'3f}i tineri, de \plain\par \pard\sl-768 \li544 \ri1241 \expndtw-11
\f10 \fs64 încre{\f63 \u539\'3f}ire, forma {\f63 \u539\'3f}i în
orogeneza alpino- \plain\par \pard\sl-760 \li544 \ri190 \expndtw-14
\f10 \fs64 carpato-himalayan{\f63 \u259\' 3f}, acum aproximativ 70
\plain\par \pard\sl-775 \li544 \ri760 \expndtw-13 \f10 \fs64 - 85
de milioane de ani. Mun{\ f63 \u539\'3f}ii C{\f63 \u259\'3f}limani
\plain\par \pard\sl-760 \li544 \ri25 \expndtw-12 \f10 \fs64 sunt de
origine vulcanic{\f63 \ u259\'3f}, cel mai înalt vârf \plain\par
\pard\sl-765 \li544 \ri791 \expndtw-10 \f10 \fs64 al lor fiind,
cu\b 2100 m\b0 ,\b Vârful Pietrosul \plain\expndtw-31 \b \f10 \fs64
C{\f63 \u259\'3f}limanilor\b0 .
\par \sect\sectd\sbkpage\margtsxn220\pard
\jexpand\viewkind1\paperw14400\paperh10800 {\shp
{\*\shpinst\shpleft0\shptop0\shpright14400\shpbottom10800
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{\sp{\sn shapeType}{\sv 75}} {\sp{\sn pib}{\sv
{\pict\jpegblip\picw720 \pich540 \picwgoal14400 \pichgoal10800
\picscalex100 \picscaley100
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n\b0 {\f63 \u539\'3f}\b ii C{\f63 \u259\'3f}limani
\par \plain\sl-184\fs18\par\sl-240\fs24\par\pard\pard\sl-383 \li4
\ri409 \expndtw-7 { \f0\fs47 \bullet } \plain\tx541 \tab \expndtw-5
\f10 \fs31 Apar{\f63 \u539\'3f}in lan{\f63 \u539\'3 f}ului vulcanic
ce c{\f63 \u259\'3f}ptu{\f63 \u537\'3f}e{\f63 \u537\'3f}te latur a
intern{\f63 \u259\'3f} a Carpa{\f63 \u539\'3f}ilor Orientali,
situat în \plain\par \sl-269\fs27\par\pard\pard\sl-374 \li544
\ri1205 \expndtw-4 \f10 \fs31 zona de c ontact a mun{\f63
\u539\'3f}ilor de încre{\f63 \u539\'3f}ire cu marile depresiuni de
pr{\f63 \u259\'3f}bu{\f63 \u537\'3f}ire ale \plain\par
\sl-279\fs28\par\pard\pard\sl-374 \li544 \ri293 \expndtw-3 \f10
\fs31 Transilvan iei {\f63 \u537\'3f}i Pannoniei. C{\f63
\u259\'3f}limanul (inclusiv Gurghiu {\f6 3 \u537\'3f}i Harghita) se
încadreaz{\f63 \u259\'3f} în \plain\par
\sl-278\fs28\par\pard\pard\sl-374 \li544 \ri175 \expndtw-4 \f10
\fs31 grupa sudi c{\f63 \u259\'3f} a celor mai tineri mun{\f63
\u539\'3f}i din România, cu cratere stinse acum circa 1,8 -
\plain\par \sl-88\fs9\par\sl-240\fs24\par\pard\pard\sl-319 \li544
\ri197 \expndtw-3 \f10 \f s31 5 milioane de ani (Cuaternarul
inferior), care s-au format în Pliocenul superi or (finele
\plain\par \sl-283\fs28\par\pard\pard\sl-374 \li544 \ri874
\expndtw-5 \f10 \fs31 Neogenului -Ter{\f63 \u539\'3f}iar). Intensa
activitate vulcanic{\f63 \u259\'3f} neogen{\f6 3 \u259\'3f} a dus
la apari{\f63 \u539\'3f}ia unor \plain\par
\sl-279\fs28\par\pard\pard\sl-374 \li544 \ri442 \expndtw-5 \f10
\fs31 imense acu mul{\f63 \u259\'3f}ri de lav{\f63 \u259\'3f}
desf{\f63 \u259\'3f}{\f63 \u537\'3f }urate pe o lungime de 450 km
(dintre care 375 pe \plain\par \sl-278\fs28\par\pard\pard\sl-374
\li544 \ri1438 \expndtw-3 \f10 \fs31 teritoriu l României).
