarote- Ilhas Canaacuterias
bull Relevo formado por 6
bull anos de erupccedilatildeo
F d d N h A i eacutel V l acirc i
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2871
bullFernando de Noronha Arquipeacutelago Vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2971
A t aacuteli
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3071
Austraacutelia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3171
Faleacutesia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3271
bullErosatildeo Diferencial
bullNiacuteveis com maior
cimentaccedilatildeo
bullShip Rock NovoMeacutexico antigo
cone vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3371
bull Milhotildees de anos de erosatildeo glacial e eoacutelica esculpiram
os profundos vales e os precipiacutecios
bull Badlands Dakota do Sul (EUA)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3471
bullSerra Pelada 1983
bullSerra Pelada atual
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3571
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3771
Ciclo das rochas
Rocha Magmaacutetica
Rocha Metamoacuterfica
Rocha Sedimentar
Magma
Erosatildeo e Sedimentaccedilatildeo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3871
Rochas Magmaacuteticas ou Iacutegneas
bullFormadas pelo resfriamento e solidificaccedilatildeo do magma dentro dacrosta terrestre em profundidade (intrusivas) ou em superfiacutecie(extrusiva)
bullExemplos Granito (intrusiva) Basalto (extrusiva) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3971
Derrame basaacuteltico em Torres- RS
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4071
Rochas Sedimentares
bull Formada a partir de material originado da destruiccedilatildeo erosivade qualquer tipo de rocha material este que deveraacute sertransportado e depositado em um dos muitos ambientes de
sedimentaccedilatildeo da superfiacutecie terrestrebull Na maioria das vezes apresenta-se estratificada
bull Exemplos Argilito arenito siltitoetc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4171
Rochas Metamoacuterficas
bull Formadas por alteraccedilotildees nas antigas condiccedilotildees de
temperatura e pressatildeo das rochas magmaacuteticas ousedimentares que geram instabilidade dosminerais preacute-existentes
bull Dependendo do caso poderaacute ou natildeo mudar acomposiccedilatildeo mineraloacutegica mas a textura mudaobrigatoriamente
bull Exemplos Quartzito (derivada do metamorfismodo arenito) Maacutermore (proveacutem do Calcaacuterio ou doDolomito) Gnaisse (muito parecida com oGranito) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4271
Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4371
Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4471
Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4571
Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4671
Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4771
Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4971
Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5071
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5271
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5371
ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2571
Tangencial ou transformante ou transcorrente
bull Falha de Santo Andreacute - EUA
bull A Placa do Pacifico tem se movido a uma velocidade meacutedia de 5 cmano
bull nos uacuteltimos 10 milhotildees de anos
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2671
bull
Formaccedilatildeoda lha deSurtsey naIslacircndia em
1963
bullVulcanismo
bullRelevo formado por 6
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2771
bullTimanfaya Lanzarote- Ilhas Canaacuterias
bull Relevo formado por 6
bull anos de erupccedilatildeo
F d d N h A i eacutel V l acirc i
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2871
bullFernando de Noronha Arquipeacutelago Vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2971
A t aacuteli
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3071
Austraacutelia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3171
Faleacutesia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3271
bullErosatildeo Diferencial
bullNiacuteveis com maior
cimentaccedilatildeo
bullShip Rock NovoMeacutexico antigo
cone vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3371
bull Milhotildees de anos de erosatildeo glacial e eoacutelica esculpiram
os profundos vales e os precipiacutecios
bull Badlands Dakota do Sul (EUA)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3471
bullSerra Pelada 1983
bullSerra Pelada atual
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3571
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3771
Ciclo das rochas
Rocha Magmaacutetica
Rocha Metamoacuterfica
Rocha Sedimentar
Magma
Erosatildeo e Sedimentaccedilatildeo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3871
Rochas Magmaacuteticas ou Iacutegneas
bullFormadas pelo resfriamento e solidificaccedilatildeo do magma dentro dacrosta terrestre em profundidade (intrusivas) ou em superfiacutecie(extrusiva)
bullExemplos Granito (intrusiva) Basalto (extrusiva) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3971
Derrame basaacuteltico em Torres- RS
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4071
Rochas Sedimentares
bull Formada a partir de material originado da destruiccedilatildeo erosivade qualquer tipo de rocha material este que deveraacute sertransportado e depositado em um dos muitos ambientes de
sedimentaccedilatildeo da superfiacutecie terrestrebull Na maioria das vezes apresenta-se estratificada
bull Exemplos Argilito arenito siltitoetc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4171
Rochas Metamoacuterficas
bull Formadas por alteraccedilotildees nas antigas condiccedilotildees de
temperatura e pressatildeo das rochas magmaacuteticas ousedimentares que geram instabilidade dosminerais preacute-existentes
bull Dependendo do caso poderaacute ou natildeo mudar acomposiccedilatildeo mineraloacutegica mas a textura mudaobrigatoriamente
bull Exemplos Quartzito (derivada do metamorfismodo arenito) Maacutermore (proveacutem do Calcaacuterio ou doDolomito) Gnaisse (muito parecida com oGranito) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4271
Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4371
Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4471
Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4571
Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4671
Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4771
Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4971
Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5071
