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Fayetteville meteorite, Fayetteville, Washington County, Arkansas, USAi
Regional Level Types
Fayetteville meteoriteMeteorite Fall Location
Fayetteville- not defined -
Washington CountyCounty
ArkansasState
USACountry

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Latitude & Longitude (WGS84):
36° 2' 59'' North , 94° 10' 0'' West
Latitude & Longitude (decimal):
Meteorite Class:
Meteoritical Society Class:
KΓΆppen climate type:
Nearest Settlements:
PlacePopulationDistance
Fayetteville82,830 (2017)1.6km
Greenland1,388 (2017)6.2km
Farmington6,701 (2017)7.3km
Johnson3,634 (2017)9.2km
Black Oak290 (2017)10.8km
Nearest Clubs:
Local clubs are the best way to get access to collecting localities
ClubLocationDistance
Northwest Arkansas Gem & Mineral SocietySiloam Springs, Arkansas37km


Ordinary chondrite (H4)
Fell, 26 December 1934; 2.358 kg, 2 stones

At midday a 2.25 kg stone was dug out by two woodcutters immediately after its fall from a small 25-30 cm wide, 7-8 cm deep hole. Six days later an additional, much smaller stone was recovered ~5 km away from the first site. A southwestwardly moving bolide had been seen from as far way as 300 km. The bolide was followed by a trail of smoke and several detonations were heard, but no other fragments of the meteorite were found. The main mass, a roughly oblong stone, was largely covered with a 0.5 mm thick fusion crust. Sectioning reveals prominent white clasts within a very dark matrix. The total iron (25.5 wt%) and olivine composition (Fa19) are characteristic of the H group of ordinary chondrites. Silicate-rich chondrules are present as well as a complicated matrix and a somewhat complex mix of opaques. The solar gases found in this brecciated and sometimes highly shocked meteorite have been a prime focus of a number of reports. In a recent development, small amounts of perchlorates have also been reported.

A complex cosmic ray exposure (CRE) age due to (1) burial within a moderately large meteoroid 25-40 Ma ago, subsequently followed by (2) a ~ 4 Ma long journey as a much smaller meteoroid before earth impact has been proposed.

Fayetteville is one of the smaller of 51 witnessed falls listed exactly as an H4 with The Meteoritical Bulletin Database (early 2016). Thirty three H4 falls have larger recovered masses including the most massive, Ochansk, Russia fall of 1887 (500 kg) and the historically important Weston, USA fall of 1807 (150 kg). The H geochemical group of ordinary chondrites (ordinary chondrites relatively low in total Iron) account for a little more than 30% of all meteorite falls.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


9 valid minerals.

Meteorite/Rock Types Recorded

Note: data is currently VERY limited. Please bear with us while we work towards adding this information!

Select Rock List Type

Alphabetical List Tree Diagram

Detailed Mineral List:

β“˜ Chromite
Formula: Fe2+Cr3+2O4
Reference: Ramdohr, P. (1973) The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pp.; Jordan, J., Barrett, R. A., Bogard, D. D., & McKay, D. S. (1987) Rare Gas and Petrological Studies of Disaggregated Size Separates of the Fayetteville Meteorite Breccia: Abstracts of the Lunar and Planetary Science Conference 18: 472-473.
β“˜ Copper
Formula: Cu
Reference: Ramdohr, P. (1973) The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pp.
β“˜ 'Fayalite-Forsterite Series'
Description: Olivine composition (Fa19) according to Mason (1963) with similar results elsewhere.
Reference: Mason, B. (1963) Olivine in ordinary chondrites. Geochimica et Cosmochimica Acta 27(9): 1011-1023. (Sept 1963).; Wagner, J. K., Cohen, A. J., Hapke, B. W., & Partlow, W. D. (1979) Vacuum ultraviolet reflectance spectra of group H chondrites:In: Lunar and Planetary Science Conference X, Proceedings, Vol 2: pp. 1797-1818. New York: Pergamon Press, Inc. (March 1979).
β“˜ 'Glass'
Reference: Jordan, J., Barrett, R. A., Bogard, D. D., & McKay, D. S. (1987) Rare Gas and Petrological Studies of Disaggregated Size Separates of the Fayetteville Meteorite Breccia: Abstracts of the Lunar and Planetary Science Conference 18: 472-473.
β“˜ Ilmenite
Formula: Fe2+TiO3
Reference: Ramdohr, P. (1973) The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pp.
β“˜ Iron
Formula: Fe
Reference: Ramdohr, P. (1973) The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pp.; Scott, E.R.D. & Rajan, R.S. (1981) Metallic minerals, thermal histories and parent bodies of some xenolithic, ordinary chondrites. Geochimica et Cosmochimica Acta 45: 53-67.
β“˜ Iron var. Kamacite
Formula: (Fe,Ni)
Reference: Ramdohr, P. (1973) The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pp.; Scott, E.R.D. & Rajan, R.S. (1981) Metallic minerals, thermal histories and parent bodies of some xenolithic, ordinary chondrites. Geochimica et Cosmochimica Acta 45: 53-67.
β“˜ Isocubanite
Formula: CuFe2S3
Reference: Ramdohr, P. (1973) The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pp.
β“˜ Merrillite
Formula: Ca9NaMg(PO4)7
Description: Reading "merrillite" (preferred for extraterrestrial objects) for "whitlockite" (terrestrial).
Reference: Kothari, B. K. & Rajan, R. S. (1980) Fission tracks in Fayetteville and Weston phosphates: Metamorphic or brecciation ages? LPI Contribution 412 (Criswell, P. ed.) Lunar and Planetary Institute: Houston, TX.
β“˜ 'Orthopyroxene Subgroup'
Reference: Wagner, J. K., Cohen, A. J., Hapke, B. W., & Partlow, W. D. (1979) Vacuum ultraviolet reflectance spectra of group H chondrites:In: Lunar and Planetary Science Conference X, Proceedings, Vol 2: pp. 1797-1818. New York: Pergamon Press, Inc. (March 1979).
β“˜ 'Plagioclase'
Formula: (Na,Ca)[(Si,Al)AlSi2]O8
Description: Plagioclase found in a number of chondrules.
Reference: Jordan, J., Barrett, R. A., Bogard, D. D., & McKay, D. S. (1987) Rare Gas and Petrological Studies of Disaggregated Size Separates of the Fayetteville Meteorite Breccia: Abstracts of the Lunar and Planetary Science Conference 18: 472-473.
β“˜ 'Plessite'
Description: Plessite kamacite-taenite intergrowths presumably due to quick cooling (post-impact??).
Reference: Scott, E.R.D. & Rajan, R.S. (1981) Metallic minerals, thermal histories and parent bodies of some xenolithic, ordinary chondrites. Geochimica et Cosmochimica Acta 45: 53-67.
β“˜ 'Pyroxene Group'
Formula: ADSi2O6
Description: Classification as an 'Olivine-bronzite' chondrites tells us that either orthopyroxene or low-Ca clinopyroxene are present.
Reference: Graham, A. L., Bevan, A. W. R. & Hutchison, B. (1985) Catalogue of Meteorites (4/e). University of Arizona Press: Tucson.
β“˜ Taenite
Formula: (Fe,Ni)
Reference: Ramdohr, P. (1973) The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pp.; Scott, E.R.D. & Rajan, R.S. (1981) Metallic minerals, thermal histories and parent bodies of some xenolithic, ordinary chondrites. Geochimica et Cosmochimica Acta 45: 53-67.
β“˜ Tetrataenite
Formula: FeNi
Reference: Scott, E.R.D. & Rajan, R.S. (1981) Metallic minerals, thermal histories and parent bodies of some xenolithic, ordinary chondrites. Geochimica et Cosmochimica Acta 45: 53-67.
β“˜ Troilite
Formula: FeS
Reference: Ramdohr, P. (1973) The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pp.; Scott, E.R.D. & Rajan, R.S. (1981) Metallic minerals, thermal histories and parent bodies of some xenolithic, ordinary chondrites. Geochimica et Cosmochimica Acta 45: 53-67.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
β“˜Copper1.AA.05Cu
β“˜Iron1.AE.05Fe
β“˜var. Kamacite1.AE.05(Fe,Ni)
β“˜Taenite1.AE.10(Fe,Ni)
β“˜Tetrataenite1.AE.10FeNi
Group 2 - Sulphides and Sulfosalts
β“˜Isocubanite2.CB.55bCuFe2S3
β“˜Troilite2.CC.10FeS
Group 4 - Oxides and Hydroxides
β“˜Chromite4.BB.05Fe2+Cr3+2O4
β“˜Ilmenite4.CB.05Fe2+TiO3
Group 8 - Phosphates, Arsenates and Vanadates
β“˜Merrillite8.AC.45Ca9NaMg(PO4)7
Unclassified Minerals, Rocks, etc.
β“˜'Fayalite-Forsterite Series'-
β“˜'Glass'-
β“˜'Orthopyroxene Subgroup'-
β“˜'Plagioclase'-(Na,Ca)[(Si,Al)AlSi2]O8
β“˜'Plessite'-
β“˜'Pyroxene Group'-ADSi2O6

