Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 117
... periglacial environment and the implication of Pleistocene glaciation and neotectonic activity on the evolution of the Uhl valley landscape . It has been observed that periglacial siope deposits are susceptible to slow mass movement in ...
... periglacial environment and the implication of Pleistocene glaciation and neotectonic activity on the evolution of the Uhl valley landscape . It has been observed that periglacial siope deposits are susceptible to slow mass movement in ...
Page 121
... periglacial material . thick soil horizon has distinct black and brown soil layers buried under 40-60 cm thick recent soil . The thickness of black soil horizon varies from 75 cm near Kurdhara to 10-20 cm in the entire mid hill slope ...
... periglacial material . thick soil horizon has distinct black and brown soil layers buried under 40-60 cm thick recent soil . The thickness of black soil horizon varies from 75 cm near Kurdhara to 10-20 cm in the entire mid hill slope ...
Page 123
... periglacial slope c- ( i ) Solifluction and periglacial deposits have covered the glacial deposits ( ii ) Continuous uplift formation of gorge , erosion of periglacial deposits . Bd = Bed rock T = Talus Ps Periglacial solifluction ...
... periglacial slope c- ( i ) Solifluction and periglacial deposits have covered the glacial deposits ( ii ) Continuous uplift formation of gorge , erosion of periglacial deposits . Bd = Bed rock T = Talus Ps Periglacial solifluction ...
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/s² 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