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Farmington meteorite, Washington Co., Kansas, USAi
Regional Level Types
Farmington meteoriteMeteorite Fall Location
Washington Co.County
KansasState
USACountry

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PhotosMapsSearch
Latitude & Longitude (WGS84):
39° 45' 0'' North , 97° 1' 59'' West
Latitude & Longitude (decimal):
Meteorite Class:
Meteoritical Society Class:
Nearest Settlements:
PlacePopulationDistance
Greenleaf312 (2017)5.4km
Washington1,085 (2017)7.7km
Linn398 (2017)8.9km
Barnes154 (2017)14.2km
Morrowville150 (2017)15.8km


Ordinary chondrite, black (L5,br)
Fall, 25 June 1890; 89.4 kg, 2 stones

Just after noon a double trail of smoke was seen and detonations were hear over a radius of ~150 km in both Kansas and Nebraska. With a loud burst an 85.3 kg stone soon struck very close to a very frightened farmer working beneath a wagon. The stone created a crater more than a meter deep. A second smaller stone (4 kg), apparently associated with the smaller smoke trail, was recovered later. Underneath a 1 mm thick fusion crust the meteorite contains numerous chondrules, mineral fragments, and prominent veins. The stone is now classified as an ordinary chondrite of the L5 class with 21.22 wt% total iron as well as relatively well-equilibrated olivine (Fa23) and orthopyroxene (Fs21). In addition to the two dominant silicates, minor amounts of albitic plagioclase, troilite, and Fe-Ni metal are present. Accessory chromite and merrillite are also present. However, most intriguing are a number of features which are associated with preterrestrial shock. The meteorite is a 'black' chondrite with much of the matrix darkened by dispersed microscopic grains (metal and, apparently, some magnetite). Small vugs also contain some intriguing shock-mobilized constituents. Chromite has unusual textures as it is found both as found as chromite aggregates and in chromite-plagioclase assemblages. Odd textures within both opaque oxides and silicates have been the focus of much attention. An unusually short cosmic ray exposure age of < 25 ka has also been reported.

Farmington is the fifth most massive of the 80 witnessed falls of L5 meteorites listed by the Meteoritical Bulletin Database (as of early 2016). The L group of ordinary chondrites (ordinary chondrites relatively high in total iron) account for ~40% of all fully classified meteorite falls. About a quarter of the larger stone was broken off and distributed locally before it was was acquired by Henry Ward who distributed it on a national and international scale. By 2000 the largest masses were held at Chicago's Field Museum of Natural History (>20 kg), the National Museum in Budapest (>10 kg), and the American Museum of Natural History in New York (6 kg).

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


14 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:

