Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 42
Due to heavy water seepage the hill slope with surficial debris slide gradually
sinks down . of weathering so that they are locally reduced to heaps of loose
rocks and argillaceous detritus causing landslides ( Sinha , 1975 ) . The
orography and ...
Due to heavy water seepage the hill slope with surficial debris slide gradually
sinks down . of weathering so that they are locally reduced to heaps of loose
rocks and argillaceous detritus causing landslides ( Sinha , 1975 ) . The
orography and ...
Page 118
The deglaciated cirques at the base are filled by glacial debris and have
moderate slope ranging between 20 ° to 25 ° . ... Consequently there is more of
snow drifted sediment accumulated along the gentle valley slopes and the
tributary ...
The deglaciated cirques at the base are filled by glacial debris and have
moderate slope ranging between 20 ° to 25 ° . ... Consequently there is more of
snow drifted sediment accumulated along the gentle valley slopes and the
tributary ...
Page 121
Weathered granite / gneiss boulders Bed rock and down slope directions . ... In
this case the continuous percolation of water to soil surface at upper slopes due
to snowmelt further facilitated the movement of solifluction lobes since in ...
Weathered granite / gneiss boulders Bed rock and down slope directions . ... In
this case the continuous percolation of water to soil surface at upper slopes due
to snowmelt further facilitated the movement of solifluction lobes since in ...
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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