Constituit din alternan{\f63 \u539\'3f}e de lave, aglomerate {\f63
\u 537\'3f}i cenu{\f63 \u537\'3f}{\f63 \u259\'3f} \plain\par
\sl-278\fs28\par\pard\pard\sl-374 \li544 \ri35 \expndtw-6 \f10
\fs31 (stratovulc an), C{\f63 \u259\'3f}limanul apar{\f63
\u539\'3f}ine grupei sudice - cea mai im portant{\f63 \u259\'3f}
mas{\f63 \u259\'3f} vulcanic{\f63 \u259\'3f} \plain\par
\sl-279\fs28\par\pard\pard\sl-374 \li544 \ri538 \expndtw-3 \f10
\fs31 - cu o sup rafa{\f63 \u539\'3f}{\f63 \u259\'3f} de
aproximativ 6.400 km², cu l{\f63 \u259\'3f }{\f63 \u539\'3f}imea de
circa 40 km (peste 50 în \plain\par
\sl-278\fs28\par\pard\pard\sl-374 \li544 \ri270 \expndtw-4 \f10
\fs31 sectorul C {\f63 \u259\'3f}limanului) {\f63 \u537\'3f}i
lungimea de aproape 160 km. Acest m asiv este caracterizat
\plain\par \sl-278\fs28\par\pard\pard\sl-374 \li544 \ri20
\expndtw-4 \f10 \fs31 prin prezen {\f63 \u539\'3f}a celor mai mari
altitudini (Pietrosul C{\f63 \u259\'3f}limanulu i - 2100 m, Gurghiu
- 1776 \plain\par \sl-278\fs28\par\pard\pard\sl-374 \li544 \ri1099
\expndtw-5 \f10 \fs31 m, Harghi ta - 1800 m), care coboar{\f63
\u259\'3f} treptat c{\f63 \u259\'3f}tre Tu{\f63 \ u537\'3f}nad
(Ciomatu - 1.301 m
\par \sect\sectd\sbkpage\margtsxn520\pard
\jexpand\viewkind1\paperw14400\paperh10800
3 \u537\'3f}i de mun{\f63 \u539\'3f}ii Giurgeului (sud-est); la sud
- defileul \plain\par \pard\sl-503 \li544 \ri286 \expndtw-5 \f10
\fs42 Mure{\f63 \u537\'3f}ului consti tuie limita spre mun{\f63
\u539\'3f}ii vulcanici ai Gurghiului; în \plain\expndtw-6 \f10
\fs42 vest - piemontul colinar al C{\f63 \u259\'3f}limanul ui face
trecerea spre partea \plain\par \pard\sl-509 \li544 \ri372
\expndtw-8 \f10 \fs42 estic{\f63 \u259\'3f} a Podi{\f 63
\u537\'3f}ului Transilvaniei. Limita septentrional{\f63 \u259\'3f}
este greu \plain\expndtw-7 \f10 \fs42 de trasat, datorit{\f63
\u259\'3f} caracterelor comp lexe ale unit{\f63 \u259\'3f}{\f63
\u539\'3f}ilor ce vin în \plain\expndtw-5 \f10 \fs42 contact: zona
C{\f63 \u259\'3f}limanului în sud {\f63 \u537\'3f}i aceea a
Mun{\f63 \u539\'3f}ilor Bârg{\f63 \u259\'3f}u {\f63 \u537\'3f} i
\plain\expndtw-8 \f10 \fs42 Depresiunea Dornelor în nord.
\plain\par \pard\sl-606 \li4 \ri951 \expndtw-4 {\f0\fs63 \bullet
}\f10 \fs42 Ea trece la n ord de Dealul T{\f63 \u259\'3f}nasa
(1.001 m), intersecteaz{\f63 \u259\'3f} \plain\par \pard\sl-504
\li544 \ri93 \expndtw-5 \f10 \fs42 cursul mijlociu al v{\f63 \u259\
'3f}ii Pietroasa de Jos, urcând spre nord pân{\f63 \u259\'3f} la
\plain\par \pard\sl-497 \li544 \ri257 \expndtw-6 \f10 \fs42
localitatea Bistri{\f63 \u539\' 3f}a Bârg{\f63 \u259\'3f}ului. În
continuare, c{\f63 \u259\'3f}tre est, urm{\f63 \u2 59\'3f}re{\f63
\u537\'3f}te \plain\par \pard\sl-515 \li544 \ri489 \expndtw-4 \f10
\fs42 valea Bistri{\f63 \u539\'3f}ei pân{\f63 \u259\'3f} în
apropiere de Colibi{\f63 \u539\'3f}a, de unde se abate \plain\par
\pard\sl-503 \li544 \ri1003 \expndtw-7 \f10 \fs42 spre sud, {\f63
\u537\'3f}i într etaie cursul superior al P{\f63
\u259\'3f}nule{\f63 \u539\'3f}ului {\f63 \u537\' 3f}i pârâul
\plain\par \pard\sl-492 \li544 \ri6322 \expndtw-8 \f10 \fs42
Colbul, pe sub Vf. {\f63 \u538 \'3f}iganca.
