Himalaya: Geological Aspects, Volume 4Contributed articles. |
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Page 96
Aungi Slide : This is located on the Uttarkashi - Gangotri road near village Aungi .
It is 2 km from Maneri towards Bhatwari . This is an old landslide , which was
activated after the earthquake of 1991 . The distance from crown to base of the
slide ...
Aungi Slide : This is located on the Uttarkashi - Gangotri road near village Aungi .
It is 2 km from Maneri towards Bhatwari . This is an old landslide , which was
activated after the earthquake of 1991 . The distance from crown to base of the
slide ...
Page 101
The distance from crown to base is 700 meters and the width is nearly 550
meters . The angle of slope is 60° on the top , 10o - 20° in the middle and 50° at
the base . Pulverised granite gneisses and water seepage is confined to the
central ...
The distance from crown to base is 700 meters and the width is nearly 550
meters . The angle of slope is 60° on the top , 10o - 20° in the middle and 50° at
the base . Pulverised granite gneisses and water seepage is confined to the
central ...
Page 278
It is possible, therefore, as seen from the small faunal assemblage that the base
of this sequence of shale-limestone at the top of Muth Quartzite, which is thinner
at the type area of Muth and thicker (up to 1 10 m) at 278 Himalaya (Geological ...
It is possible, therefore, as seen from the small faunal assemblage that the base
of this sequence of shale-limestone at the top of Muth Quartzite, which is thinner
at the type area of Muth and thicker (up to 1 10 m) at 278 Himalaya (Geological ...
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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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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