Tenoumer crater: Difference between revisions
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The crater is exposed at the surface and is nearly circular. Edges of the crater rise up to {{cvt|110|m||}} high above the base of the crater, but the bottom of the crater is covered with approximately {{cvt|200|to|300|m}} thick layer of sediments.{{citation needed|date=August 2019}} |
The crater is exposed at the surface and is nearly circular. Edges of the crater rise up to {{cvt|110|m||}} high above the base of the crater, but the bottom of the crater is covered with approximately {{cvt|200|to|300|m}} thick layer of sediments.{{citation needed|date=August 2019}} |
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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 |
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,<ref>[http://www.wondermondo.com/Countries/Af/Mauritania/TirisZemmour/Tenoumer.htm METEORITE OR VOLCANO?]</ref> but current evidence clearly indicates an impact origin.<ref>{{cite web |author=Brügge, Norbert |url=http://www.b14643.de/Sahara/Mauritania%20Craters/index.htm |title=The "impact" craters of Mauritania: Aouelloul, Tenoumer, Temimichat and El Mrayer |url-status=dead |archiveurl=https://web.archive.org/web/20100223024521/http://www.b14643.de/Sahara/Mauritania%20Craters/index.htm |archivedate=2010-02-23 }}</ref> |
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Revision as of 05:49, 15 March 2021
Tenoumer crater | |
---|---|
Impact crater/structure | |
Confidence | Confirmed |
Diameter | 1.9 km (1.2 mi) |
Depth |
|
Age | 21,400 ± 9,700 |
Location | |
Coordinates | 22°55′5″N 10°24′27″W / 22.91806°N 10.40750°W |
Country | Mauritania |
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 its age is estimated to be 1.57 ± 0.14 million years old.[2]
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.[citation needed]
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,[3] but current evidence clearly indicates an impact origin.[4]
References
- ^ "Tenoumer". Earth Impact Database. Planetary and Space Science Centre University of New Brunswick Fredericton. Retrieved 2009-08-16.
- ^ Schultze, Dina Simona; Jourdan, Fred; Hecht, Lutz; Reimold, Wolf Uwe; Ralf-Thomas, Schmitt (2016). "Tenoumer impact crater, Mauritania: Impact melt genesis from a lithologically diverse target" (PDF). Meteoritics and Planetary Science. 51 (2). The Meteoritical Society: 323–350. Bibcode:2016M&PS...51..323S. doi:10.1111/maps.12593.
- ^ METEORITE OR VOLCANO?
- ^ Brügge, Norbert. "The "impact" craters of Mauritania: Aouelloul, Tenoumer, Temimichat and El Mrayer". Archived from the original on 2010-02-23.