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5271
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5371
ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2671
bull
Formaccedilatildeoda lha deSurtsey naIslacircndia em
1963
bullVulcanismo
bullRelevo formado por 6
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2771
bullTimanfaya Lanzarote- Ilhas Canaacuterias
bull Relevo formado por 6
bull anos de erupccedilatildeo
F d d N h A i eacutel V l acirc i
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2871
bullFernando de Noronha Arquipeacutelago Vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2971
A t aacuteli
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3071
Austraacutelia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3171
Faleacutesia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3271
bullErosatildeo Diferencial
bullNiacuteveis com maior
cimentaccedilatildeo
bullShip Rock NovoMeacutexico antigo
cone vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3371
bull Milhotildees de anos de erosatildeo glacial e eoacutelica esculpiram
os profundos vales e os precipiacutecios
bull Badlands Dakota do Sul (EUA)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3471
bullSerra Pelada 1983
bullSerra Pelada atual
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3571
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3771
Ciclo das rochas
Rocha Magmaacutetica
Rocha Metamoacuterfica
Rocha Sedimentar
Magma
Erosatildeo e Sedimentaccedilatildeo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3871
Rochas Magmaacuteticas ou Iacutegneas
bullFormadas pelo resfriamento e solidificaccedilatildeo do magma dentro dacrosta terrestre em profundidade (intrusivas) ou em superfiacutecie(extrusiva)
bullExemplos Granito (intrusiva) Basalto (extrusiva) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3971
Derrame basaacuteltico em Torres- RS
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4071
Rochas Sedimentares
bull Formada a partir de material originado da destruiccedilatildeo erosivade qualquer tipo de rocha material este que deveraacute sertransportado e depositado em um dos muitos ambientes de
sedimentaccedilatildeo da superfiacutecie terrestrebull Na maioria das vezes apresenta-se estratificada
bull Exemplos Argilito arenito siltitoetc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4171
Rochas Metamoacuterficas
bull Formadas por alteraccedilotildees nas antigas condiccedilotildees de
temperatura e pressatildeo das rochas magmaacuteticas ousedimentares que geram instabilidade dosminerais preacute-existentes
bull Dependendo do caso poderaacute ou natildeo mudar acomposiccedilatildeo mineraloacutegica mas a textura mudaobrigatoriamente
bull Exemplos Quartzito (derivada do metamorfismodo arenito) Maacutermore (proveacutem do Calcaacuterio ou doDolomito) Gnaisse (muito parecida com oGranito) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4271
Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4371
Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4471
Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4571
Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4671
Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4771
Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4971
Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5071
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5271
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5371
ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2771
bullTimanfaya Lanzarote- Ilhas Canaacuterias
bull Relevo formado por 6
bull anos de erupccedilatildeo
F d d N h A i eacutel V l acirc i
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2871
bullFernando de Noronha Arquipeacutelago Vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2971
A t aacuteli
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3071
Austraacutelia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3171
Faleacutesia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3271
bullErosatildeo Diferencial
bullNiacuteveis com maior
cimentaccedilatildeo
bullShip Rock NovoMeacutexico antigo
cone vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3371
bull Milhotildees de anos de erosatildeo glacial e eoacutelica esculpiram
os profundos vales e os precipiacutecios
bull Badlands Dakota do Sul (EUA)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3471
bullSerra Pelada 1983
bullSerra Pelada atual
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3571
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3771
Ciclo das rochas
Rocha Magmaacutetica
Rocha Metamoacuterfica
Rocha Sedimentar
Magma
Erosatildeo e Sedimentaccedilatildeo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3871
Rochas Magmaacuteticas ou Iacutegneas
bullFormadas pelo resfriamento e solidificaccedilatildeo do magma dentro dacrosta terrestre em profundidade (intrusivas) ou em superfiacutecie(extrusiva)
bullExemplos Granito (intrusiva) Basalto (extrusiva) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3971
Derrame basaacuteltico em Torres- RS
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4071
Rochas Sedimentares
bull Formada a partir de material originado da destruiccedilatildeo erosivade qualquer tipo de rocha material este que deveraacute sertransportado e depositado em um dos muitos ambientes de
sedimentaccedilatildeo da superfiacutecie terrestrebull Na maioria das vezes apresenta-se estratificada
bull Exemplos Argilito arenito siltitoetc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4171
Rochas Metamoacuterficas
bull Formadas por alteraccedilotildees nas antigas condiccedilotildees de
temperatura e pressatildeo das rochas magmaacuteticas ousedimentares que geram instabilidade dosminerais preacute-existentes
bull Dependendo do caso poderaacute ou natildeo mudar acomposiccedilatildeo mineraloacutegica mas a textura mudaobrigatoriamente
bull Exemplos Quartzito (derivada do metamorfismodo arenito) Maacutermore (proveacutem do Calcaacuterio ou doDolomito) Gnaisse (muito parecida com oGranito) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4271
Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4371
Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4471
Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4571
Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4671
Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4771
Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4971
Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5071
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5271
