Roter Kamm crater
Roter Kamm, aerial view direction south (April 2017)
Impact crater/structure
ConfidenceConfirmed
Diameter2.5 km (1.6 mi)
Age4.81 ± 0.5 Ma
Zanclean
ExposedYes
DrilledNo
Location
LocationSperrgebiet, Namib Desert
Coordinates27°46′0″S 16°17′20″E / 27.76667°S 16.28889°E / -27.76667; 16.28889
CountryNamibia
StateǁKaras Region
Roter Kamm crater is located in Namibia
Roter Kamm crater
Location of the crater in Namibia

Roter Kamm (German: Red Ridge) is a meteorite crater, located in the Sperrgebiet, within the Namibian section of the Namib Desert, approximately 80 kilometres (50 mi) north of Oranjemund and 12 kilometres (7.5 mi) southwest of Aurus Mountain in the ǁKaras Region. The crater is 2.5 kilometres (1.6 mi) in diameter and is 130 metres (430 ft) deep. The age is estimated at 4.81 ± 0.5 Ma, placing it in the Pliocene.[1] The crater is exposed at the surface, but its original floor is covered by sand deposits at least 100 metres (330 ft) thick.

Description

The meteorite hit a layer of Precambrian granitic gneiss that is part of the Namaqua Metamorphic Complex, overlaid with some younger sedimentary rocks. No parts of the meteorite have been found, suggesting that it completely evaporated upon impact.[2] The meteor that hit it was approximately the size of an SUV.[3]

The Roter Kamm impact structure exposes a large volume of cataclastic/mylonitic and pseudotachylitic breccias in the basement granite and gneisses, which is unusual for small craters.[4] Anomalous quartz found at the rim of the crater, and the primary fluid inclusions in the quartz, seem to provide evidence for post-impact hydrothermal activity, generated by impact heat, at the Roter Kamm impact crater.[5] Eolian and alluvial processes each played a role in modifying the Roter Kamm impact crater since its formation. Much of the more recent history of crater modification relates to eolian processes. Active mobile sands largely bury the crater and effectively mask most of the signatures associated with prior activity by other processes. Ongoing eolian erosion is responsible for scouring of the exposed rim.[6]

Gallery

See also

References

  1. ^ Hecht et al., 2008, p.1216
  2. ^ "Roter Kamm crater". Wondermondo.
  3. ^ "Roter Kamm". Earth Impact Database. Planetary and Space Science Centre University of New Brunswick Fredericton. Retrieved 2009-08-16.
  4. ^ Reimold et al., 1994, p.2703
  5. ^ Koeberl et al., 1989, p.2118
  6. ^ Grant et al., 1997, p.16,334

Bibliography

Further reading