Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 119
... to high Structural Ridges ME 3308 Mr 29 Lr Lower Quaternary Deposits Hur 21
3122 24 26 3161 o 30 * Recent glacial deposits Past glacial deposits 30 ° 31 34
o 28 Past glaciofluvial deposits 1000 500 Metres L SCALE a Mr Fluvial deposits ...
... to high Structural Ridges ME 3308 Mr 29 Lr Lower Quaternary Deposits Hur 21
3122 24 26 3161 o 30 * Recent glacial deposits Past glacial deposits 30 ° 31 34
o 28 Past glaciofluvial deposits 1000 500 Metres L SCALE a Mr Fluvial deposits ...
Page 123
New slides C - Creep zone Slide scar Rodial crack Debris fan Bed rock Ch -
Channel BD- Bed rock head scar * Pine , Deeda Oak Forest VVv Agricultural land
Evolution of Uhl landscape 0 - Down word cutting of glacial deposit ( M ) due to ...
New slides C - Creep zone Slide scar Rodial crack Debris fan Bed rock Ch -
Channel BD- Bed rock head scar * Pine , Deeda Oak Forest VVv Agricultural land
Evolution of Uhl landscape 0 - Down word cutting of glacial deposit ( M ) due to ...
Page 124
The Uhl was temporarily blicked by the morainie deposits brought by the former
Uhl glacier at the Mehot spur . Beyond Mehot in upstream direction the Uhl valley
is broad and full of glacial deposits . The presence of fine clay and sandy alluvial
...
The Uhl was temporarily blicked by the morainie deposits brought by the former
Uhl glacier at the Mehot spur . Beyond Mehot in upstream direction the Uhl valley
is broad and full of glacial deposits . The presence of fine clay and sandy alluvial
...
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Contents
Petrogenesis of the Granitoid Rocks Chor Region Himachal Himalaya | 1 |
N S VIRDI Basement Structures and their possible relation to Sedimentation and Tectonics in | 9 |
N S VIRDI Basement Structures and their possible relation to Sedimentation and Tectonics in | 11 |
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Common terms and phrases
Agglomeratic Slate analysis associated band base basin bedded belt chert components composition comprising conglomerate contain covered deformation Dehra deposits developed direction distribution district earthquake et al exposed facies fault fault plane feldspar field folds foliation followed Formation fossils Garhwal Geol gneiss grained granites granitoids grey Group higher Himalaya Himalayan Geology India indicates inversion Jour Kashmir Ladakh Lamayuru Late Lesser limestone lineation locality locations lower major Member metamorphic minerals observed occur Panjal pebbles phase phyllites plagioclase plane Pleistocene porphyries present quartz quartzite range region reported represented river road rocks samples sandstone schist sector sedimentary sediments sequence shale Sharma shown Slate slide slip slope soil strain stratigraphy strike structures suggest Surv Table tectonic thick thrust trace unit upper valley VALUES Volcanics Wadia weathered Zanskar zone