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5371
ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2871
bullFernando de Noronha Arquipeacutelago Vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2971
A t aacuteli
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3071
Austraacutelia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3171
Faleacutesia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3271
bullErosatildeo Diferencial
bullNiacuteveis com maior
cimentaccedilatildeo
bullShip Rock NovoMeacutexico antigo
cone vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3371
bull Milhotildees de anos de erosatildeo glacial e eoacutelica esculpiram
os profundos vales e os precipiacutecios
bull Badlands Dakota do Sul (EUA)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3471
bullSerra Pelada 1983
bullSerra Pelada atual
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3571
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3771
Ciclo das rochas
Rocha Magmaacutetica
Rocha Metamoacuterfica
Rocha Sedimentar
Magma
Erosatildeo e Sedimentaccedilatildeo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3871
Rochas Magmaacuteticas ou Iacutegneas
bullFormadas pelo resfriamento e solidificaccedilatildeo do magma dentro dacrosta terrestre em profundidade (intrusivas) ou em superfiacutecie(extrusiva)
bullExemplos Granito (intrusiva) Basalto (extrusiva) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3971
Derrame basaacuteltico em Torres- RS
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4071
Rochas Sedimentares
bull Formada a partir de material originado da destruiccedilatildeo erosivade qualquer tipo de rocha material este que deveraacute sertransportado e depositado em um dos muitos ambientes de
sedimentaccedilatildeo da superfiacutecie terrestrebull Na maioria das vezes apresenta-se estratificada
bull Exemplos Argilito arenito siltitoetc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4171
Rochas Metamoacuterficas
bull Formadas por alteraccedilotildees nas antigas condiccedilotildees de
temperatura e pressatildeo das rochas magmaacuteticas ousedimentares que geram instabilidade dosminerais preacute-existentes
bull Dependendo do caso poderaacute ou natildeo mudar acomposiccedilatildeo mineraloacutegica mas a textura mudaobrigatoriamente
bull Exemplos Quartzito (derivada do metamorfismodo arenito) Maacutermore (proveacutem do Calcaacuterio ou doDolomito) Gnaisse (muito parecida com oGranito) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4271
Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4371
Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4471
Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4571
Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4671
Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4771
Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4971
Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5071
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5271
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5371
ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 2971
A t aacuteli
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3071
Austraacutelia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3171
Faleacutesia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3271
bullErosatildeo Diferencial
bullNiacuteveis com maior
cimentaccedilatildeo
bullShip Rock NovoMeacutexico antigo
cone vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3371
bull Milhotildees de anos de erosatildeo glacial e eoacutelica esculpiram
os profundos vales e os precipiacutecios
bull Badlands Dakota do Sul (EUA)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3471
bullSerra Pelada 1983
bullSerra Pelada atual
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3571
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3771
Ciclo das rochas
Rocha Magmaacutetica
Rocha Metamoacuterfica
Rocha Sedimentar
Magma
Erosatildeo e Sedimentaccedilatildeo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3871
Rochas Magmaacuteticas ou Iacutegneas
bullFormadas pelo resfriamento e solidificaccedilatildeo do magma dentro dacrosta terrestre em profundidade (intrusivas) ou em superfiacutecie(extrusiva)
bullExemplos Granito (intrusiva) Basalto (extrusiva) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3971
Derrame basaacuteltico em Torres- RS
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4071
Rochas Sedimentares
bull Formada a partir de material originado da destruiccedilatildeo erosivade qualquer tipo de rocha material este que deveraacute sertransportado e depositado em um dos muitos ambientes de
sedimentaccedilatildeo da superfiacutecie terrestrebull Na maioria das vezes apresenta-se estratificada
bull Exemplos Argilito arenito siltitoetc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4171
Rochas Metamoacuterficas
bull Formadas por alteraccedilotildees nas antigas condiccedilotildees de
temperatura e pressatildeo das rochas magmaacuteticas ousedimentares que geram instabilidade dosminerais preacute-existentes
bull Dependendo do caso poderaacute ou natildeo mudar acomposiccedilatildeo mineraloacutegica mas a textura mudaobrigatoriamente
bull Exemplos Quartzito (derivada do metamorfismodo arenito) Maacutermore (proveacutem do Calcaacuterio ou doDolomito) Gnaisse (muito parecida com oGranito) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4271
Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4371
Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4471
Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4571
Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4671
Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4771
Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4971
Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5071
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5271
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5371
ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3071
Austraacutelia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3171
Faleacutesia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3271
bullErosatildeo Diferencial
bullNiacuteveis com maior
cimentaccedilatildeo
bullShip Rock NovoMeacutexico antigo
cone vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3371
bull Milhotildees de anos de erosatildeo glacial e eoacutelica esculpiram
os profundos vales e os precipiacutecios
bull Badlands Dakota do Sul (EUA)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3471
bullSerra Pelada 1983
bullSerra Pelada atual
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3571
