Gweni-Fada crater

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Gweni-Fada crater
Gweni-Fada crater.jpg
Landsat image of the Gweni-Fada crater; screen capture from NASA World Wind
Impact crater/structure
ConfidenceConfirmed
Diameter14 km (8.7 mi)
Age <345 Ma
<Early Carboniferous
ExposedYes
DrilledNo
Location
Location Sahara
Coordinates 17°25′7″N21°45′8″E / 17.41861°N 21.75222°E / 17.41861; 21.75222
Country Chad
State Ennedi-Ouest
Chad adm location map.svg
Map pointer.svg
Location of the crater in Chad
Gweni-Fada crater viewed from the International Space Station ISS021-E-5375 Gweni-Fada crater.jpg
Gweni-Fada crater viewed from the International Space Station
Oblique Landsat image of Gweni-Fada crater draped over digital elevation model (x2 vertical exaggeration); screen capture from NASA World Wind Gweni-Fada crater x2.jpg
Oblique Landsat image of Gweni-Fada crater draped over digital elevation model (x2 vertical exaggeration); screen capture from NASA World Wind

Gweni-Fada is a meteorite crater in the Ennedi Plateau, Chad. [1] [2]

Contents

The Gweni Fada structure was first noted on the map NE 34 X Fada of the IGN (National Geographic Institute France) and aerial photographs in the 1950s of IGN by Alain Beauvilain (Paris X- Nanterre University). In April 1995, at the initiative of CNAR (National Center to Help Research of Chad) a team of French geologists (Pierre Vincent, University of Clermont-Ferrand, Alain and Najia Beauvilain, CNAR Chad) visited the site and reported evidence of shock metamorphism within rock samples they had collected inside the structure.

Centered at 17°25′N and 21°45′E, being slightly wider in the NW-SE direction (cf. topographic map), the asymmetric structure is deeply eroded. A broad depression (diameter 12 km) forms a crescent around two thirds of the inner complex zone. On the northern side, an elevated outer ring of outward-dipping sandstones surrounds the depression. In its south, the external depression is absent. The inner zone (diameter 10 km) consists of a rugged terrain with hills several hundred meters in height. The latter may be remnants of the central uplift (see topographic map).

The age is estimated to be less than 345 million years (Carboniferous). It is older than that of Aorounga because its coverage of impactite has disappeared as a result of erosion.

Topographic map of Gweni-Fada crater Gweni-Fada crater.png
Topographic map of Gweni-Fada crater

See also

References

  1. "Gweni-Fada". Earth Impact Database . Planetary and Space Science Centre University of New Brunswick Fredericton . Retrieved 2009-08-13.
  2. VINCENT P.M., BEAUVILAIN A., The circular structure of Gweni-Fada, Ennedi : a new meteoritic impact crater in northern Chad. C.R. Acad. Sci. Paris, t. 323, série II a, pp. 987-997, 1996.

Further reading