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Ottawa meteorite, Franklin Co., Kansas, USA

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Latitude & Longitude (WGS84): 38° 36' North , 95° 13' West
Latitude & Longitude (decimal): 38.60000,-95.21667
Non-native locality type:Meteorite
Meteorite Class:LL6 chondrite meteorite
Meteoritical Society Class: LL6
Metbull:View entry in Meteoritical Bulletin Database
KΓΆppen climate type:Cfa : Humid subtropical climate


Ordinary chondrite, brecciated (LL6)
Fall, 9 April 1896; 840 g, single stone

In the late afternoon a series of rapid fire detonations were followed by a whirring sound and a thud. A very surprised farmer attempted to locate the fallen object, but was unable to find anything that day. The next morning his sister found a small meteorite, largely covered with a fusion crust, embedded in the ground about 200 m away from where the farmer had first stood. Detonations had been heard up to 50 km from the impact. The broken portions revealed a light grey chondritic interior with silicate-rich chondrules embedded in a matrix of silicates and opaques. Chondrules of granular olivine (up to 5 mm in diameter) and rarer fine-grained pyroxenes are present. Silicates in both chondrules and matrix β€” olivine, orthopyroxene, and lesser albitic plagioclase β€” are accompanied by troilite (~6 wt%) and Fe-Ni metal (~4 wt%). Kamacite and taenite are found both as separate and as contiguous grains. A number of very minor accessory opaques are also reported.

Total iron (21.24 wt%), olivine composition (Fa28), and orthopyroxene composition (Fs25) are characteristic of the LL, very low iron, chondrite group. The LL chondrite group is the smallest of the 3 ordinary chondrite groups and representS ~10 % of all witnessed meteorite falls. Ottawa itself is one of 42 witnessed falls classified exactly as petrologic type 'LL6' at the Meteoritical Bulletin Database (February 2016).

A moderately long cosmic ray exposure age of ~45 Ma has been reported.


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9 valid minerals.

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This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders for access and that you are aware of all safety precautions necessary.

References

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Mason, B. & Wiik, H.B. (1961) The Composition of the Ottawa, Chateau-Renard, Mocs, and New Concord Meteorites: American Museum Novitates, #2069: 26 pp. (Dec 1961).
Mason, B. (1962) The Classification of Chondritic Meteorites: American Museum Novitates, #2085. New York. 20 pp. (May 1962).
Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites.Elsevier Publishing Company: Amsterdam; London: New York. 245 pages.
Saxena, S.K. (1976) Two-pyroxene geothermometer: a model with an approximate solution. American Mineralogist 61(7&8): 643-652. (July-August 1976).
Grady, M.M. (2000). Catalogue of Meteorites (5/e). Cambridge University Press: Cambridge; New York; Oakleigh; Madrid; Cape Town. 689 pages.

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