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3771
Ciclo das rochas
Rocha Magmaacutetica
Rocha Metamoacuterfica
Rocha Sedimentar
Magma
Erosatildeo e Sedimentaccedilatildeo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3871
Rochas Magmaacuteticas ou Iacutegneas
bullFormadas pelo resfriamento e solidificaccedilatildeo do magma dentro dacrosta terrestre em profundidade (intrusivas) ou em superfiacutecie(extrusiva)
bullExemplos Granito (intrusiva) Basalto (extrusiva) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3971
Derrame basaacuteltico em Torres- RS
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4071
Rochas Sedimentares
bull Formada a partir de material originado da destruiccedilatildeo erosivade qualquer tipo de rocha material este que deveraacute sertransportado e depositado em um dos muitos ambientes de
sedimentaccedilatildeo da superfiacutecie terrestrebull Na maioria das vezes apresenta-se estratificada
bull Exemplos Argilito arenito siltitoetc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4171
Rochas Metamoacuterficas
bull Formadas por alteraccedilotildees nas antigas condiccedilotildees de
temperatura e pressatildeo das rochas magmaacuteticas ousedimentares que geram instabilidade dosminerais preacute-existentes
bull Dependendo do caso poderaacute ou natildeo mudar acomposiccedilatildeo mineraloacutegica mas a textura mudaobrigatoriamente
bull Exemplos Quartzito (derivada do metamorfismodo arenito) Maacutermore (proveacutem do Calcaacuterio ou doDolomito) Gnaisse (muito parecida com oGranito) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4271
Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4371
Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4471
Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4571
Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4671
Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4771
Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4971
Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5071
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5271
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5371
ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3171
Faleacutesia
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3271
bullErosatildeo Diferencial
bullNiacuteveis com maior
cimentaccedilatildeo
bullShip Rock NovoMeacutexico antigo
cone vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3371
bull Milhotildees de anos de erosatildeo glacial e eoacutelica esculpiram
os profundos vales e os precipiacutecios
bull Badlands Dakota do Sul (EUA)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3471
bullSerra Pelada 1983
bullSerra Pelada atual
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3571
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3771
Ciclo das rochas
Rocha Magmaacutetica
Rocha Metamoacuterfica
Rocha Sedimentar
Magma
Erosatildeo e Sedimentaccedilatildeo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3871
Rochas Magmaacuteticas ou Iacutegneas
bullFormadas pelo resfriamento e solidificaccedilatildeo do magma dentro dacrosta terrestre em profundidade (intrusivas) ou em superfiacutecie(extrusiva)
bullExemplos Granito (intrusiva) Basalto (extrusiva) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3971
Derrame basaacuteltico em Torres- RS
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4071
Rochas Sedimentares
bull Formada a partir de material originado da destruiccedilatildeo erosivade qualquer tipo de rocha material este que deveraacute sertransportado e depositado em um dos muitos ambientes de
sedimentaccedilatildeo da superfiacutecie terrestrebull Na maioria das vezes apresenta-se estratificada
bull Exemplos Argilito arenito siltitoetc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4171
Rochas Metamoacuterficas
bull Formadas por alteraccedilotildees nas antigas condiccedilotildees de
temperatura e pressatildeo das rochas magmaacuteticas ousedimentares que geram instabilidade dosminerais preacute-existentes
bull Dependendo do caso poderaacute ou natildeo mudar acomposiccedilatildeo mineraloacutegica mas a textura mudaobrigatoriamente
bull Exemplos Quartzito (derivada do metamorfismodo arenito) Maacutermore (proveacutem do Calcaacuterio ou doDolomito) Gnaisse (muito parecida com oGranito) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4271
Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4371
Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4471
Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4571
Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4671
Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4771
Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4971
Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5071
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5271
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5371
ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3271
bullErosatildeo Diferencial
bullNiacuteveis com maior
cimentaccedilatildeo
bullShip Rock NovoMeacutexico antigo
cone vulcacircnico
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3371
bull Milhotildees de anos de erosatildeo glacial e eoacutelica esculpiram
os profundos vales e os precipiacutecios
bull Badlands Dakota do Sul (EUA)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3471
bullSerra Pelada 1983
bullSerra Pelada atual
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3571
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3771
Ciclo das rochas
Rocha Magmaacutetica
Rocha Metamoacuterfica
Rocha Sedimentar
Magma
Erosatildeo e Sedimentaccedilatildeo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3871
Rochas Magmaacuteticas ou Iacutegneas
bullFormadas pelo resfriamento e solidificaccedilatildeo do magma dentro dacrosta terrestre em profundidade (intrusivas) ou em superfiacutecie(extrusiva)
bullExemplos Granito (intrusiva) Basalto (extrusiva) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3971
Derrame basaacuteltico em Torres- RS
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4071
Rochas Sedimentares
bull Formada a partir de material originado da destruiccedilatildeo erosivade qualquer tipo de rocha material este que deveraacute sertransportado e depositado em um dos muitos ambientes de
sedimentaccedilatildeo da superfiacutecie terrestrebull Na maioria das vezes apresenta-se estratificada
bull Exemplos Argilito arenito siltitoetc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4171
Rochas Metamoacuterficas
bull Formadas por alteraccedilotildees nas antigas condiccedilotildees de
