Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 117
Geomorphology of the Uhl valley , Chhota Bhangal , Kangra District , Himachal
Pradesh , India M.P. SAH Wadia Institute of Himalayan Geology , Dehra Dun -
248001 , India Abstract : The paper deals with the geomorphology , formation of ...
Geomorphology of the Uhl valley , Chhota Bhangal , Kangra District , Himachal
Pradesh , India M.P. SAH Wadia Institute of Himalayan Geology , Dehra Dun -
248001 , India Abstract : The paper deals with the geomorphology , formation of ...
Page 118
Geomorphology of Uhl valley Morphological features Chino H.P. LOCATION OF
STUDY AREA Arabian Soo Longel 10 . Th J. K. Dhauladhar Ro Kan 32 ° N U.
130 ° 100 km 74 ° C 70 ° 80 D : Deot S = Salatri poss Me = Mahot K Kothikor -
Road ...
Geomorphology of Uhl valley Morphological features Chino H.P. LOCATION OF
STUDY AREA Arabian Soo Longel 10 . Th J. K. Dhauladhar Ro Kan 32 ° N U.
130 ° 100 km 74 ° C 70 ° 80 D : Deot S = Salatri poss Me = Mahot K Kothikor -
Road ...
Page 124
present day cross profile of the Uhl valley distinctly represents the upper broader
valley of glacial origin terminating into a narrow gorge of fluvial origin in the lower
section of the profile . Along the upper reaches the Uhl valley represents a ...
present day cross profile of the Uhl valley distinctly represents the upper broader
valley of glacial origin terminating into a narrow gorge of fluvial origin in the lower
section of the profile . Along the upper reaches the Uhl valley represents a ...
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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