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Broken Bow meteorite, Custer Co., Nebraska, USA

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Latitude & Longitude (WGS84): 41° 26' North , 99° 42' West
Latitude & Longitude (decimal): 41.43333,-99.70000
Non-native locality type:Meteorite
KΓΆppen climate type:Dfa : Hot-summer humid continental climate


Ordinary chondrite (H4)
Find, 1937; 6.8 kg

A single stone was found. Inspections reveal distinct chondrules, chondrule fragments, and Fe-Ni metal within a moderately equilibrated and sometimes weathered matrix. Compositionally, mostly equilibrated olivine (Fa20) and roughly equilibrated low Ca-pyroxene are characteristic of H4-chondrites. Mineralogically, the meteorite consists primarily of dominant olivine and pyroxene along with minor plagioclase, troilite, and Fe-Ni metal. Accessory chromite and very minor copper, ilmenite, isocubanite, and mackinawite are also reported.

As with many meteorites collected by Harvey Nininger, a moderately large mass is held at the Center for Meteorite Studies [1.5938 kg in 2017].

Mineral List


8 valid minerals.

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

Nininger, H.H. (1950) The Nininger Collection of Meteorites. A Catalogue and a History. Winslow, Arizona. 144 pages.

Mason, B. (1963) Olivine Composition in Chondrites: Geochimica et Cosmochimica Acta 27(9): 1011-1023. (Sept 1963).

Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages.

Graham, A.L., Bevan, A.W. R. & Hutchison, B. (1985) Catalogue of Meteorites (4/e). University of Arizona Press: Tucson.

Grady, M.M. (2000). Catalogue of Meteorites (5/e). Cambridge University Press: Cambridge; New York; Oakleigh; Madrid; Cape Town. 689 pages.

Rubin, A.E. (2003) Chromite-plagioclase assemblages as a new shock indicator: Implications for the shock and thermal and histories of ordinary chondrites. Geochimica et Cosmochimica Acta 67 (14): 2695-2709. (July 2003).

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