temperatura e pressatildeo das rochas magmaacuteticas ousedimentares que geram instabilidade dosminerais preacute-existentes
bull Dependendo do caso poderaacute ou natildeo mudar acomposiccedilatildeo mineraloacutegica mas a textura mudaobrigatoriamente
bull Exemplos Quartzito (derivada do metamorfismodo arenito) Maacutermore (proveacutem do Calcaacuterio ou doDolomito) Gnaisse (muito parecida com oGranito) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4271
Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4371
Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4471
Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4571
Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4671
Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4771
Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4971
Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5071
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5271
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5371
ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3371
bull Milhotildees de anos de erosatildeo glacial e eoacutelica esculpiram
os profundos vales e os precipiacutecios
bull Badlands Dakota do Sul (EUA)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3471
bullSerra Pelada 1983
bullSerra Pelada atual
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3571
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3771
Ciclo das rochas
Rocha Magmaacutetica
Rocha Metamoacuterfica
Rocha Sedimentar
Magma
Erosatildeo e Sedimentaccedilatildeo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3871
Rochas Magmaacuteticas ou Iacutegneas
bullFormadas pelo resfriamento e solidificaccedilatildeo do magma dentro dacrosta terrestre em profundidade (intrusivas) ou em superfiacutecie(extrusiva)
bullExemplos Granito (intrusiva) Basalto (extrusiva) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3971
Derrame basaacuteltico em Torres- RS
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4071
Rochas Sedimentares
bull Formada a partir de material originado da destruiccedilatildeo erosivade qualquer tipo de rocha material este que deveraacute sertransportado e depositado em um dos muitos ambientes de
sedimentaccedilatildeo da superfiacutecie terrestrebull Na maioria das vezes apresenta-se estratificada
bull Exemplos Argilito arenito siltitoetc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4171
Rochas Metamoacuterficas
bull Formadas por alteraccedilotildees nas antigas condiccedilotildees de
temperatura e pressatildeo das rochas magmaacuteticas ousedimentares que geram instabilidade dosminerais preacute-existentes
bull Dependendo do caso poderaacute ou natildeo mudar acomposiccedilatildeo mineraloacutegica mas a textura mudaobrigatoriamente
bull Exemplos Quartzito (derivada do metamorfismodo arenito) Maacutermore (proveacutem do Calcaacuterio ou doDolomito) Gnaisse (muito parecida com oGranito) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4271
Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4371
Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4471
Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4571
Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4671
Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4771
Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4971
Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5071
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5271
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5371
ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3471
bullSerra Pelada 1983
bullSerra Pelada atual
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3571
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3771
Ciclo das rochas
Rocha Magmaacutetica
Rocha Metamoacuterfica
Rocha Sedimentar
Magma
Erosatildeo e Sedimentaccedilatildeo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3871
Rochas Magmaacuteticas ou Iacutegneas
bullFormadas pelo resfriamento e solidificaccedilatildeo do magma dentro dacrosta terrestre em profundidade (intrusivas) ou em superfiacutecie(extrusiva)
bullExemplos Granito (intrusiva) Basalto (extrusiva) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3971
Derrame basaacuteltico em Torres- RS
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4071
Rochas Sedimentares
bull Formada a partir de material originado da destruiccedilatildeo erosivade qualquer tipo de rocha material este que deveraacute sertransportado e depositado em um dos muitos ambientes de
sedimentaccedilatildeo da superfiacutecie terrestrebull Na maioria das vezes apresenta-se estratificada
bull Exemplos Argilito arenito siltitoetc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4171
Rochas Metamoacuterficas
bull Formadas por alteraccedilotildees nas antigas condiccedilotildees de
temperatura e pressatildeo das rochas magmaacuteticas ousedimentares que geram instabilidade dosminerais preacute-existentes
bull Dependendo do caso poderaacute ou natildeo mudar acomposiccedilatildeo mineraloacutegica mas a textura mudaobrigatoriamente
bull Exemplos Quartzito (derivada do metamorfismodo arenito) Maacutermore (proveacutem do Calcaacuterio ou doDolomito) Gnaisse (muito parecida com oGranito) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4271
Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4371
Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4471
Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4571
Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4671
Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4771
Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4971
Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5071
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5271
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5371
ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3571
Placas Tectocircnicas
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3771
Ciclo das rochas
Rocha Magmaacutetica
Rocha Metamoacuterfica
Rocha Sedimentar
Magma
Erosatildeo e Sedimentaccedilatildeo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3871
Rochas Magmaacuteticas ou Iacutegneas
bullFormadas pelo resfriamento e solidificaccedilatildeo do magma dentro dacrosta terrestre em profundidade (intrusivas) ou em superfiacutecie(extrusiva)
bullExemplos Granito (intrusiva) Basalto (extrusiva) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3971
Derrame basaacuteltico em Torres- RS
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4071
Rochas Sedimentares