\par \sect\sectd\sbkpage\margtsxn240\pard
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}}\margt280\margb320\margr800\margl860 \plain\pard\sl-941 \li4
\ri5977 \expndtw-18 {\f0\fs117 \bullet }\b \f10 \fs78 M un\b0 {\f63
\u539\'3f}\b ii Gurghiu \plain\par \pard\sl-886 \li4 \ri1200
\expndtw-18 \f10 \fs60 Sunt o grup{\f63 \u259\'3f} mun toas{\f63
\u259\'3f} a Carpa{\f63 \u539\'3f}ilor Moldo- \plain\par
\pard\sl-720 \li544 \ri1369 \expndtw-10 \f10 \fs60 Transilvani,
apar{\f63 \u539\ '3f}inând de lan{\f63 \u539\'3f}ul muntos
\plain\par \pard\sl-703 \li544 \ri1470 \expndtw-9 \f10 \fs60 al
Carpa{\f63 \u539\'3f}ilor O rientali. Cel mai înalt pisc \plain\par
\pard\sl-727 \li544 \ri988 \expndtw-10 \f10 \fs60 este Vârful Saca
Mare, având\b 1. 776 m\b0 . Al \plain\par \pard\sl-728 \li544 \ri29
\expndtw-5 \f10 \fs60 doilea vârf ca în{\f63 \u259\'3f}l{\ f63
\u539\'3f}ime este\i Vârful Fâncelu\i0 , cu \plain\par \pard\sl-694
\li544 \ri8876 \expndtw-26 \f10 \fs60 1.684 m. \plain\par
\sl-116\fs12\par\sl-240\fs24\par\par\par\par\pard\pard\sl-914 \li4
\ri5977 \expn dtw-18 {\f0\fs117 \bullet }\b \f10 \fs78 Mun\b0 {\f63
\u539\'3f}\b ii Gurghiu \plain\par \pard\sl-828 \li4 \ri460
\expndtw-10 \f10 \fs55 Sunt cuprin{\f63 \u537\'3f}i între
valea Mure{\f63 \u537\'3f}ului {\f63 \u537\'3f}i râul Târnava
\plain\par \pard\sl-666 \li4 \ri453 \fi540 \expndtw-10 \f10 \fs55
Mare. Creasta are o orien tare general{\f63 \u259\'3f} NV-SE.
\par \sect\sectd\sbkpage\margtsxn200\pard
\jexpand\viewkind1\paperw14400\paperh10800 {\shp
{\*\shpinst\shpleft0\shptop0\shpright14400\shpbottom10800
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\pard\sl-524 \li544 \ri773 \expndtw-8 \f10 \fs54 dintre Homorodul
Mic {\f63 \u53 7\'3f}i Vârghi{\f63 \u537\'3f} iar spre sud de
\plain\par \pard\sl-518 \li544 \ri2925 \expndtw-9 \f10 \fs54
Depresiunea {\f63 \u537\'3f}i Mun{\f63 \u539\'3f}ii Baraolt pe
linia \plain\par \pard\sl-519 \li544 \ri304 \expndtw-11 \f10 \fs54
localit{\f63 \u259\'3f}{\f63 \ u539\'3f}ilor Filia{\f63 \u537\'3f}i
Herculian, în lungul v{\f63 \u259\'3f}ii Ozun ca \plain\expndtw-4
\f10 \fs54 {\f63 \u537\'3f}i peste pasul Hatod pân{\f63 \u259\'3f }
în valea Oltului. În sud \plain\expndtw-7 \f10 \fs54 se mai
învecineaz{\f63 \u259\'3f} cu Mun{\f63 \u539\'3 f}ii
Bodocului(desp{\f63 \u259\'3f}r{\f63 \u539\'3f}i{\f63 \u539\'3f}i
\plain\par \pard\sl-518 \li544 \ri946 \expndtw-8 \f10 \fs54 de
Valea Ro{\f63 \u537\'3f}ie { \f63 \u537\'3f}i pasul Jimbor) iar în
est limita \plain\par \pard\sl-510 \li544 \ri2053 \expndtw-8 \f10
\fs54 trece pe la baza conului vulca nic Puciosu \plain\par
\pard\sl-519 \li544 \ri5736 \expndtw-11 \f10 \fs54 {\f63
\u537\'3f}i Depresiunea Ciucului.
