File:Himalayan Tectonic Summary.png

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English: Seismicity in the Himalaya dominantly results from the continental collision of the India and Eurasia plates, which are converging at a relative rate of 40-50 mm/yr. Northward underthrusting of India beneath Eurasia generates numerous earthquakes and consequently makes this area one of the most seismically hazardous regions on Earth. The surface expression of the plate boundary is marked by the foothills of the north-south trending Sulaiman Range in the west, the Indo-Burmese Arc in the east and the east-west trending Himalaya Front in the north of India.
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Source https://earthquake.usgs.gov/earthquakes/tectonic/images/himalaya_tsum.pdf
Author United States Geological Survey

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This image is in the public domain in the United States because it only contains materials that originally came from the United States Geological Survey, an agency of the United States Department of the Interior. For more information, see the official USGS copyright policy.

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current10:53, 26 April 2015Thumbnail for version as of 10:53, 26 April 20152,658 × 1,723 (729 KB)Tatiraju.rishabh (talk | contribs)User created page with UploadWizard

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