bull Formada a partir de material originado da destruiccedilatildeo erosivade qualquer tipo de rocha material este que deveraacute sertransportado e depositado em um dos muitos ambientes de
sedimentaccedilatildeo da superfiacutecie terrestrebull Na maioria das vezes apresenta-se estratificada
bull Exemplos Argilito arenito siltitoetc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4171
Rochas Metamoacuterficas
bull Formadas por alteraccedilotildees nas antigas condiccedilotildees de
temperatura e pressatildeo das rochas magmaacuteticas ousedimentares que geram instabilidade dosminerais preacute-existentes
bull Dependendo do caso poderaacute ou natildeo mudar acomposiccedilatildeo mineraloacutegica mas a textura mudaobrigatoriamente
bull Exemplos Quartzito (derivada do metamorfismodo arenito) Maacutermore (proveacutem do Calcaacuterio ou doDolomito) Gnaisse (muito parecida com oGranito) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4271
Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4371
Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4471
Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4571
Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4671
Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4771
Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4971
Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5071
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5271
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5371
ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3771
Ciclo das rochas
Rocha Magmaacutetica
Rocha Metamoacuterfica
Rocha Sedimentar
Magma
Erosatildeo e Sedimentaccedilatildeo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3871
Rochas Magmaacuteticas ou Iacutegneas
bullFormadas pelo resfriamento e solidificaccedilatildeo do magma dentro dacrosta terrestre em profundidade (intrusivas) ou em superfiacutecie(extrusiva)
bullExemplos Granito (intrusiva) Basalto (extrusiva) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3971
Derrame basaacuteltico em Torres- RS
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4071
Rochas Sedimentares
bull Formada a partir de material originado da destruiccedilatildeo erosivade qualquer tipo de rocha material este que deveraacute sertransportado e depositado em um dos muitos ambientes de
sedimentaccedilatildeo da superfiacutecie terrestrebull Na maioria das vezes apresenta-se estratificada
bull Exemplos Argilito arenito siltitoetc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4171
Rochas Metamoacuterficas
bull Formadas por alteraccedilotildees nas antigas condiccedilotildees de
temperatura e pressatildeo das rochas magmaacuteticas ousedimentares que geram instabilidade dosminerais preacute-existentes
bull Dependendo do caso poderaacute ou natildeo mudar acomposiccedilatildeo mineraloacutegica mas a textura mudaobrigatoriamente
bull Exemplos Quartzito (derivada do metamorfismodo arenito) Maacutermore (proveacutem do Calcaacuterio ou doDolomito) Gnaisse (muito parecida com oGranito) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4271
Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4371
Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4471
Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4571
Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4671
Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4771
Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4971
Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5071
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5271
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5371
ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3771
Ciclo das rochas
Rocha Magmaacutetica
Rocha Metamoacuterfica
Rocha Sedimentar
Magma
Erosatildeo e Sedimentaccedilatildeo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3871
Rochas Magmaacuteticas ou Iacutegneas
bullFormadas pelo resfriamento e solidificaccedilatildeo do magma dentro dacrosta terrestre em profundidade (intrusivas) ou em superfiacutecie(extrusiva)
bullExemplos Granito (intrusiva) Basalto (extrusiva) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3971
Derrame basaacuteltico em Torres- RS
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4071
Rochas Sedimentares
bull Formada a partir de material originado da destruiccedilatildeo erosivade qualquer tipo de rocha material este que deveraacute sertransportado e depositado em um dos muitos ambientes de
sedimentaccedilatildeo da superfiacutecie terrestrebull Na maioria das vezes apresenta-se estratificada
bull Exemplos Argilito arenito siltitoetc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4171
Rochas Metamoacuterficas
bull Formadas por alteraccedilotildees nas antigas condiccedilotildees de
temperatura e pressatildeo das rochas magmaacuteticas ousedimentares que geram instabilidade dosminerais preacute-existentes
bull Dependendo do caso poderaacute ou natildeo mudar acomposiccedilatildeo mineraloacutegica mas a textura mudaobrigatoriamente
bull Exemplos Quartzito (derivada do metamorfismodo arenito) Maacutermore (proveacutem do Calcaacuterio ou doDolomito) Gnaisse (muito parecida com oGranito) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4271
Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4371
Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4471
Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4571
Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4671
Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4771
Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4971
Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5071
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5271
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5371
ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3871
Rochas Magmaacuteticas ou Iacutegneas
bullFormadas pelo resfriamento e solidificaccedilatildeo do magma dentro dacrosta terrestre em profundidade (intrusivas) ou em superfiacutecie(extrusiva)
bullExemplos Granito (intrusiva) Basalto (extrusiva) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3971
Derrame basaacuteltico em Torres- RS
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4071
Rochas Sedimentares
bull Formada a partir de material originado da destruiccedilatildeo erosivade qualquer tipo de rocha material este que deveraacute sertransportado e depositado em um dos muitos ambientes de
sedimentaccedilatildeo da superfiacutecie terrestrebull Na maioria das vezes apresenta-se estratificada
bull Exemplos Argilito arenito siltitoetc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4171
Rochas Metamoacuterficas
