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Zhamanshin crater | |
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Jaman şıñ | |
Impact glass from the Zhamanshin impact site | |
Impact crater/structure | |
Confidence | Confirmed |
Diameter | 14 km (8.7 mi) |
Age | 900,000 ± 100,000 years Mid Pleistocene |
Exposed | Yes |
Drilled | Yes |
Bolide type | Chondrite |
Location | |
Coordinates | 48°24′N 60°58′E / 48.400°N 60.967°E / 48.400; 60.967 |
Country | Kazakhstan |
State | Aktobe Region |
Location of the crater in Kazakhstan |
Zhamanshin (Kazakh: Жаман шың, romanized: Jaman shun) is a meteorite crater in Kazakhstan. It is 14 kilometres (8.7 mi) in diameter and the age is estimated to be 900,000 ± 100,000 years (Pleistocene). The crater is exposed at the surface.
Description
It is believed that the Zhamanshin crater is the site of the most recent meteorite impact event of the magnitude that could have produced a disruption comparable to that of a nuclear winter, but it was not sufficiently large enough to have caused a mass extinction.
Preliminary papers in the late 1970s suggested either Elgygytgyn, or Zhamanshin, as the source of the Australasian strewnfield.
References
- "Zhamanshin". Earth Impact Database. Planetary and Space Science Centre University of New Brunswick Fredericton. Retrieved 2017-10-09.
- Essay "Impact Cratering on Earth", based on: R.A.F. Grieve, 1990, Impact cratering on the Earth, Scientific American, v. 262, 66-73. Archived 23 September 2010 at the Wayback Machine
- R.S. Dietz (1977), Elgygytgyn Crater, Siberia: Probable Source Of Australasian Tektite Field Meteoritics, June 1977, Vol 12, Issue 2, p. 145–157
- B.P. Glass (1979), Zhamanshin crater, a possible source of Australasian tektites? Geology, July 1979, v. 7, p. 351-353
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