\par \sect\sectd\sbkpage\margtsxn100\pard
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0028a28a0028a28a0028a28a0028a28a0028a28a0028a28a0028a28a0028a28a0028a28a0028a28a
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0028a28a0028a28a0028a28a0028a28a0028a28a0028a28a0028a28a0028a28a0028a28a0028a28a
\pard\sl-415 \li544 \ri1037 \expndtw-4 \f10 \fs37 Mari prin Pasul
Liban (1000 m) {\f63 \u537\'3f}i Valea Târnavei Mici prin
Pasul \plain\par \pard\sl-410 \li544 \ri98 \expndtw-5 \f10 \fs37
Bucin (1273 m). Prin Defileul De da - Topli{\f63 \u539\'3f}a
comunic{\f63 \u259\'3f} cu Depresiunea \plain\par \pard\sl-398
\li544 \ri4165 \expndtw-7 \f10 \fs37 V{\f63 \u259\'3f}lenii de Mure
{\f63 \u537\'3f} spre Podi{\f63 \u537\'3f}ul Transilvaniei.
\plain\par \pard\sl-513 \li4 \ri821 \expndtw-9 {\f0\fs56 \bullet }
\plain\tx541 \tab \expndtw-4 \f10 \fs37 Are un fundament de {\f63
\u537\'3f}istu ri cristaline peste care stau depozite de \plain\par
\pard\sl-410 \li544 \ri743 \expndtw-4 \f10 \fs37 pietri{\f63
\u537\'3f}uri, nisi puri {\f63 \u537\'3f}i chiar marne. Depresiunea
a evoluat în direc{\f63 \u539\'3f} ia \plain\par \pard\sl-410
\li544 \ri426 \expndtw-3 \f10 \fs37 punerii în eviden{\f63
\u539\'3f} {\f63 \u259\'3f} a trei trepte de relief: piemonturi
laterale, lunca {\f63 \u537 \'3f}i \plain\par \pard\sl-392 \li544
\ri9432 \expndtw-14 \f10 \fs37 terasele. \plain\par \pard\sl-514
\li4 \ri331 \expndtw-9 {\f0\fs56 \bullet } \plain\tx541 \tab
\expndtw-4 \f10 \fs37 Numeroase probe arheologice dovedesc c{\ f63
\u259\'3f} bazinul Giurgeului a fost \plain\par \pard\sl-414 \li544
\ri819 \expndtw-3 \f10 \fs37 locuit înc{\f63 \u259\'3f} din ti
mpuri str{\f63 \u259\'3f}vechi. Despre secuii din Giurgeu {\f63
\u537\'3f}i Ciuc \plain\par \pard\sl-411 \li544 \ri792
\expndtw-4 \f10 \fs37 g{\f63 \u259\'3f}sim men{\f63 \ u539\'3f}iuni
înc{\f63 \u259\'3f} din 1285, când au luptat împotriva t{\f63
\u259\'3f} tarilor în \plain\expndtw-16 \f10 \fs37 Mun{\f63
\u539\'3f}ii Tarc{\f63 \u259\'3f}ului. \plain\par \pard\sl-501 \li4
\ri298 \expndtw-9 {\f0\fs56 \bullet } \plain\tx541 \tab \expndtw-6
\f10 \fs37 Prima men{\f63 \u539\'3f}iune documentar {\f63
\u259\'3f} despre existen{\f63 \u539\'3f}a a{\f63 \u537\'3f}ez{\f63
\u259\ '3f}rilor din bazinul \plain\par \pard\sl-404 \li544 \ri770
\expndtw-3 \f10 \fs37 Giurgeului o avem din anii 1332 -1334, cu
ocazia conscrierii dijmei \plain\par \pard\sl-416 \li544 \ri397
\expndtw-6 \f10 \fs37 papale. Documentele amintite di n ace{\f63
\u537\'3f}ti ani se refer{\f63 \u259\'3f} la trei localit{\f63
\u259\ '3f}{\f63 \u539\'3f}i \plain\expndtw-6 \f10 \fs37 sub numele
de Gheorgheni, Joseni {\f63 \u537\'3f}i L {\f63
\u259\'3f}zarea.