bull Formadas por alteraccedilotildees nas antigas condiccedilotildees de
temperatura e pressatildeo das rochas magmaacuteticas ousedimentares que geram instabilidade dosminerais preacute-existentes
bull Dependendo do caso poderaacute ou natildeo mudar acomposiccedilatildeo mineraloacutegica mas a textura mudaobrigatoriamente
bull Exemplos Quartzito (derivada do metamorfismodo arenito) Maacutermore (proveacutem do Calcaacuterio ou doDolomito) Gnaisse (muito parecida com oGranito) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4271
Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4371
Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4471
Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4571
Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4671
Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4771
Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4971
Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5071
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5271
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5371
ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 3971
Derrame basaacuteltico em Torres- RS
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4071
Rochas Sedimentares
bull Formada a partir de material originado da destruiccedilatildeo erosivade qualquer tipo de rocha material este que deveraacute sertransportado e depositado em um dos muitos ambientes de
sedimentaccedilatildeo da superfiacutecie terrestrebull Na maioria das vezes apresenta-se estratificada
bull Exemplos Argilito arenito siltitoetc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4171
Rochas Metamoacuterficas
bull Formadas por alteraccedilotildees nas antigas condiccedilotildees de
temperatura e pressatildeo das rochas magmaacuteticas ousedimentares que geram instabilidade dosminerais preacute-existentes
bull Dependendo do caso poderaacute ou natildeo mudar acomposiccedilatildeo mineraloacutegica mas a textura mudaobrigatoriamente
bull Exemplos Quartzito (derivada do metamorfismodo arenito) Maacutermore (proveacutem do Calcaacuterio ou doDolomito) Gnaisse (muito parecida com oGranito) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4271
Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4371
Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4471
Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4571
Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4671
Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4771
Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4971
Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5071
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5271
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5371
ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4071
Rochas Sedimentares
bull Formada a partir de material originado da destruiccedilatildeo erosivade qualquer tipo de rocha material este que deveraacute sertransportado e depositado em um dos muitos ambientes de
sedimentaccedilatildeo da superfiacutecie terrestrebull Na maioria das vezes apresenta-se estratificada
bull Exemplos Argilito arenito siltitoetc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4171
Rochas Metamoacuterficas
bull Formadas por alteraccedilotildees nas antigas condiccedilotildees de
temperatura e pressatildeo das rochas magmaacuteticas ousedimentares que geram instabilidade dosminerais preacute-existentes
bull Dependendo do caso poderaacute ou natildeo mudar acomposiccedilatildeo mineraloacutegica mas a textura mudaobrigatoriamente
bull Exemplos Quartzito (derivada do metamorfismodo arenito) Maacutermore (proveacutem do Calcaacuterio ou doDolomito) Gnaisse (muito parecida com oGranito) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4271
Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4371
Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4471
Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4571
Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4671
Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4771
Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4971
Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5071
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5271
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5371
ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4171
Rochas Metamoacuterficas
bull Formadas por alteraccedilotildees nas antigas condiccedilotildees de
temperatura e pressatildeo das rochas magmaacuteticas ousedimentares que geram instabilidade dosminerais preacute-existentes
bull Dependendo do caso poderaacute ou natildeo mudar acomposiccedilatildeo mineraloacutegica mas a textura mudaobrigatoriamente
bull Exemplos Quartzito (derivada do metamorfismodo arenito) Maacutermore (proveacutem do Calcaacuterio ou doDolomito) Gnaisse (muito parecida com oGranito) etc
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4271
Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4371
Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4471
Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4571
Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4671
Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4771
Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4971
Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5071
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5271
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5371
ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4271
Descontinuidades siacutesmicas
bullSatildeo locais onde haacute mudanccedila raacutepida navelocidade da propagaccedilatildeo da onda
siacutesmica revelando a existecircncia dematerial rochoso diferenciado
bullProvam que a Terra eacute constituiacuteda de
vaacuterias capas concecircntricas de materiaisdiferentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4371
Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4471
Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4571
Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4671
Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4771
Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4971
Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5071
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5271
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5371
ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4371
Manto
bullEncontra-se em estado pastoso oumagmaacuteticobullO material que o forma move-se segundo
ceacutelulas de convecccedilatildeobullO manto superior eacute responsaacutevel pelasgrandes perturbaccedilotildees verificadas na