Albite
Formula: Na(AlSi3O8)
Description: Instances of nearly pure albite within a few vugs.
Reference: Olsen, E. (1981) Vugs in ordinary chondrites: Meteoritics 16 (1): 45-59. (Mar., 1981).
Chromite
Formula: Fe2+Cr3+2O4
Description: Chromite found as aggregates and in chromite-plagioclase assemblages.
Reference: Buseck, P., Mason, B. & Wiik, H.B. (1966) The Farmington meteorite. Geochimica et Cosmochimica Acta, vol. 30; Issue 1; Pages 1-8. (Jan 1966).; Buseck, P. & Keil, K. (1966) Meteoritic Rutile: American Mineralogist 51(9&10): 1506-1515. (Sept-Oct 1966).; Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 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.
'Clinopyroxene Subgroup'
Description: Within vugs (rare).
Reference: Olsen, E. (1981) Vugs in ordinary chondrites: Meteoritics 16 (1): 45-59. (Mar., 1981).
Copper
Formula: Cu
Reference: Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages.
Cristobalite
Formula: SiO2
Reference: Grady, M.M (2000). Catalogue of Meteorites (5/e). Cambridge University Press: Cambridge; New York; Oakleigh; Madrid; Cape Town. 689 pages. ; Binns, R. A. (1967) Farmington meteorite: Cristobalite xenoliths and blackening. Science 156: 1222- 1226.
Diopside
Formula: CaMgSi2O6
Reference: Binns, R. A. (1967) Farmington meteorite: Cristobalite xenoliths and blackening. Science 156: 1222- 1226.
'Fayalite-Forsterite Series'
Reference: Kunz, G.F. & Weinschenk, E. (1890) Farmington, Washington Co., Kansas Aerolite: American Journal of Science and Arts (3rd Series) 43: 65-67.; Keil, K. & 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). ; Buseck, P., Mason, B. & Wiik, H.B. (1966) The Farmington meteorite. Geochimica et Cosmochimica Acta, vol. 30; Issue 1; Pages 1-8. (Jan 1966).; Dodd, R.T. & Jarosewich, E. (1979) Incipient melting in and shock classification of L-Group chondrites: Earth and Planetary Science Letters 44(2):335-340. (Aug 1979).
Ilmenite
Formula: Fe2+TiO3
Reference: Buseck, P., Mason, B. & Wiik, H.B. (1966) The Farmington meteorite. Geochimica et Cosmochimica Acta, vol. 30; Issue 1; Pages 1-8. (Jan 1966).; Buseck, P. & Keil, K. (1966) Meteoritic Rutile: American Mineralogist 51(9&10): 1506-1515. (Sept-Oct 1966).; Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages.
Iron
Formula: Fe
Reference: Buseck, P., Mason, B. & Wiik, H.B. (1966) The Farmington meteorite. Geochimica et Cosmochimica Acta, vol. 30; Issue 1; Pages 1-8. (Jan 1966).; Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages.; Smith, B. A. & Goldstein, J. I. (1977) The metallic microstructures and thermal histories of severely reheated chondrites: Geochimica et Cosmochimica Acta 41: 1061-1072. (Aug. 1977).
Iron var. Kamacite
Formula: (Fe,Ni)
Reference: Buseck, P., Mason, B. & Wiik, H.B. (1966) The Farmington meteorite. Geochimica et Cosmochimica Acta, vol. 30; Issue 1; Pages 1-8. (Jan 1966).; Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages.; Smith, B. A. & Goldstein, J. I. (1977) The metallic microstructures and thermal histories of severely reheated chondrites: Geochimica et Cosmochimica Acta 41: 1061-1072. (Aug. 1977).
Iron var. Martensite
Formula: Fe
Reference: Smith, B. A. & Goldstein, J. I. (1977) The metallic microstructures and thermal histories of severely reheated chondrites: Geochimica et Cosmochimica Acta 41: 1061-1072. (Aug. 1977).
Isocubanite
Formula: CuFe2S3
Reference: Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages.
Magnetite
Formula: Fe2+Fe3+2O4
Description: Apparently primary (pre-terrestrial) according to Ramdohr (1973).
Reference: Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages.
'Maskelynite'
Description: In some regions most of the plagioclase has been converted into maskelynite.
Reference: Dodd, R.T. & Jarosewich, E. (1979) Incipient melting in and shock classification of L-Group chondrites: Earth and Planetary Science Letters 44(2):335-340. (Aug 1979).
Merrillite
Formula: Ca9NaMg(PO4)7
Description: Within vugs.
Reference: Fuchs, L.H. (1969) The Phosphate Mineralogy of Meteorites: IN: Meteoritic Research: Millman, P.M.-Ed.: pp. 683-695. D. Reidel Publishing Company: Dordrecht-Holland.; Olsen, E. (1981) Vugs in ordinary chondrites: Meteoritics 16 (1): 45-59. (Mar., 1981).
'Orthopyroxene Subgroup'
Reference: Kunz, G.F. & Weinschenk, E. (1890) Farmington, Washington Co., Kansas Aerolite: American Journal of Science and Arts (3rd Series) 43: 65-67.; Keil, K. & 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). ; Buseck, P., Mason, B. & Wiik, H.B. (1966) The Farmington meteorite. Geochimica et Cosmochimica Acta, vol. 30; Issue 1; Pages 1-8. (Jan 1966).
'Plagioclase'
Formula: (Na,Ca)[(Si,Al)AlSi2]O8
Description: Apparently oligoclase [anorthite component (An~10) with, presumably, a minor orthoclase (<10 Or) component. Albitic content of Ab~90 are, however, frequently present.
Reference: Buseck, P., Mason, B. & Wiik, H.B. (1966) The Farmington meteorite. Geochimica et Cosmochimica Acta, vol. 30; Issue 1; Pages 1-8. (Jan 1966).; 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.; Olsen, E. (1981) Vugs in ordinary chondrites: Meteoritics 16 (1): 45-59. (Mar., 1981).
Rutile
Formula: TiO2
Description: As lamellae in ilmenite.
Reference: Buseck, P. & Keil, K. (1966) Meteoritic Rutile: American Mineralogist 51(9&10): 1506-1515. (Sept-Oct 1966).; Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages.
Spinel
Formula: MgAl2O4
Reference: Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages.
Taenite
Formula: (Fe,Ni)
Reference: Buseck, P., Mason, B. & Wiik, H.B. (1966) The Farmington meteorite. Geochimica et Cosmochimica Acta, vol. 30; Issue 1; Pages 1-8. (Jan 1966).; Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages.
Troilite
Formula: FeS
Reference: Kunz, G.F. & Weinschenk, E. (1890) Farmington, Washington Co., Kansas Aerolite: American Journal of Science and Arts (3rd Series) 43: 65-67.; Buseck, P., Mason, B. & Wiik, H.B. (1966) The Farmington meteorite. Geochimica et Cosmochimica Acta, vol. 30; Issue 1; Pages 1-8. (Jan 1966).; Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages.; Smith, B. A. & Goldstein, J. I. (1977) The metallic microstructures and thermal histories of severely reheated chondrites: Geochimica et Cosmochimica Acta 41: 1061-1072. (Aug. 1977).