00ffd9 }}} {\sp{\sn fRecolorFillAsPicture}{\sv 0}} {\sp{\sn
posrelh}{\sv 1}} {\sp{\sn posrelv}{\sv 1}} {\sp{\sn
fAllowOverlap}{\sv 1}} {\sp{\sn fBehindDocument}{\sv 1}}
}}\margt360\margb280\margr840\margl860 \plain\pard\sl-652 \li4
\ri629 \expndtw-3 {\f0\fs81 \bullet }\f10 \fs54 Înc{\f63 \u259\'3f}
din perioada antichit{\f63 \u259\'3f}{\f63 \u539\'3f}ii, râul
Mure{\f63 \u537\'3f} a fost o \plain\par \pard\sl-577 \li544
\ri788 \expndtw-11 \f10 \fs54 cale navigabil{\f63 \u259\'3f}
foarte intens folosit{\f63 \u259\'3f} atât pentru \plain\par
\pard\sl-589 \li544 \ri147 \expndtw-7 \f10 \fs54 traficul comercial
cât {\f63 \u53 7\'3f}i în scop strategic, devenind \plain\par
\pard\sl-576 \li544 \ri1192 \expndtw-15 \f10 \fs54 o adev{\f63
\u259\'3f}rat{\f6 3 \u259\'3f} autostrad{\f63 \u259\'3f} a zonei de
la Nord de \plain\par \pard\sl-590 \li544 \ri539 \expndtw-7 \f10
\fs54 Dun{\f63 \u259\'3f}re. Men{\f63 \u539\'3f}ionat de
Herodot înc{\f63 \u259\'3f} din anul 484 \plain\par \pard\sl-576
\li544 \ri1221 \expndtw-12 \f10 \fs54 î.h. (cu 4 secole înainte de
crea rea "Drumului \plain\par \pard\sl-589 \li544 \ri440
\expndtw-17 \f10 \fs54 M{\f63 \u259\'3f}t{\f63 \u259\ '3f}sii"),
sub denumirea de Maris, Mure{\f63 \u537\'3f}ul este, \plain\par
\pard\sl-576 \li544 \ri31 \expndtw-12 \f10 \fs54 dup{\f63
\u259\'3f} Dun{\f63 \u 259\'3f}re, al doilea râu al României ca
lungime \plain\par \pard\sl-590 \li544 \ri1088 \expndtw-10 \f10
\fs54 (761 km) {\f63 \u537\'3f}i al treilea ca suprafa{\f63
\u539\'3f}{\f63 \u259\'3f} hidrografic{\f63 \u259\'3f}
\plain\expndtw-15 \f10 \fs54 (27.890 kmp, dup{\f63 \u259\'3f}
Dun{\f63 \u259\'3f }re {\f63 \u537\'3f}i Siret). \plain\par
\pard\sl-706 \li4 \ri299 \expndtw-2 {\f0\fs81 \bullet }\f10 \fs54
Înc{\f63 \u259\ '3f} din timpul r{\f63 \u259\'3f}zboaielor
daco-romane controlul \plain\par \pard\sl-590 \li544 \ri578
\expndtw-7 \f10 \fs54 Mure{\f63 \u537\'3f}ului a cons tituit una
din manevrele militare \plain\par \pard\sl-576 \li544 \ri866
\expndtw-13 \f10 \fs54 cheie, pe care armata roman{\f 63 \u259\'3f}
s-a str{\f63 \u259\'3f}duit s{\f63 \u259\'3f} o \plain\par
\pard\sl-589 \li544 \ri188 \expndtw-9 \f10 \fs54 ob{\f63
\u539\'3f}in{\f63 \u259 \'3f} pentru a avea un avantaj asupra
sistemului \plain\par \pard\sl-575 \li544 \ri5025 \expndtw-9 \f10
\fs54 defensiv al Regatului dacic.
ile acestuia \plain\par \pard\sl-605 \li544 \ri399 \expndtw-7 \f10
\fs55 sunt: lacul se întinde pe un peri metru de 2.830
\plain\expndtw-8 \f10 \fs55 m, aria este de 114.676 m² {\f63
\u537\'3f}i volumul a pei care \plain\par \pard\sl-598 \li544
\ri560 \expndtw-10 \f10 \fs55 se acumuleaz{\f63 \u259\'3f} e ste de
587.503 m³. Lacul s-a \plain\par \pard\sl-603 \li544 \ri29
\expndtw-7 \f10 \fs55 format la altitudinea de 983 m, în tr-o
depresiune \plain\par \pard\sl-588 \li544 \ri3121 \expndtw-8 \f10
\fs55 cu un climat predominant subal pin
\par \sect\sectd\sbkpage\margtsxn140\pard
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\sl-81\fs8\par\sl-240\fs24\par\par\par\pard\pard\sl-669 \li4 \ri513
\expndtw-11 \f10 \fs60 Împrejurimile lacului au un microclimat
pl{\f63 \u259\'3f}cut, \plain\par \pard\sl-576 \li544 \ri25
\expndtw-11 \f10 \fs60 deosebit de benefic pentru trat area st{\f63
\u259\'3f}rilor de \plain\par \pard\sl-583 \li544 \ri2364
\expndtw-16 \f10 \fs60 extenuare fizic{\f63 \u259\'3 f} {\f63
\u537\'3f}i psihic{\f63 \u259\'3f}, insomnii, \plain\par
\pard\sl-568 \li544 \ri421 \expndtw-14 \f10 \fs60 neurastenii.
