Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 117
... glacial deposits . ( b ) ( c ) Middle transitional zone - lying between 3500-2000 m and remaining under annual snow for 4-6 months . In this zone the Pliestocenic glacial deposits are generally covered by old periglacial material which ...
... glacial deposits . ( b ) ( c ) Middle transitional zone - lying between 3500-2000 m and remaining under annual snow for 4-6 months . In this zone the Pliestocenic glacial deposits are generally covered by old periglacial material which ...
Page 118
... glaciation ( Fig . 2 ) . The recent glacial features are restricted to the upper catchment and higher reaches characterized by permanent snow banks , small nivational cirques , subrecent morainic deposits and boulder field of present ...
... glaciation ( Fig . 2 ) . The recent glacial features are restricted to the upper catchment and higher reaches characterized by permanent snow banks , small nivational cirques , subrecent morainic deposits and boulder field of present ...
Page 124
... glacial deposits were eroded later on by the fluvial action and particularly most of the glacial deposits of left valley side were washed out due to leftward shifting of the Uhl along the anticlinal axis . The occurrence of about 40 m ...
... glacial deposits were eroded later on by the fluvial action and particularly most of the glacial deposits of left valley side were washed out due to leftward shifting of the Uhl along the anticlinal axis . The occurrence of about 40 m ...
Contents
CHOUBEY Kewal K Sharma D RAMESHWAR RAO Crustal anatexis | 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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02:53 IST MAGNITUDE Accel cm/sē Agglomeratic Slate Amritpur axial plane Bafliaz Formation basin biotite Budhal Burtsa Formation calcite chert clasts conglomerate Cretaceous deformation Dehra Dun deposits dolomite Dum Gali Quartzite facies fault plane feldspar folds foliation fossils Garhwal Geol gneiss grained granites granitoids grey Gulabgarh Himachal Himalaya Himalayan Geology India Infrakrol Institute of Himalayan inversion Jour Jutogh Kashmir Kharnak Krol Ladakh landslides Lesser Himalaya limestone lineation Maastrichtian Mandi metamorphic Nappe Nilkanth Panjal thrust Panjal Volcanic Parautochthonous belt pebbles periglacial Permian phyllites Pir Panjal range plagioclase porphyries Proterozoic quartz quartzite Rampur Ramsu region rocks Salkhala samples sandstone Sarkanth schist sector sedimentary sediments sequence shale Sharma shear Shergol Singh SiO2 slide slip slope soil strain Stratigraphy structures Surv Suture Zone Syncline tectonic Tethyan Thakur thick Thinly bedded Uhl valley Unconformity upper UTTARKASHI UTTARKASHI EARTHQUAKE Verma Wadia Institute WIMF/A Ypresian Zanskar