Luizi crater explained

Luizi crater
Other Name:Luizi impact structure
Map:Democratic Republic of the Congo
Age:<542 myr (basement rock age)
Confidence:Confirmed
Diameter:17km (11miles)
Exposed:Yes
Drilled:No
Country:Democratic Republic of the Congo
Province:Haut-Katanga Province

Luizi is a meteorite impact structure that lies on the Kundelungu Plateau of Haut-Katanga province, in an underexplored region of southeastern Democratic Republic of the Congo.[1] The crater, ~17 kilometer in diameter, is visible from satellite imagery, and has been confirmed in 2011 by Ferrière et al.[2] as being caused by a large impact event. This complex meteorite impact crater is so far the only recognized one in the Democratic Republic of the Congo and even in the whole Central Africa.[3]

The crater was initially described as a semi-circular basin by German geologist E. Grosse in 1919.[4]

See also

References

-10.1667°N 28°W

Notes and References

  1. Luizi . 2016-04-08.
  2. The newly confirmed Luizi impact structure, Democratic Republic of Congo—Insights into central uplift formation and post-impact erosion . 10.1130/G31990.1 . 2011 . Ferrière . Ludovic . Lubala . François R.T. . Osinski . Gordon R. . Kaseti . Pierre K. . Geology . 39 . 9 . 851–854 . 2011Geo....39..851F .
  3. Web site: Archived copy . 2011-11-22 . 2011-11-11 . https://web.archive.org/web/20111111113809/http://news.nationalgeographic.com/news/2011/03/110308-meteor-impact-crater-found-confirmed-congo-ferriere-science . dead .
  4. E. Grosse, 1919. Grundlinien der Geologie und Petrographie des östlichen Katanga. Neues Jahrbuch Mineralogie, Geologie and Paläontologie, 42, 272–419. Google Book