Journal of Himalayan Geology, Volumes 1-2Wadia Institute of Himalayan Geology, 1990 - Geology |
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Page 189
... moraines : These are confined to the altitudinal range of 3700 to 4300 m . The length of ablation moraine zone in ... moraines are most probably formed by the disintegration of medial moraines due to divergent flow of the glacier in the ...
... moraines : These are confined to the altitudinal range of 3700 to 4300 m . The length of ablation moraine zone in ... moraines are most probably formed by the disintegration of medial moraines due to divergent flow of the glacier in the ...
Page 193
... moraine lateral channels were developed and formed distinct lateral valleys which gradually widened out due to continous erosion and shift of the lateral moraines . Later on these lateral valleys were blocked at several places by down ...
... moraine lateral channels were developed and formed distinct lateral valleys which gradually widened out due to continous erosion and shift of the lateral moraines . Later on these lateral valleys were blocked at several places by down ...
Page 194
... moraines on both sides of the glacier are the remanants of past glaciations . At a later stage glacial advance was restricted between these static moraines and never touched the glacial trough . The second glacial advance was relatively ...
... moraines on both sides of the glacier are the remanants of past glaciations . At a later stage glacial advance was restricted between these static moraines and never touched the glacial trough . The second glacial advance was relatively ...
Contents
RAJESH SHARMA B K NAYAK Ore petrology and origin of leadzinc deposits in great limestone | 103 |
R K MAZARI T N BAGATI Postcollision graben development in the Spiti valley Himachal | 111 |
P Dobhal SURENDAR KUMAR A K MUNDEPI Mass wasting and slope analysis of Chhota | 119 |
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amphibolite Amritpur Amritpur Granite basin beds biotite block chlorite clasts conglomerate Cretaceous Crystallines deformation deposits developed dolerite dolomite earthquakes eastern Eocene evaporites facies fault feldspars folds fossils Garhwal Garhwal Himalaya garnet Geol glacial glacier gneisses Gondwana grained granitoids Group Himachal Pradesh Himalaya Himalayan Geology hornblende hornblende schists India Indian plate indicate Indus Suture Institute of Himalayan Jour Journal of Himalayan K-feldspar Krol Belt Kumar Kumaun Ladakh Lesser Himalaya limestone lineaments lithology lower magmatic margin metamorphism Middle Siwalik migmatites minerals Molnar moraines muscovite Nayar observed occur ophiolitic Ophiolitic Melange Pakistan phase phyllite plagioclase plane Precambrian quartz quartzite Rawat region river rocks Salt Range samples sandstone schist sedimentary sediments sequence shale Sharma shear zones shows Shyok Singh Siwalik slope Spiti stratigraphic structure Subathu Subathu Formation subduction Surv Suture Zone syncline tectonic Tethyan Thakur thick Thrust trend Upper Siwalik valley volcanics Wadia Institute western Zanskar