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Page 124
1988 ) . MFS index is determined as Smf = Lmf / L where Smf is the mountain
front sinuosity , Lmf is the length of mountain front along the foot of mountain at
the pronounced break in slope and L is the straight line length of the mountain
front .
1988 ) . MFS index is determined as Smf = Lmf / L where Smf is the mountain
front sinuosity , Lmf is the length of mountain front along the foot of mountain at
the pronounced break in slope and L is the straight line length of the mountain
front .
Page 203
In the north / east facing Oytag Valley of the King Ata Tagh Mountains ( Fig . ... (
37°50 ' - 39°N , 74°40 ' - 75°40 ' E ) , the end moraines of marginal outletand
mountain glaciers suggest evidence , as for instance the Oytag - and Gez
Glaciers .
In the north / east facing Oytag Valley of the King Ata Tagh Mountains ( Fig . ... (
37°50 ' - 39°N , 74°40 ' - 75°40 ' E ) , the end moraines of marginal outletand
mountain glaciers suggest evidence , as for instance the Oytag - and Gez
Glaciers .
Page 251
The Siang Group has been classified into three formations - namely i ) Pari
Mountain , ii ) Singing and iii ) Yang Sang Chu in an ascending tectonic order .
Pari Mountain Formation : Named after the Pari Mountains , which forms a
spectacular ...
The Siang Group has been classified into three formations - namely i ) Pari
Mountain , ii ) Singing and iii ) Yang Sang Chu in an ascending tectonic order .
Pari Mountain Formation : Named after the Pari Mountains , which forms a
spectacular ...
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Contents
Evidence | 1 |
Tectonomagmatic Evolutionary Model of the KuluRampur | 47 |
Tectonic and Geochemical Signifcance of Black Shale | 65 |
Copyright | |
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Common terms and phrases
active Alaknanda Arunachal associated bands basin beds belt biotite Central characterized concentration Crystalline deformation Delhi deposits developed direction drainage Early east eastern elements et al evidence exposed extending fault field Figure folds Formation fractures further Garhwal Geol Geological Glacial glacier gneisses grains granite granitoids Group Himalaya India indicate Indus Kuhle Ladakh Late length Lesser limestone lineaments Lower Main major margin metamorphic moraines mountain nature ND ND normal northern Nummulitic observed occur Pakistan parallel pattern phyllites places plane plate Pleistocene Pradesh present quartzite range region represented resulted river rocks Saklani samples schist sediments sequence shale Siang districts side similar Siyom slide slope southern streams structural studies suggest surface Suture Table tectonic thick thrust Tibet trend unit upper valley values Volcanics western zone
Bibliographic information
| Title | Himalaya: Geological Aspects, Volume 4 Volume 15 of Current trends in geology Himalaya: Geological Aspects, P. S. Saklani, ISBN 8189304003, 9788189304003 Volume 4 of Himalaya:, P. S. Saklani, ISBN 8189304003, 9788189304003 |
| Editor | P. S. Saklani |
| Publisher | Satish Serial Publishing House, 2005 |
| Original from | the University of Michigan |
| Digitized | 19 Feb 2010 |
| ISBN | 818930402X, 9788189304027 |
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