Journal of Himalayan Geology, Volumes 1-2Wadia Institute of Himalayan Geology, 1990 - Geology |
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Page 185
... glacial and fluvial origin . Distinct ' U ' - shaped glacial troughs , hanging valleys , moraines , waterfalls and other landforms indicate a major phase of glacial activity in the area during the Pleistocene . The maximum limit up to ...
... glacial and fluvial origin . Distinct ' U ' - shaped glacial troughs , hanging valleys , moraines , waterfalls and other landforms indicate a major phase of glacial activity in the area during the Pleistocene . The maximum limit up to ...
Page 189
... glacial ice . At the leeward side of the mounds moulins are filled with glacial melt . The size of ablation moraines increases towards the snout and are 3-4 m high and consist of very coarse material , while as towards upper side of the ...
... glacial ice . At the leeward side of the mounds moulins are filled with glacial melt . The size of ablation moraines increases towards the snout and are 3-4 m high and consist of very coarse material , while as towards upper side of the ...
Page 194
... glacial advance was restricted between these static moraines and never touched the glacial trough . The second glacial advance was relatively weaker to erode the previously deposited lateral moraines and simply moved on previously ...
... glacial advance was restricted between these static moraines and never touched the glacial trough . The second glacial advance was relatively weaker to erode the previously deposited lateral moraines and simply moved on previously ...
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