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Beaver Creek meteorite, West Kootenay District, Golden Mining Division, British Columbia, Canada

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Latitude & Longitude (WGS84): 51° 10' 0'' North , 117° 19' 59'' West
Latitude & Longitude (decimal): 51.16667,-117.33333
Non-native locality type:Meteorite
Meteorite Class:H5 chondrite meteorite
Meteoritical Society Class: H5
Metbull:View entry in Meteoritical Bulletin Database
Köppen climate type:ET : Tundra


Type: Ordinary chondrite (H4; S3)

Fall: 26 May 1893

Weight: 14 kg

During the afternoon a meteoritic stone fell and broke into two pieces. The largest piece (~14 kg) dug a hole ~90 cm deep. Mean composition of the olivine (Fa18.6) is characteristic of the H-chondrite geochemical group. Mineralogically, the meteorite consists primarily of olivine and pyroxene accompanied by troilite and Fe-Ni metal. Accessory chromite, isocubanite, chlorapatite and merrillite are also present. The phosphates have been critical for chronological studies. An absolute age (I-Xe) for the putative parent body of 4.569 Ga and a cosmic ray exposure age of 45.9 Ma for the preterrestrial meteoroid have been reported.


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10 valid minerals.

Meteorite/Rock Types Recorded

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References

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Harrington, B.J. (1893) The Beaver Creek Meteorite. Nature, vol. 48, n° 1244, 426.
Howell, E.E. (1894) Beaver Creek Meteorite. American Journal of Science and Arts (3rd Series) Vol. 47: pp 430-435.
Oliver Cummings Farrington (1915) Catalogue of the meteorites of North America: Memoirs of the National Academy of Sciences, Vol. 13: Washington. 545 pages.
Mason, B. (1963) Olivine in ordinary chondrites. Geochimica et Cosmochimica Acta 27(9): 1011-1023. (Sept 1963).
Merrill, G.P. (1916) Handbook and Descriptive Catalogue of the Meteorite Collections in the U.S. National Museum. Bull. U. S. Natl. Museum, No.94, Washington. 207 pp., 41 pls.
Prior, G.T. (1923) Catalogue of Meteorites: with special reference to those represented in the collection of the British Museum of Natural History. Richard Clay & Sons, Limited: Bungay, Suffolk.
Keil, K. and Fredriksson, K. (1964) The Fe, Mg and Ca Distribution in Coexisting Olivines and Rhombic Pyroxenes of Chondrites. Journal of Geophysical Research Atmospheres 69 (16): 3487-3515. (August 1964).
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. and Hutchison, B. (1985) Catalogue of Meteorites (4/e). University of Arizona Press: Tucson.
Crozaz G., Pellas, P., Bourot-Denise, M., de Chazal, S.M., Fieni, C., Lundberg, L.L., and Zinner, E. (1989) Plutonium, uranium and rare earths in the phosphates of ordinary chondrites—the quest for a chronometer: Earth and Planetary Science Letters 93: 157-169.
Rubin, A.E. (1990) Olivine & Kamacite in Ordinary Chondrites: Intergroup and Intragroup relationships. Geochimica et Cosmochimica Acta 54: 1217-1230. (May 1990).
Brearley, A.J. and Jones, R.H. (1998) Chondritic Meteorites. In: Planetary Materials, Chapter 3; Papike, J.J.-Ed.: Mineralogical Society of America: Washington, DC, USA. 398 pages.
Grady, M.M. (2000) Catalogue of Meteorites (5/e). Cambridge University Press: Cambridge; New York; Oakleigh; Madrid; Cape Town. 689 pages.
Wlotzka, F. (2005) Cr spinel and chromite as petrogenetic indicators in ordinary chondrites: Equilibrium temperatures of petrologic type 3.7 to 6. Meteoritics & Planetary Science 40 (11): 1673-1702. (Nov 2005).
Telus, M., Huss, H.R., Nagashima, K., and Ogliore, R.C. (2014) Revisiting 26Al-26Mg systematics of plagioclase in H4 chondrites: Meteoritics & Planetary Science 49 (6): 929-945. (June 2014).

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