Temperatura medie multianual{\f63 \u259\'3f} \plain\par
\pard\sl-574 \li544 \ri2586 \expndtw-10 \f10 \fs60 este de 8°C,
peste media de 6°C a \plain\par \pard\sl-576 \li544 \ri1717
\expndtw-11 \f10 \fs60 depresiunilor intramontane. V alea este
\plain\par \pard\sl-578 \li544 \ri1011 \expndtw-11 \f10 \fs60
practic ferit{\f63 \u259\'3f} de vânturi, aerul deosebit de
\plain\par \pard\sl-574 \li544 \ri111 \expndtw-8 \f10 \fs60 curat,
bogat în aerosoli naturali , împrejurimile \plain\par \pard\sl-585
\li544 \ri120 \expndtw-11 \f10 \fs60 pitore{\f63 \u537\'3f}ti ofer{
\f63 \u259\'3f} condi{\f63 \u539\'3f}ii excelente pentru cei ce
\plain\par \pard\sl-569 \li544 \ri1043 \expndtw-15 \f10 \fs60
caut{\f63 \u259\'3f} surse de regenerare rapid{\f63
\u259\'3f} pe cale \plain\par \pard\sl-575 \li544 \ri1494
\expndtw-12 \f10 \fs60 natural{\f63 \u259\'3f}. Începând cu
anii 1900, tocmai \plain\par \pard\sl-574 \li544 \ri862 \expndtw-8
\f10 \fs60 turismul balnear-recreativ a fo st cel care a
\plain\expndtw-9 \f10 \fs60 adus dezvoltarea din punctul de vedere
a \plain\par \pard\sl-569 \li544 \ri3019 \expndtw-9 \f10 \fs60
serviciilor turistice a aceste i zone
\par \sect\sectd\sbkpage\margtsxn200\pard
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\plain\par \pard\sl-379 \li544 \ri572 \expndtw-7 \f10 \fs40
caracteristic{\f63 \u259\'3f} a parte, pe care ne-o dezv{\f63
\u259\'3f}luie directorul fabricii de \plain\expndtw-13 \f10 \fs40
îmbuteliere, Florin R{\f63 \u259\'3f}ducu L{\f63 \u25 9\'3f}z{\f63
\u259\'3f}roiu. \plain\par \pard\sl-480 \li4 \ri1048 \expndtw-6
{\f0\fs60 \bullet }\f10 \fs40 ''Numeroasel e izvoare de ap{\f63
\u259\'3f} mineral{\f63 \u259\'3f} din aceast{\f63 \u259\'3 f}
zon{\f63 \u259\'3f} sunt \plain\par \pard\sl-383 \li544 \ri507
\expndtw-9 \f10 \fs40 alimentate cu ap{\f63 \u259\'3f }
provenit{\f63 \u259\'3f} din topirea z{\f63 \u259\'3f}pezilor, iar
temperatura \plain\expndtw-5 \f10 \fs40 este în jur de zece
grade, ceea ce este neobi{\f63 \u5 37\'3f}nuit în condi{\f63
\u539\'3f}iile în \plain\par \pard\sl-378 \li544 \ri1384 \expndtw-6
\f10 \fs40 care apele minerale carbogazoa se din Câmpia Vestului
sau \plain\par \pard\sl-390 \li544 \ri210 \expndtw-5 \f10 \fs40
Depresiunea Bra{\f63 \u537\'3f} ovului, precum {\f63 \u537\'3f}i
cele din Cehia, Italia, Germania \plain\expndtw-9 \f10 \fs40 sau
Fran{\f63 \u539\'3f}a sunt ape calde, de 18-22 g rade'',
explic{\f63 \u259\'3f} L{\f63 \u259\'3f}z{\f63 \u259\'3f}roiu.
\plain\par \pard\sl-475 \li4 \ri813 \expndtw-3 {\f0\fs60 \bullet
}\f10 \fs40 Multe secole mai târziu, dup{\f63 \u259\'3f}
descoperirea lor de c{\f63 \u259\'3f}tre romani, \plain\par
\pard\sl-383 \li544 \ri51 \expndtw-5 \f10 \fs40 apele minerale de
la Borsec au înc eput s{\f63 \u259\'3f} fie îmbuteliate în ulcioare
\plain\par \pard\sl-389 \li544 \ri1960 \expndtw-6 \f10 \fs40 de lut
ars {\f63 \u537\'3f}i t ransportate în desagi, pe spinarea cailor,
în \plain\par \pard\sl-383 \li544 \ri67 \expndtw-6 \f10 \fs40
Transilvania, Moldova, {\f63 \u5 38\'3f}ara Româneasc{\f63
\u259\'3f} {\f63 \u537\'3f}i Ungaria. Exist{\f63 \u259\' 3f}
atest{\f63 \u259\'3f}ri \plain\par \pard\sl-379 \li544 \ri1234
\expndtw-8 \f10 \fs40 documentare potrivit c{\f63 \u 259\'3f}rora
apa mineral{\f63 \u259\'3f} de la Borsec a fost \plain\par
\pard\sl-388 \li544 \ri854 \expndtw-8 \f10 \fs40 transportat{\f63
\u259\'3f} cu c{\f63 \u259\'3f}ru{\f63 \u539\'3f}ele, în 1594, în
butoaie de stejar, la curtea \plain\par \pard\sl-379 \li544 \ri410
\expndtw-6 \f10 \fs40 domneasc{\f63 \u259\'3f} de la Alba Iulia,
unde au fost folosite pentru tratament \plain\par \pard\sl-384
\li544 \ri783 \expndtw-8 \f10 \fs40 de c{\f63 \u259\'3f}tre Sigismu
nd Bathory. În 1844, poetul Vasile Alecsandri a \plain\par
\pard\sl-389 \li544 \ri157 \expndtw-5 \f10 \fs40 ajuns la Borsec
{\f63 \u537\'3f }i a povestit un an mai târziu, cu entuziasm,
despre \plain\expndtw-5 \f10 \fs40 calitatea, îmbutelierea {\f63
\u537\'3f}i transportare a apelor, într-un text publicat în
\plain\expndtw-9 \f10 \fs40 ''Calendarul Foaiei s{\f63
\u259\'3f}te{\f63 \u537\' 3f}ti''.
