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8/17/2019 geogrplat l2
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Burning and Melting of rocks
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Divergent BoundaryPlate Interactions
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• Ascending limb ofconvection current– below O /C
• Below ocean – MO
• Below continent –rift valley! nascent
sea
Divergent Plate Boundary
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Oceanic crust - MORContinental crust
Divergent Plate Boundary
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ift valley
P"ases of Divergent continentalcrust
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P"ases of Divergent continentalcrust
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#"e $reat African rift valley
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ed sea – %ascent sea
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Africa after &' ml years
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(not of Plates
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(not of )lates
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*akes and %ile river +African riftvalley
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African lakes
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iver %ile
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• ,rom -'&& on Blue %ile
• Africa.s largest"ydroelectric dam
• gy)t to lose water
s"are 0 "ydroelectricity from Aswan
• gy)t s"owedreservation but t"io)iadid not )ay "eed
• gy)t ready for militaryintervention
• Britis" treaties betweengy)t and 1udan
$rand enaissance dam! t"io)ia
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• %ubian desert
• astern desert
• %amib desert
• *ake 2ictoria• *ake Malawi
• *ake #urkana
•*ake c"ad
• iver Congo
• iver %iger
• Mt3 (iliman4aro
•
(atanga )lateau• $rain coast
• Ivory coast
• $old coast
• 1lave coast
• Darfur
*ocations in Africa
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Prelims -'''
53 6"ic" one of t"efollowing lakes form aninternational boundarybetween #an7ania and
8ganda9a: C"ad
b: Malawi
c: 2ictoria
d: ;ambe7i
8P1C
5uestion
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O+OConvergent Plate Boundary
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O+O convergence
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• Islands in 1
Asia• Indo+ Austral
)late and
urasian )latemovement
• 2olcano 0 5
Island Arc
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Mains
-'&<
53 =)lain t"eformation of t"ousandsof islands in Indonesiaand P"ili))ines
arc"i)elago9 >&':
8P1C
5uestion
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Islands of 1out" ast Asia
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Islands of Indian Ocean
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O+OConvergent Plate Boundary
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O+C convergence
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?3
• Andes !ockies!Atlas
mountain• ,rom Andes
@andesitic
rocks
• 2olcano 0
5
2olcanic Mountains
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Andes mountain range
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• Atacama desert
• Bolivian )lateau
•
*ake #iticaca• Mt3 Aconcagua >"ig"est )eak:
• Mt3 Coto)a=i
•
Mt3 C"imbra7o• *ake Maracaibo
*ocation near Andes
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ockies mountain range
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$rand canyon – Colorado river
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• Columbia +snake )lateau
• $rand canyon /Colorado )lateau
•
Deat" valley• $reat salt lake
• Mt3*ogan >"ig"est )eak of rockies:
•
Mt3 Mckinley >"ig"est )eak of %3America: in Alaskan range
*ocations near ockies
5 ti
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Prelims -''
53 6"ere is t"e volcanicmountain3 Mount3 1t3elens is located9
a: C"ileb: a)an
c: P"ili))inesd: 81A
Ans3 D:
8P1C
5uestion
5 ti
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Mains-'&<
53 w"y are t"e world.sfold mountain systemslocated along t"emargins of continents9
Bring out t"eassociation betweenglobal distribution of
fold +mountains andeart"Euakes and
volcanoes >&':
8P1C
5uestion
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O+OConvergent Plate Boundary
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C+C convergence
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1. O-C convergence2. C-C convergence
imalayan formation
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(arakoram range
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Al)s mountain range
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P"ysical ma) of uro)e
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Bos)orus strait
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City River
Paris 1eine
,rankfurt "ine
2enice Po2ienna!Buda)est!Belgrade
Danube
(iev Dniester
Berlin lbe
Cities of uro)e
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• iversF "one! Danube and Po
• Black forest mountains
• mountainsF Pyrenees! A)ennines
• Islands of Mediterranean seaFBalearic! 1ardinia! Corsica! 1icily!Malta! Cy)rus
• 1traitsF Bonifacio! Messina! Marmara
• 1eaF #yrr"enian! Adriatic! Ionian andAegean
*ocations near Al)s
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• 6"en two )latessli) )ass+oG eac"
ot"er• %o mountains but
seismic activity
• 1an Andreas fault
in California! 81A
#ransform Boundary
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Plate movement
San Andreas fault,
USA
1an Andreas fault
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• arly atmos)"ere –t"in layer of ! e
• %umerous
meteorites attackon eart"
• Break t"e surface
• 8nderlying lava
eru)tion
• ,irst oceanic crustformed
Meteorite Im)act t"eory
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Continental driftH #"eories
5uestio
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Prelims -'&&
