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Tenoumer crater: Difference between revisions

Coordinates: 22°55′5″N 10°24′27″W / 22.91806°N 10.40750°W / 22.91806; -10.40750
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[[Image:Tenoumer x3.jpg|thumb|200px|right|Oblique [[Landsat]] image of Tenoumer crater draped over digital elevation model (x3 vertical exaggeration); screen capture from [[NASA World Wind]]]]
[[Image:Tenoumer x3.jpg|thumb|200px|right|Oblique [[Landsat]] image of Tenoumer crater draped over digital elevation model (x3 vertical exaggeration); screen capture from [[NASA World Wind]]]]


'''Tenoumer''' is an [[impact crater]] in [[Mauritania]].<ref>{{cite Earth Impact DB | name = Tenoumer| accessdate = 2009-08-16}}</ref>
'''Tenoumer''' is considered to be an [[impact crater]] in [[Mauritania]].<ref>{{cite Earth Impact DB | name = Tenoumer| accessdate = 2009-08-16}}</ref>


==Details==
==Details==

Revision as of 11:47, 16 August 2019

Tenoumer crater
Tenoumer crater is located in Africa
Tenoumer crater
Tenoumer crater
Asteroid impact location in Africa
Impact crater/structure
ConfidenceConfirmed
Diameter1.9 km (1.2 mi)
Depth
  • 110 m (360 ft) (currently exposed)
  • 300 to 400 m (980 to 1,310 ft) (originally)
Age21,400 ± 9,700
Location
Coordinates22°55′5″N 10°24′27″W / 22.91806°N 10.40750°W / 22.91806; -10.40750
CountryMauritania
Landsat image of the Tenoumer crater; screen capture from NASA World Wind
Oblique Landsat image of Tenoumer crater draped over digital elevation model (x3 vertical exaggeration); screen capture from NASA World Wind

Tenoumer is considered to be an impact crater in Mauritania.[1]

Details

The crater is located in the western Sahara Desert. It is 1.9 km (1.2 mi) in diameter and the age is estimated to be 21,400 ± 9,700 years old, placing it in the Pleistocene epoch.[2][3]

The crater is exposed at the surface and is nearly circular. Edges of the crater rise up to 110 m (360 ft) high above the base of the crater, but the bottom of the crater is covered with approximately 200 to 300 m (660 to 980 ft) thick layer of sediments.

Tenoumer crater has formed in gneiss and granite of Precambrian peneplain with a thin layer of Pliocene sediments (no older). The crater is believed to be caused by an impact event due to basement rocks found outside the crater. A volcanic origin was once theorized because of the discovery of basalt and rhyodacite outside of the crater basin, but current evidence clearly indicates an impact origin.

References

  1. ^ "Tenoumer". Earth Impact Database. Planetary and Space Science Centre University of New Brunswick Fredericton. Retrieved 2009-08-16.
  2. ^ Jaret, S. J.; Kah, L. C.; French, B. M. (2009). "40th Lunar and Planetary Science Conference" (PDF). Lunar and Planetary Institute. {{cite web}}: |chapter= ignored (help)
  3. ^ Storzer, D.; Selo, M.; Latouche, L.; Fabre, J. (2003). "The Age of Tenoumer Crater, Mauritania, Revisited" (PDF). XXXIV. Lunar and Planetary Institute. {{cite journal}}: Cite journal requires |journal= (help)