Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 117
About 37.74 percent of catchment area is under forest , covered by Pine , Cedrus
, Quercus , Abes and Rhododendron forming tree line at an altitude of 3500 m .
The higher reaches of the valley ( more than 4200 m ) remain under snow cover ...
About 37.74 percent of catchment area is under forest , covered by Pine , Cedrus
, Quercus , Abes and Rhododendron forming tree line at an altitude of 3500 m .
The higher reaches of the valley ( more than 4200 m ) remain under snow cover ...
Page 123
... geological conditions and recent tectonic activity the evolution of the Uhl
landscape is sketched ( Fig . 9 ) . The presence of Quaternary deposits reveal
that during the Pleistocene the entire Uhl valley was covered by the valley glacier
.
... geological conditions and recent tectonic activity the evolution of the Uhl
landscape is sketched ( Fig . 9 ) . The presence of Quaternary deposits reveal
that during the Pleistocene the entire Uhl valley was covered by the valley glacier
.
Page 124
Glaciofluvial deposits are also seen at village Kothikor which are covered by
recent to subrecent scree brought by lateral channels . A number of waterfalls
almost along the same line from the Malatha to Deot droping from the left bank of
Uhl ...
Glaciofluvial deposits are also seen at village Kothikor which are covered by
recent to subrecent scree brought by lateral channels . A number of waterfalls
almost along the same line from the Malatha to Deot droping from the left bank of
Uhl ...
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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