53 Between India andast Asia! t"e
navigation time anddistance can be greatly
reduced by w"ic" of t"efollowing9
a: Dee)ening Malacca
strait betweenIndonesia and
Malaysia
8P1C
5uestion
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*andforms on eart"
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#y)es of mountains
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,old mountains
$eomor
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Mountains createddue to convergent
boundaries of bot"
&: O+C >ockies! Andes:
-: C+C >imalayas!Al)s:
Com)ressive forces of)lates
) oungest mountains
on eart"
,old
mountains
$eomor)"
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&:=tensive mountain c"ain
H: $reat "eig"ts
C+C:
C"aracteristics of ,old mountains
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•
Pull ofdescending limbof convectioncurrent
• great )ressureof com)ressiveforce e=erted byt"e convectioncells
P"ases of mountain building
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• longated! narrow
de)ression oncontinentalmargins
• ere sedimentsfrom bot" landand oceanaccumulate
•
8nder intense)ressure!sediments of geo+syncline folded
$eo+syncline
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• 1ediments fromcontinentalcrusts of bot")lates 0 geo+
syncline folded• Because of
sediments of
geo+syncline –marine origin
C+C collision
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,old mountains of t"e world
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&: Alaska range
-: ockies
H: Andes
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• understanding of t"e origin andevolution of eart".s crust3
• At t"e time of t"e formation of t"e
eart" crust! Nrst basaltic crust of ocean+ breaking and melting + a lig"tercontinental crust develo)ed3
•
collide wit" one anot"er @ a largerland mass3
• #"e 4oints @ fold+mountains3
Im)ortance of mountain building
)rocess
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#y)es of mountains
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Block mountains formation
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Block mountains formation
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• ,ault+block mt3
• Due to forces wit"ininterior of t"e eart"
•
8)lifted )art @ "orst• de)ressed )art @
$rabben
• orst @ block
mountains• $rabben @ rift
valley
Block mountains
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uro!e
"ndia
=am)le of block mountains
• a se and i
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MeaningF
#able land!
u)land!"ig"er t"an
surroundingareas
duringmountainsbuilding)rocess
•rodedmountains
• roded dueto glaciers
• De)osition
from lava
Plateaus
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"ntermontane !lateau
• Bolivia )lateau
• #ibetan )lateau• Columbia )lateau
• Colorado )lateau
• Anatolia Plateau>#urkey:
• Deccan )lateau
• (atanga )lateau• O7ark )lateau>81A:
• t"io)ian"ig"land
Continental !lateau
#y)es of )lateau
$
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#lacial
!lateau
• $ra"wal
)lateau• *aurentian
)lateau>Canada:
• Columbia+
snake)lateau
>81A:• DeccanPlateau
• 1"an)lateau
$ava!lateau
#y)es of Plateau
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• Origin of iverCongo and;ambe7i
•
Dense eEuatorialforest
• (nown forresources
+ $old! diamonds!Co))er
(atanga Plateau
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• $ranite• *ess mobile!
cannotmoveu)ward
• Backbone offold
mountains
Bat"olit"
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Plains
• Meaning
• ,lat areas wit" low"eig"ts
•Best for "uman"abitation
• Most )o)ulatedareas of t"e world –
alluvial )lains ofrivers
• De)ositional )lains
+ ivers
+ 1ea >sub+mergedcoast:
•
rosional )lains+ rosion of )lateau
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Asia ur
o!e
Afri
ca
Sout
%America
&ort%
America
Indus Danu
be
%ile Ama7
on
Mississi))i –
Missouri$anga –Bra"ma)utra
"ine Congo
Parana+Paraguay
Colorado
angt7e>C"ina:
"one
%iger 1t3 *awrence
wang e>C"ina:
Po ;ambe7i
ukon
+
Im)ortant river basins of t"e world
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angt7e river! C"ina
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• %avigable river – H of C"ina.s )o)ulation
• 1ic"uan basin – rice cultivation
• 1"ang"ai – biggest )ort of C"ina
• 6u"an – Iron and steel
• %an4ing – te=tile! iron and steel
• C"engdu – oil and gas
• #"ree gorge dam
• un "o canal – connect angt7e wit" wange
Im)ortant locations
" i i i
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u)"rates+ #igris river! IraE
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• *ake 2an!
• *ake 8rmia
• Im)ortant centers in IraEF
• Bag"dad! Mosul! (irkuk! Al Basra
*ocations near u)"rates+#igris
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Ama7on river! Bra7il
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• *argest! -nd longest river
• 1elvas – eEuatorial rain forest
• #in! rubber in 1elvas
• 1ertao – ranc"ing region
• Petroleum reserve at t"e mout"
•
Manaus – Iron ore! navigable• )lateau of Mato $rasso – gold
reserve
*ocations near Ama7on river
i i i i
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Mississi))i ! 81A
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• #em)erate grasslands – Prairies
• 6"eat! corn and cotton cultivation
• Im)ortant citesF
• (ansas – agriculture
• 1t3 Pittsburg – iron and steel
•
%ew Orleans – )ort! s"i) building
*ocations near Mississi))i basin
li b i li
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Murray+Darling basin! Australia
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• #em)erate grassland – downs
• 6"eat cultivation
• 1"ee) rearing !Animal "usbandry
• 6ool and dairy )roduction
*ocation near Murray+darling basin
Continental drift t"eory
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Continental drift t"eory+ sea+oor s)reading
t"eory + )late tectonict"eory
*andforms on eart"Mountains >fold and
block:Plateaus