Jump to content

Twannberg meteorite

Coordinates: 47°7′28″N 7°10′44″E / 47.12444°N 7.17889°E / 47.12444; 7.17889
From Wikipedia, the free encyclopedia

This is an old revision of this page, as edited by Bibcode Bot (talk | contribs) at 09:26, 3 February 2018 (Adding 0 arxiv eprint(s), 2 bibcode(s) and 0 doi(s). Did it miss something? Report bugs, errors, and suggestions at User talk:Bibcode Bot). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

Twannberg
TypeIron
Structural classificationHexahedrite
GroupIIG
Parent bodyIIG-IIAB
CompositionMeteoric iron 5.1 % Ni (Kamacite), Schreibersite[1]
CountrySwitzerland
RegionCanton of Bern
Coordinates47°7′28″N 7°10′44″E / 47.12444°N 7.17889°E / 47.12444; 7.17889
Observed fallNo
Found date9 May 1984
TKW20.69 kilograms (45.6 lb) (6 fragments)[2]

The Twannberg meteorite is a hexahedrite iron meteorite. It is the only meteorite of the IIG group found in Europe and the largest meteorite ever found in Switzerland.[1]

Discovery and naming

The first fragment (15.91 kilograms (35.1 lb)) was found on 9 May 1984 in a barley field near Twann, after it had been ploughed (Twannberg I). Two additional fragments were found in an unnatural setting. One fragment (II) was found 2000 in an attic in Twann and another (III) in 2005 in the Naturhistorisches Museum Bern, in a collection received from the Museum Schwab in Biel where it had been labeled as hematite around 1930.[1] Twannberg IV, V and VI were found in the creek Twannbach.[2]

The meteorite is named after Twannberg (from German: Twann mountain), a mountain that lies north of Twann.

Original label of Twannberg mass III, written by Fritz Antenen (1867-1944). Eisenglanz is a German term for hematite.

The find location is a glacial till deposit. This paired with minerals found in the oxidized surface of the meteorite are an indicator that the meteorite fell on the Rhone glacier and was transported by it to Twann during the Würm ice age and then deposited there.[2]

Mineralogy

The meteorite is composed of meteoric iron and schreibersite. The meteoric iron has 5.1% Nickel, and is all in the form of kamacite. The preatmospheric mass was estimated to be at least 11,000 kilograms (24,000 lb). The surface of the meteorite is covered in an oxidation layer.[2]

Classification

The meteorite is classified as a member of group IIG.[3]

See also

References

  1. ^ a b c "Twannberg". Meteoritical Society.
  2. ^ a b c d Hofmann, Beda A.; Lorenzetti, Silvio; Eugster, Otto; Krähenbühl, Urs; Herzog, Gregory; Serefiddin, Feride; Gnos, Edwin; Eggimann, Manuel; Wasson, John T. (1 February 2009). "The Twannberg (Switzerland) IIG iron meteorites: Mineralogy, chemistry, and CRE ages". Meteoritics & Planetary Science. 44 (2): 187–199. Bibcode:2009M&PS...44..187H. doi:10.1111/j.1945-5100.2009.tb00727.x.
  3. ^ Wasson, John T.; Choe, Won-Hie (31 July 2009). "The IIG iron meteorites: Probable formation in the IIAB core". Geochimica et Cosmochimica Acta. 73 (16): 4879–4890. Bibcode:2009GeCoA..73.4879W. doi:10.1016/j.gca.2009.05.062.