\par \sect\sectd\sbkpage\margtsxn240\pard
\jexpand\viewkind1\paperw14400\paperh10800 {\shp
\sl-314\fs31\par\pard\pard\sl-379 \li4 \ri1480 \expndtw-8 {\f0\fs51
\bullet } \plain\tx541 \tab \expndtw-3 \f10 \fs34 Potrivit
documentelor vremii, erau îmbutel iate 5.000 de sticle pe zi, iar
\plain\par \pard\sl-616 \li544 \ri1022 \expndtw-5 \f10 \fs34
ambalarea se f{\f63 \u259\'3f} cea în l{\f63 \u259\'3f}zi
necompartimentate, {\f63 \u537\'3f}ocurile transportulu i fiind
\plain\par \pard\sl-607 \li544 \ri308 \expndtw-5 \f10 \fs34
atenuate cu cetin{\f63 \u259\'3 f} sau fân. De-a lungul anilor,
îmbutelierea a fost efectuat{\f63 \u259\'3f} de \plain\par
\pard\sl-616 \li544 \ri1109 \expndtw-4 \f10 \fs34 diferi{\f63
\u539\'3f}i propri etari {\f63 \u537\'3f}i a stagnat, câte doi ani,
atât în timpul Primului R{\f63 \u259\ '3f}zboi \plain\expndtw-4
\f10 \fs34 Mondial, cât {\f63 \u537\'3f}i în perioada celei de-a do
ua conflagra{\f63 \u539\'3f}ii mondiale. \plain\par
\sl-294\fs29\par\pard\pard\sl-399 \li4 \ri169 \expndtw-8 {\f0\fs51
\bullet } \plain\tx541 \tab \expndtw-5 \f10 \fs34 Odat{\f63
\u259\'3f} cu na{\f63 \u539\'3 f}ionaliz{\f63 \u259\'3f}rile din
1948, activitatea de îmbuteliere a intrat în atrib u{\f63
\u539\'3f}iile \plain\par \pard\sl-611 \li544 \ri29 \expndtw-4 \f10
\fs34 statului, care a efectuat import ante investi{\f63
\u539\'3f}ii în vederea moderniz{\f63 \u259\'3f}rii produc{\f63
\u539\'3f}iei {\f63 \u537\'3f}i \plain\par \pard\sl-608 \li544
\ri809 \expndtw-6 \f10 \fs34 dezvolt{\f63 \u259\'3f}rii zone i.
Dup{\f63 \u259\'3f} 1989 întreprinderea de stat s-a transformat în
firm{\f63 \u25 9\'3f} \plain\par \pard\sl-612 \li544 \ri111
\expndtw-4 \f10 \fs34 privat{\f63 \u259\'3f} cu capit al integral
autohton, iar istoria de succes a brandului a continuat.