List of minerals for each chemical element

OOxygen
Oβ“˜ Pyroxene GroupADSi2O6
Oβ“˜ ChromiteFe2+Cr23+O4
Oβ“˜ IlmeniteFe2+TiO3
Oβ“˜ MerrilliteCa9NaMg(PO4)7
Oβ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
NaSodium
Naβ“˜ MerrilliteCa9NaMg(PO4)7
Naβ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
MgMagnesium
Mgβ“˜ MerrilliteCa9NaMg(PO4)7
AlAluminium
Alβ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
SiSilicon
Siβ“˜ Pyroxene GroupADSi2O6
Siβ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
PPhosphorus
Pβ“˜ MerrilliteCa9NaMg(PO4)7
SSulfur
Sβ“˜ IsocubaniteCuFe2S3
Sβ“˜ TroiliteFeS
CaCalcium
Caβ“˜ MerrilliteCa9NaMg(PO4)7
Caβ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
TiTitanium
Tiβ“˜ IlmeniteFe2+TiO3
CrChromium
Crβ“˜ ChromiteFe2+Cr23+O4
FeIron
Feβ“˜ ChromiteFe2+Cr23+O4
Feβ“˜ IlmeniteFe2+TiO3
Feβ“˜ IsocubaniteCuFe2S3
Feβ“˜ Iron var. Kamacite(Fe,Ni)
Feβ“˜ Taenite(Fe,Ni)
Feβ“˜ TroiliteFeS
Feβ“˜ TetrataeniteFeNi
Feβ“˜ IronFe
NiNickel
Niβ“˜ Iron var. Kamacite(Fe,Ni)
Niβ“˜ Taenite(Fe,Ni)
Niβ“˜ TetrataeniteFeNi
CuCopper
Cuβ“˜ CopperCu
Cuβ“˜ IsocubaniteCuFe2S3

References

Sort by

Year (asc) Year (desc) Author (A-Z) Author (Z-A)
Richardson, D.P. (1935) The Fayetteville, Arkansas, Meteorite: Popular Astronomy 43: 384-385.
Mason, B. (1963) Olivine in ordinary 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 pp.
Wagner, J.K., Cohen, A.J., Hapke, B.W., & Partlow, W.D. (1979) Vacuum ultraviolet reflectance spectra of group H chondrites:In: Lunar and Planetary Science Conference X, Proceedings, Vol 2: pp. 1797-1818. New York: Pergamon Press, Inc. (March 1979).
Kothari, B.K. & Rajan, R.S. (1980) Fission tracks in Fayetteville and Weston phosphates: Metamorphic or brecciation ages? LPI Contribution 412 (Criswell, P. ed.) Lunar and Planetary Institute: Houston, TX.
Scott, E.R.D. & Rajan, R.S. (1981) Metallic minerals, thermal histories and parent bodies of some xenolithic, ordinary chondrites. Geochimica et Cosmochimica Acta 45: 53-67.
Graham, A.L., Bevan, A.W.R. & Hutchison,B. (1985) Catalogue of Meteorites (4/e). University of Arizona Press: Tucson.
Jordan, J., Barrett, R.A., Bogard, D.D., & McKay, D.S. (1987) Rare Gas and Petrological Studies of Disaggregated Size Separates of the Fayetteville Meteorite Breccia: Abstracts of the Lunar and Planetary Science Conference 18: 472-473.
Nishiizumi, K., Arnold, J.R., & Sharma, P. (1993) Two-Stage Exposure of the Fayetteville Meteorite Based on 129I. meteoritics 28(3): 412-413.
Grady, M.M. (2000). Catalogue of Meteorites (5/e). Cambridge University Press: Cambridge; New York; Oakleigh; Madrid; Cape Town. 689 pp.
Jackson,Β W.A. & 7 others (2015) Widespread occurrence of (per)chlorate in the Solar System: Earth and Planetary Science Letters 430: 470-476. (Nov 2015).

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