Journal of Himalayan Geology, Volume 5Wadia Institute of Himalayan Geology, 1994 - Geology |
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Page 42
The orography and slope aspect also play very significant role in the distribution
of rainfall in the area and this rainfall intum controls the distribution and location
of landslide -prone areas (Rudra et al., l982). Under heavy saturation most of the
...
The orography and slope aspect also play very significant role in the distribution
of rainfall in the area and this rainfall intum controls the distribution and location
of landslide -prone areas (Rudra et al., l982). Under heavy saturation most of the
...
Page 121
The thickness of black soil horizon varies from 75 cm near Kurdhara to 10-20 cm
in the entire mid hill slope. At few places these black soil horizones show 8-l0
layers, each having a thickness between 5-10 cm and at places show active
creep ...
The thickness of black soil horizon varies from 75 cm near Kurdhara to 10-20 cm
in the entire mid hill slope. At few places these black soil horizones show 8-l0
layers, each having a thickness between 5-10 cm and at places show active
creep ...
Page 123
Mass Movement of Pcriglacial Material along the Uhl Valley Slope 0 —
Downward culling ol glacial deposit lM) due to increase Ifl discharge b— Gradual
uplift rapid erosion and formation of periglacial slope c -( i) Solitluction and
periglacial ...
Mass Movement of Pcriglacial Material along the Uhl Valley Slope 0 —
Downward culling ol glacial deposit lM) due to increase Ifl discharge b— Gradual
uplift rapid erosion and formation of periglacial slope c -( i) Solitluction and
periglacial ...
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Contents
Cnouasv KEWAL K SHARMA D RAMESHWAR RAO Crustal anatexis | 1 |
N S VIRDI Basement Structures and their possible relation to Sedimentation and Tectonics in | 21 |
G S MEHROTRA S SARKAR D P KANUNGO A geological appraisal of Landslide Hazards | 35 |
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Common terms and phrases
02:53 IST MAGNITUDE acanthomorphic acritarchs Agglomeratic Slate Amritpur axial plane Bafliaz Formation band basin biotite Budhal calcite chert classified clasts conglomerate defined deformation Dehra Dun deposits diamictite dolomite Doushantuo Formation Dum Gali Quartzite facies fault plane feldspar fi'om field figure fine first flank flows folds foliation fossils Garhwal Geol glacial gneiss granites granitoids grey Gulabgarh Himachal Himalaya Himalayan Geology inversion Jour Jutogh Kashmir Kharnak Krol Ladakh landslides Lesser Himalaya limestone lineation lndia lnfrakrol metamorphic Nappe ofthe Panjal thrust Parautochthonous belt pebbles periglacial Permian phyllites Pir Panjal range plagioclase porphyries Proterozoic quartz quartzite Rampur Ramsu region rocks Salkhala samples sandstone schist sector sedimentary sediments sequence shale Sharma shear Shergol significance SiO2 slide slip slope soil stratigraphic structures Surv Suture Zone tectonic Tethyan Thakur thick Thinly bedded Uhl valley unconformably upper UTTARKASHI UTTARKASHI EARTHQUAKE Verma Wadia Institute WIMF/A Zanskar