Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 121
Most probably the soils are of Upper Pleistocene period . Palynological analysis
of black soil horizone ( Phadtare , 1988 ) reveals that the lower most black soil
horizon contain pollens of annual open grass and primary wood . This
succeeded ...
Most probably the soils are of Upper Pleistocene period . Palynological analysis
of black soil horizone ( Phadtare , 1988 ) reveals that the lower most black soil
horizon contain pollens of annual open grass and primary wood . This
succeeded ...
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
The evidence oi full glacial phase in the Uhl during the Pleistocene is profoundly
displayed by glacial deposits , erratic blocks , wide U shaped valley , waterfalls ,
deglaciated cirques etc. At the apex of glaciation the Uhl glacier extended ...
The evidence oi full glacial phase in the Uhl during the Pleistocene is profoundly
displayed by glacial deposits , erratic blocks , wide U shaped valley , waterfalls ,
deglaciated cirques etc. At the apex of glaciation the Uhl glacier extended ...
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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