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The Richardton meteorite is a 90 kilograms (200 lb) H5 Ordinary chondrite that was seen to fall at 21:48 on 30 June 1918 between Mott, North Dakota and Richardton, North Dakota, United States.[1][2]

Richardton meteorite
TypeChondrite
ClassOrdinary chondrite
GroupH5
CountryUnited States
RegionRichardton, North Dakota
Coordinates46°37′30″N 102°16′17″W
Observed fallYes
Fall date1918-06-30
TKW90 kilograms (200 lb)
Strewn fieldYes
Related media on Wikimedia Commons

Pieces were found in a strewn field of about 9 miles (14 km) by 5 miles (8.0 km) centred on 46°37′30″N 102°16′17″W and oriented north–south.[2] As of December 2012 pieces of this meteorite were for sale online at up to US$80/g.[3]

In 1960 John Reynolds discovered that the Richardton meteorite had an excess of 129Xe, a result of the presence of 129I in the solar nebula.[4][5]


Mineralogy



Classification



See also



References


  1. "Richardton". Meteoritical Bulletin Database. Meteoritical Society. Retrieved 24 December 2012.
  2. Quirke, T. T. (Sep–Oct 1919). "The Richardton Meteorite". The Journal of Geology. The University of Chicago Press. 27 (6): 431–448. Bibcode:1919JG.....27..431Q. doi:10.1086/622670. JSTOR 30057982.
  3. "Richardton". Meteorites and Related Geology Specimens for Sale. New England Meteoritical Services. Retrieved 24 December 2012.
  4. Reynolds, J. (31 March 1960). "Isotopic Composition of Primordial Xenon". Physical Review Letters. 4 (7): 351–354. Bibcode:1960PhRvL...4..351R. doi:10.1103/PhysRevLett.4.351.
  5. "John Hamilton Reynolds, 77; Improved Study of Cosmic Ages". Retrieved 25 December 2012.



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[de] Richardton (Meteorit)

Richardton ist ein als H5-Chondrit klassifizierter Meteorit. Er fiel am 30. Juni 1918 in North Dakota, USA. Insgesamt wurden 90 kg geborgen.
- [en] Richardton meteorite



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