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Geology of the Himalayas - Wikipedia
The geology of the Himalayas is a record of the most dramatic and visible creations of the immense mountain range formed by plate tectonic forces and sculpted by weathering and erosion. The Himalayas, which stretch over 2400 km between the Namcha Barwa syntaxis at the eastern end of the mountain … See more
During Late Precambrian and the Palaeozoic, the Indian subcontinent, bounded to the north by the Cimmerian Superterranes, was part of Gondwana and was separated from Eurasia by the Paleo-Tethys Ocean (Fig. … See more
Localized geology and geomorphology topics for various parts of the Himalaya are discussed on other pages:
• Geology of Nepal
• Zanskar is a subdistrict of the Kargil district, which lies in the eastern half of the Indian union territory of See moreThe modern day rate of convergence between the Indian and Eurasian plates is measured to be approximately 17 mm/yr. This convergence is accommodated through seismic … See more
• Catlos, Elizabeth Jacqueline (2000). Geochronologic and Thermobarometric Constraints on the Evolution of the Main Central Thrust, Himalayan Orogen (PDF). PhD Thesis. University of California.
• "Geology and Petrographic study of the area from Chiraundi … See moreWikipedia text under CC-BY-SA license - bing.com/videosWatch full video
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Geological map of the Himalaya. Fig. 2 . Photograph taken from the Space Shuttle looking west along the Himalaya with the outline of the major structural divisions and major faults of the Himalaya.
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Himalayas - Peaks, Glaciers, Rivers | Britannica
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