Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 38
Type of material Rock Types Causative Factors Slide Area Slide Width along
road ( m ) Location Movement ( km ) involved 40 8.0 Debris slide Majadhari slide
Large size boulders Gneissic boulders , associated with no perfect orientsandy
soil ...
Type of material Rock Types Causative Factors Slide Area Slide Width along
road ( m ) Location Movement ( km ) involved 40 8.0 Debris slide Majadhari slide
Large size boulders Gneissic boulders , associated with no perfect orientsandy
soil ...
Page 39
Type of material Debris consisting of Schist , strike NWsmall rock pieces SE dip
34 ° NE with clayey soil Rock slide Moderate to highly Phyllites , strike NE-
Weathered phyllites , unfavourable beds , ( planar failure ) disintegrated rocks
SW dip ...
Type of material Debris consisting of Schist , strike NWsmall rock pieces SE dip
34 ° NE with clayey soil Rock slide Moderate to highly Phyllites , strike NE-
Weathered phyllites , unfavourable beds , ( planar failure ) disintegrated rocks
SW dip ...
Page 121
The vertical movement of soil particle is associated with the heave and
downward movement is associated with thaw and gravity flow in annual freeze -
thaw cycle ( Jahn , 1975 ) . In this case the continuous percolation of water to soil
surface ...
The vertical movement of soil particle is associated with the heave and
downward movement is associated with thaw and gravity flow in annual freeze -
thaw cycle ( Jahn , 1975 ) . In this case the continuous percolation of water to soil
surface ...
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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