crostabullPerfaz 683 da massa da Terra
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4471
Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4571
Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4671
Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4771
Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4971
Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5071
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5271
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5371
ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4471
Nuacutecleos interno e externo
bullSatildeo constituiacutedos por niacutequel e ferrobullPor estar sob pressotildees 3 milhotildees de vezesmaiores que as observadas ao niacutevel do mar o
nuacutecleo interno encontra-se em estado soacutelidobullTemperatura do centro da Terra eacute de cerca de6000 ordmC
bullO nuacutecleo externo provavelmente encontra-seem estado liacutequido
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4571
Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4671
Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4771
Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4971
Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5071
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5271
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5371
ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4571
Correntes de Convecccedilatildeo
bull Movimentaccedilatildeo do magmamotivada por diferenccedilasteacutermicas em um meiosoacutelido poreacutem dotado de
plasticidade com elevadograu de viscosidade (mantosuperior)
bull Satildeo responsaacuteveis pela
movimentaccedilatildeo doscontinentes
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4671
Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4771
Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4971
Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5071
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5271
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5371
ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4671
Relevo brasileiro
bull Desgastado e aplainado pela erosatildeo
bull Baixa altimetria e formas suaves earredondadas
bull Segundo a classificaccedilatildeo de Jurandyr Ross haacute opredomiacutenio de planaltos e depressotildees e a splaniacutecies limitam-se aos vales dos rios e agravesaacutereas litoracircneas
bull Obs Existem outras classificaccedilotildees do relevobrasileiro Aroldo Azevedo e Aziz AbrsquoSaber
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4771
Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4971
Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5071
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5271
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5371
ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4771
Planaltos
Aacutereas com superfiacutecies irregulares serraschapadas e morros onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(mais de 300 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4971
Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5071
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5271
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5371
ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4871
Depressotildees
Superfiacutecies suavemente inclinadas e bastanteaplainadas onde o processo de erosatildeo
predomina sobre a deposiccedilatildeo de sedimentos(entre 100 e 500 metros)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4971
Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5071
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5271
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5371
ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 4971
Planiacutecies
Superfiacutecies aplainadas onde a sedimentaccedilatildeopredomina sobre a erosatildeo
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5071
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5271
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5371
ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5071
Classificaccedilatildeo de Jurandyr Ross
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5271
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5371
ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5271
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5371
ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5271
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5371
ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5371
ldquoMares de morrosrdquo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5471
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5571
ldquoMares de morrosrdquo
Meacutedio vale do rio Paraiacuteba do Sul (Bananal - SP)
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5671
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5771
Fiordes
Corredores estreitos e profundos numlitoral alto cavados pela erosatildeo glaciaacuteria
que estatildeo hoje submersos invadidos pelomar
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5871
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 5971
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6071
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7171
Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6171
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6271
Cachoeira do Veacuteu da Noiva ndash Chapada dos GuimaratildeesMT
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6371
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6471
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6571Derrames Basaacutelticos no Brasil
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6671
Fonte SILVA Wagner Augusto da Geografia do Brasil e Geral povos e territoacuterios Satildeo Paulo Escala Educacional 2005 p32
Convergente
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6771
Co ve ge te
Formaccedilatildeo do petroacuteleo
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6871
ccedil p
Formaccedilatildeo do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 6971
ccedil
Estaacutegios do carvatildeo mineral
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
httpslidepdfcomreaderfullaula-1-wwwyoutubecomwatchv1kiwr1jlonsfeaturerelated 7071
g
E t atilde d atilde i l P d atilde d atilde t l
5132018 Aula-1 Wwwyoutubecomwatchv=1KiWr1JlonsampFeature=Related - slidepdfcom
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Extraccedilatildeo de carvatildeo mineral Produccedilatildeo de carvatildeo vegetal
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