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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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{{Short description|Impact crater in Mauritania}}
{{Infobox terrestrial impact site
{{Infobox terrestrial impact site
| name = Tenoumer crater
| name = Tenoumer crater
| other_name =
| other_name =
| photo =
| photo = Tenoumer Krater.jpg
| photo_caption =
| photo_caption =
| map = Africa
| map = Africa
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'''Tenoumer''' is considered to be 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>
[[Image:Tenoumer.jpg|thumb|left|[[Landsat]] image of the Tenoumer crater; screen capture from [[NASA World Wind]]]]
[[Image:Tenoumer x3.jpg|thumb|left|Oblique [[Landsat]] image of Tenoumer crater draped over digital elevation model (x3 vertical exaggeration); screen capture from [[NASA World Wind]]]]


==Details==
==Details==
The crater is located in the western [[Sahara Desert]]. It is {{cvt|1.9|km||}} in diameter and the age is estimated to be 21,400 ± 9,700 years old, placing it in the [[Pleistocene]] [[Epoch (geology)|epoch]].<ref>{{cite web |url=http://www.lpi.usra.edu/meetings/lpsc2009/pdf/1281.pdf |publisher=Lunar and Planetary Institute |title=40th Lunar and Planetary Science Conference |year=2009 |chapter=Petrographic Investigation of Ejecta from the Tenoumer Impact Crater, Mauritania |last1=Jaret |first1=S. J. |last2=Kah |first2=L. C. |last3=French |first3=B. M. }}</ref><ref>{{cite journal |url=http://www.lpi.usra.edu/meetings/lpsc2003/pdf/1183.pdf |publisher=Lunar and Planetary Institute |title=The Age of Tenoumer Crater, Mauritania, Revisited |year=2003 |volume=XXXIV |last1=Storzer |first1=D. |last2=Selo |first2=M. |last3=Latouche |first3=L. |last4=Fabre |first4=J. }}</ref>
The crater is located in the western [[Sahara Desert]]. It is {{cvt|1.9|km||}} in diameter and its age was estimated to be 21,400 ± 9,700 years old but as of 2016, is thought to be ~1.57 Ma.<ref>{{cite journal |url=http://www.lpi.usra.edu/meetings/lpsc2003/pdf/1183.pdf |publisher=The Meteoritical Society |title=Tenoumer impact crater, Mauritania: Impact melt genesis from a lithologically diverse target |journal=Meteoritics and Planetary Science |year=2016 |volume=51 |issue=2 |pages=323–350 |last1=Schultze |first1=Dina Simona |last2=Jourdan |first2=Fred |last3=Hecht |first3=Lutz |last4=Reimold |first4=Wolf Uwe |last5=Ralf-Thomas |first5=Schmitt |doi=10.1111/maps.12593|bibcode=2016M&PS...51..323S |doi-access=free }}</ref>


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 an approximately {{cvt|200|to|300|m}} thick layer of sediments.<ref>{{Cite web |title=Tenoumer Crater, Mauritania |url=https://www.esa.int/ESA_Multimedia/Images/2022/06/Tenoumer_Crater_Mauritania |access-date=2022-11-20 |website=www.esa.int |language=en}}</ref>


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.{{citation needed|date=August 2019}}
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>
{{clear}}
{{clear}}

==References==
==References==
{{reflist}}
<references/>
* {{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 |deadurl=yes |archiveurl=https://web.archive.org/web/20100223024521/http://www.b14643.de/Sahara/Mauritania%20Craters/index.htm |archivedate=2010-02-23 |df= }}


==External links==
==External links==
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[[Category:Impact craters of Mauritania]]
[[Category:Impact craters of Mauritania]]
[[Category:Pleistocene impact craters]]
[[Category:Pleistocene impact craters]]


{{Earth-crater-stub}}

Latest revision as of 00:51, 27 July 2023

Tenoumer crater
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
Tenoumer crater is located in Africa
Tenoumer crater
Tenoumer crater
Asteroid impact location in Africa

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

Details

[edit]

The crater is located in the western Sahara Desert. It is 1.9 km (1.2 mi) in diameter and its age was estimated to be 21,400 ± 9,700 years old but as of 2016, is thought to be ~1.57 Ma.[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 an approximately 200 to 300 m (660 to 980 ft) thick layer of sediments.[3]

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,[4] but current evidence clearly indicates an impact origin.[5]

References

[edit]
  1. ^ "Tenoumer". Earth Impact Database. Planetary and Space Science Centre University of New Brunswick Fredericton. Retrieved 2009-08-16.
  2. ^ 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.
  3. ^ "Tenoumer Crater, Mauritania". www.esa.int. Retrieved 2022-11-20.
  4. ^ METEORITE OR VOLCANO?
  5. ^ Brügge, Norbert. "The "impact" craters of Mauritania: Aouelloul, Tenoumer, Temimichat and El Mrayer". Archived from the original on 2010-02-23.
[edit]