|The Muonionalusta, on loan to the Prague National Museum in 2010. It is the largest meteorite ever exhibited in the Czech Republic.|
|Structural classification||Fine Octahedrite|
|Composition||Ni, Ga, Ge|
|Full slice (across 9.6 cm) of the Muonionalusta, showing the Widmanstätten pattern.|
The first fragment of the Muonionalusta was found in 1906 near the village of Kitkiöjärvi. Around forty pieces are known today, some being quite large. Other fragments have been found in a 25-by-15-kilometre (16 mi × 9.3 mi) area in the Pajala district of Norrbotten County, approximately 140 kilometres (87 mi) north of the Arctic Circle.
The meteorite was first described in 1910 by Professor A. G. Högbom, who named it "Muonionalusta", after a nearby place on the Muonio River. It was studied in 1948 by Professor Nils Göran David Malmqvist. The Munionalusta, probably the oldest meteorite known to man, marks the first occurrence of stishovite in an iron meteorite.
Studies have shown it to be the oldest discovered meteorite impacting the Earth during the Quaternary period, about one million years ago. It is quite clearly part of the iron core or mantle of a planetoid, which shattered into many pieces upon its fall on our planet. Since landing here this meteorite has experienced four ice ages. It was unearthed from a glacial moraine in the northern tundra. A strongly weathered surface covered with cemented faceted pebbles leaves no doubt that its sojourn on Earth has been long and dramatic.
New analysis of this strongly shock-metamorphosed iron meteorite has shown a content of 8.4% nickel and trace amounts of rare elements—0.33 ppm gallium, 0.133 ppm germanium and 1.6 ppm iridium. It also contains the minerals chromite, daubréelite, schreibersite, akaganéite and inclusions of troilite. For the first time, analysis has proved the presence of a form of quartz altered by extremely high pressure—stishovite, probably a pseudomorphosis after tridymite. From the article "First discovery of stishovite in an iron meteorite":
Stishovite, a high pressure polymorph of SiO2, is an exceptionally rare mineral...and has only been found in association with a few meteorite impact structures.... Clearly, the meteoritic stishovite cannot have formed by isostatic pressure prevailing in the core of the parent asteroid.... One can safely assume then that stishovite formation (in the Muonionalusta meteorite) is connected with an impact event. The glass component might have formed directly as a shock melt....
A 2010 study reported the lead isotope dating in the Muonionalusta meteorite and concluded the stishovite was from an impact event hundreds of millions of years ago: "The presence of stishovite signifies that this meteorite was heavily shocked, possibly during the 0.4 Ga [billion years] old breakup event indicated by cosmic ray exposure...."
Fragments of the Muonionalusta meteorite are held by numerous institutions around the world.
- Geological Institute, Uppsala, 15 kilograms (33 lb).
- Naturhistorisches Museum, Vienna, 96 gr.
- Museum für Naturkunde, Berlin, 82 gr.
- Max Planck Institute, Mainz, 96.3 gr.
- Paneth Collection (also at the Max Planck Institute), Mainz, 142.5 gr.
- National Museum of Natural History, Washington, 197 gr.
- American Museum of Natural History, New York, 84 gr.
- Field Museum of Natural History, Chicago, 65.2 gr.
- University of California, Los Angeles, 55 gr.
Additional information 
- Malmqvist, David: Structure of the Muonionalusta iron meteorite and a method of determining the orientation of lamellae of octahedrites, Almquist & Wiksells, Uppsala (1948), OCLC 494672409
- Holtstam, D., Broman, C., Söderhielm, J., Dan; Broman, C.; Söderhielm, J.; Zetterqvist, A. (2003). "First discovery of stishovite in an iron meteorite". Meteoritics & Planetary Science (Meteoritical Society) 38 (11): 1579. Bibcode:2003M&PS...38.1579H. doi:10.1111/j.1945-5100.2003.tb00002.x. More than one of
- Svensson, Daniel. "Muonionalusta". Muonionalusta Meteorites. Retrieved 2 November 2011.
- National Museums Scotland. "Muonionalusta meteorite". NMS. Retrieved 2 November 2011.
- Blichert-Toft, Janne; "The early formation of the IVA iron meteorite parent body", Earth and Planetary Science Letters, 296 (2010) pp. 469–480
- Monica M. Grady, A. L. Graham (2000). Catalogue of Meteorites. England: Cambridge University Press. p. 350. ISBN 0-521-66303-2.
See also 
- Muonionalusta at The Meteoritical Society Website