Shelter Island meteorite explained

Shelter Island meteorite
Type:Iron
Parent Body:Unknown
Weathering:Large-scale, cavernous weathering
Country:Mars
Region:Meridiani Planum
Lat Long:-2.1178°N -5.5281°W[1]
Observed Fall:No
Fall Date:Possibly late Noachian
Found Date:December 1, 2009
Strewn Field:Possibly
Image2 Caption:Shelter Island meteorite - close-up (October 1, 2009).

Shelter Island meteorite was found on Mars by the Opportunity rover on October 1, 2009. It is about long.[2]

History

Shelter Island was the second of three iron meteorites encountered by the rover on Meridiani Planum within a few hundred meters, the others being Block Island and Mackinac Island.[3]

Shelter Island may have fallen on Mars in the late Noachian period and is extensively weathered.[4]

See also

Notes and References

  1. Google Mars
  2. Web site: Opportunity Finds Another Meteorite. NASA. January 5, 2013.
  3. Ashley. J. W.. etal . Evidence for mechanical and chemical alteration of iron-nickel meteorites on Mars: Process insights for Meridiani Planum. Journal of Geophysical Research: Planets. July 2011. 116. E7. E00F20. 10.1029/2010JE003672. 2011JGRE..116.0F20A . 1893/17110. free.
  4. Beech. Martin. Ian M. Coulson. The making of Martian meteorite Block Island. Monthly Notices of the Royal Astronomical Society. 2010. 404. 3. 1457. 10.1111/j.1365-2966.2010.16350.x. 2010MNRAS.404.1457B.