ꯐꯥꯏꯜ:Himalayan Tectonic Summary.png
ꯃꯁꯤꯒꯤ ꯄ꯭ꯔꯚꯤꯌꯨ ꯑꯁꯤꯒꯤ ꯁꯥꯏꯓ: ২২০ × ১৪৩ ꯄꯤꯛꯆꯦꯜꯁ. ꯑꯇꯩ ꯁꯦꯡꯅ ꯌꯦꯡꯕ ꯌꯥꯕ: ৩২০ × ২০৭ ꯄꯤꯛꯆꯦꯜꯁ | ২,৬৫৮ × ১,৭২৩ ꯄꯤꯛꯆꯦꯜꯁ.
ꯐꯥꯏꯜ ꯑꯁꯦꯡꯕ (২,৬৫৮ × ১,৭২৩ ꯄꯤꯛꯆꯦꯜꯁ, ꯐꯥꯏꯜ ꯆꯥꯎꯕꯒꯤ ꯆꯥꯡ: ৭২৯ KB, MIME ꯃꯈꯜ: image/png)
ꯑꯇꯦꯟꯕꯥ ꯁꯟꯗꯣꯛꯅꯥ ꯇꯥꯛꯄꯥ
| ꯁꯟꯗꯣꯛꯅꯥ ꯇꯥꯛꯄꯥHimalayan Tectonic Summary.png |
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. |
| ꯆꯩꯆꯠ | |
| ꯍꯧꯔꯛꯐꯛ | https://earthquake.usgs.gov/earthquakes/tectonic/images/himalaya_tsum.pdf |
| ꯄꯨꯊꯣꯛꯂꯤꯕ ꯃꯤ | United States Geological Survey |
ꯑꯌꯥꯕꯥ
| Public domainPublic domainfalsefalse |
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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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