\par \sect\sectd\sbkpage\margtsxn480\pard
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}}\margt320\margb220\margr640\margl380 \plain\pard\sl-584 \li3
\ri556 \fi751 \expndtw-9 \b\i \f10 \fs49 Culoarul depres ionar
Dr{\f63 \u259\'3f}goiasa - Glodu - Bilbor - \plain\par \pard\sl-471
\li3 \ri4978 \fi6205 \expndtw-24 \b\i \f10 \fs49 Pintec\b0 :
\plain\par \sl-171\fs17\par\sl-240\fs24\par\par\pard\pard\sl-556
\li3 \ri678 \expndtw-6 {\f 0\fs74 \bullet }\f10 \fs49 - se
desf{\f63 \u259\'3f}{\f63 \u351\'3f}oar{\f63 \u 259\'3f} în general
la contactul dintre cristalinul \plain\par \pard\sl-480 \li3
\ri5307 \fi540 \expndtw-14 \f10 \fs49 Bistri{\f63 \u355\'3f}ei
{\f63 \u351\'3f}i eruptivul C{\f63 \u259\'3f}limanilor;
\plain\par \pard\sl-600 \li3 \ri822 \expndtw-5 {\f0\fs74 \bullet
}\f10 \fs49 - curgerile d e lav{\f63 \u259\'3f}, datorate erup{\f63
\u355\'3f}iilor ce au avut loc în \plain\par \pard\sl-479 \li544
\ri202 \expndtw-8 \f10 \fs49 intervalul dintre sarma{\f63 \u
355\'3f}ian {\f63 \u351\'3f}i cuaternarul inferior, au barat
\plain\par \pard\sl-480 \li544 \ri2001 \expndtw-7 \f10 \fs49
obâr{\f63 \u351\'3f}iile unor râur i ce se îndreptau spre Bazinul
\plain\par \pard\sl-478 \li544 \ri18 \expndtw-6 \f10 \fs49
Transilvaniei, transformându-le în b azine lacustre; ulterior,
\plain\par \pard\sl-481 \li544 \ri798 \expndtw-10 \f10 \fs49 prin
p{\f63 \u259\'3f}trundere a regresiv{\f63 \u259\'3f} în aceste
bazine lacustre a \plain\par \pard\sl-479 \li544 \ri102 \expndtw-11
\f10 \fs49 unor afluen{\f63 \u355\'3f}i a i Bistri{\f63
\u355\'3f}ei moldave, p{\f63 \u259\'3f}trundere ce a avut loc
\plain\par \pard\sl-480 \li544 \ri2355 \expndtw-7 \f10 \fs49 în
pliocenul superior, acestea a u fost scurse {\f63 \u351\'3f}i
\plain\par \pard\sl-478 \li544 \ri7199 \expndtw-9 \f10 \fs49
transformate în uscat; \plain\par \pard\sl-602 \li3 \ri701
\expndtw-6 {\f0\fs74 \bullet }\f10 \fs49 -\i Depresiu nea Dr{\f63
\u259\'3f}goiasa\i0 este situat{\f63 \u259\'3f} pe valea Neagra
\plain\par \pard\sl-479 \li544 \ri902 \expndtw-6 \f10 \fs49
Bro{\f63 \u351\'3f}tenilor, înreg istrând o altitudine în partea de
jos a \plain\par \pard\sl-478 \li544 \ri7008 \expndtw-10 \f10 \fs49
depresiunii de 1050 m; \plain\par \pard\sl-601 \li3 \ri753
\expndtw-4 {\f0\fs74 \bullet }\f10 \fs49 -\i Depresiu nea Bilbor\i0
este situat{\f63 \u259\'3f} în bazinul superior al \plain\par
\pard\sl-480 \li3 \ri227 \fi540 \expndtw-6 \f10 \fs49 râului
Bistricioara, la o al titudine medie de 920 - 1050 m;
\plain\par \pard\sl-518 \li544 \ri258 \expndtw-11 \f10 \fs54
Grin{\f63 \u355\'3f}ie{\f63 \u 351\'3f}, Telec), mân{\f63
\u259\'3f}stiri vechi (Dur{\f63 \u259\'3f}u, Cerebuc) \plain\par
\pard\sl-518 \li544 \ri599 \expndtw-4 \f10 \fs54 sau mai noi
(mân{\f63 \u259\'3f}s tirea de pe munte cu hramul \plain\par
\pard\sl-518 \li544 \ri1002 \expndtw-14 \f10 \fs54 Schimbarea la
Fa{\f63 \u355\' 3f}{\f63 \u259\'3f}, Poiana Maicilor, Port{\f63
\u259\'3f}ri{\f63 \u355\'3f}a \plain\par \pard\sl-518 \li544
\ri9803 \expndtw-33 \f10 \fs54 {\f63 \u351\'3f}.a.); \plain\par
\pard\sl-648 \li4 \ri275 \expndtw0 {\f0\fs81 \bullet }\f10 \fs54 -
mân{\f63 \u259 \'3f}stirea Dur{\f63 \u259\'3f}u, întemeiat{\f63
\u259\'3f} în secolul XVII, în \plain\par \pard\sl-518 \li544
\ri113 \expndtw-14 \f10 \fs54 prezent de maici (17 vie{\f63
\u355\'3f}uitoare), cu hramul {\f63 \u8222\'3f}Buna \plain\par
\pard\sl-518 \li544 \ri1005 \expndtw-14 \f10 \fs54 Vestire" (25
martie); biseric a de zid, pictat{\f63 \u259\'3f} pe \plain\par
\pard\sl-518 \li544 \ri446 \expndtw-11 \f10 \fs54 interior de N.
Tonitza {\f63 \ u351\'3f}i un grup de ucenici ai s{\f63
\u259\'3f}i;
\par \sect\sectd\sbkpage\margtsxn320\pard
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