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Erebus (crater)

Coordinates:2°06′S5°30′W / 2.1°S 5.5°W /-2.1; -5.5
From Wikipedia, the free encyclopedia
Crater on Mars
This article is about theimpact crater onMars. For other uses, seeErebus (disambiguation).
Crater on Mars
Erebus
Erebus, as seen by HiRISE.
PlanetMars
RegionMeridiani Planum
Coordinates2°06′S5°30′W / 2.1°S 5.5°W /-2.1; -5.5
QuadrangleMargaritifer Sinus
Diameter~350 metres
DepthEffectively zero depth
DiscovererOpportunity rover
EponymHMSErebus
Erebus is located near the center of this satellite image.

Erebus is acrater lying situated within theMargaritifer Sinus quadrangle (MC-19) region of the planetMars, this extraterrestrial geological feature was visited by theOpportunity rover on the way to the much larger craterVictoria. It is named after the polar exploration vesselHMSErebus which was used byJames Clark Ross in 1841 to discover theGreat Ice Barrier, now known as theRoss Ice Shelf. The rover was in the immediate vicinity of the crater from approximatelysol 550 to 750 (October 2005 to March 2006).

This crater features two other minor named outcrops on the edges of this topographical depression. These includePayson Ridge andOlympia Ridge (see gallery below).

Erebus is located roughly 2,500 metres (8,200 ft) south of the much smaller craterVostok, which was previously visited byOpportunity. It is located within a type of terrain that a team of scientists led by J. M. Metz described as "etched terrain". The etched terrain is characterized by heavily eroded rocks that form polygonal structures separated by ridges and valleys.[1]

Erebus is about 350 metres (1,150 ft) wide, twice as large as the craterEndurance. However, it is very old and eroded, and is barely visible from the ground; it appears merely as a number of flat rocky outcrops encircling a region ofdunes.

  • An outcrop named "Payson", on the western edge of Erebus.
    An outcrop named "Payson", on the western edge of Erebus.
  • "Olympia" outcrop on northwestern margin of Erebus
    "Olympia" outcrop on northwestern margin of Erebus
  • Color panorama taken by Opportunity on the rim of Erebus. The crater itself can be seen in the center of the pan, at the top.
    Color panorama taken byOpportunity on the rim of Erebus. The crater itself can be seen in the center of the pan, at the top.

See also

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References

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  1. ^Metz, J. M.; Grotzinger, J. P.; Rubin, D. M.; Lewis, K. W.; Squyres, S. W.; Bell, J. F. (1 May 2009). "Sulfate-Rich Eolian and Wet Interdune Deposits, Erebus Crater, Meridiani Planum, Mars".Journal of Sedimentary Research.79 (5):247–264.doi:10.2110/jsr.2009.033.

External links and further reading

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