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
Copper1.AA.05Cu
Iron1.AE.05Fe
var. Kamacite1.AE.05(Fe,Ni)
var. Martensite1.AE.05Fe
Taenite1.AE.10(Fe,Ni)
Group 2 - Sulphides and Sulfosalts
Isocubanite2.CB.55bCuFe2S3
Troilite2.CC.10FeS
Group 4 - Oxides and Hydroxides
Chromite4.BB.05Fe2+Cr3+2O4
Cristobalite4.DA.15SiO2
Ilmenite4.CB.05Fe2+TiO3
Magnetite4.BB.05Fe2+Fe3+2O4
Rutile4.DB.05TiO2
Spinel4.BB.05MgAl2O4
Group 8 - Phosphates, Arsenates and Vanadates
Merrillite8.AC.45Ca9NaMg(PO4)7
Group 9 - Silicates
Albite9.FA.35Na(AlSi3O8)
Diopside9.DA.15CaMgSi2O6
Unclassified Minerals, Rocks, etc.
'Clinopyroxene Subgroup'-
'Fayalite-Forsterite Series'-
'Maskelynite'-
'Orthopyroxene Subgroup'-
'Plagioclase'-(Na,Ca)[(Si,Al)AlSi2]O8

List of minerals for each chemical element

OOxygen
O ChromiteFe2+Cr23+O4
O IlmeniteFe2+TiO3
O Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
O RutileTiO2
O MagnetiteFe2+Fe23+O4
O SpinelMgAl2O4
O CristobaliteSiO2
O MerrilliteCa9NaMg(PO4)7
O AlbiteNa(AlSi3O8)
O DiopsideCaMgSi2O6
NaSodium
Na Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
Na MerrilliteCa9NaMg(PO4)7
Na AlbiteNa(AlSi3O8)
MgMagnesium
Mg SpinelMgAl2O4
Mg MerrilliteCa9NaMg(PO4)7
Mg DiopsideCaMgSi2O6
AlAluminium
Al Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
Al SpinelMgAl2O4
Al AlbiteNa(AlSi3O8)
SiSilicon
Si Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
Si CristobaliteSiO2
Si AlbiteNa(AlSi3O8)
Si DiopsideCaMgSi2O6
PPhosphorus
P MerrilliteCa9NaMg(PO4)7
SSulfur
S TroiliteFeS
S IsocubaniteCuFe2S3
CaCalcium
Ca Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
Ca MerrilliteCa9NaMg(PO4)7
Ca DiopsideCaMgSi2O6
TiTitanium
Ti IlmeniteFe2+TiO3
Ti RutileTiO2
CrChromium
Cr ChromiteFe2+Cr23+O4
FeIron
Fe TroiliteFeS
Fe ChromiteFe2+Cr23+O4
Fe Iron var. Kamacite(Fe,Ni)
Fe IlmeniteFe2+TiO3
Fe Taenite(Fe,Ni)
Fe IsocubaniteCuFe2S3
Fe MagnetiteFe2+Fe23+O4
Fe Iron var. MartensiteFe
Fe IronFe
NiNickel
Ni Iron var. Kamacite(Fe,Ni)
Ni Taenite(Fe,Ni)
CuCopper
Cu CopperCu
Cu IsocubaniteCuFe2S3

References

Sort by

Year (asc) Year (desc) Author (A-Z) Author (Z-A)
Kunz, G.F. & Weinschenk, E. (1890) Farmington, Washington Co., Kansas Aerolite: American Journal of Science and Arts (3rd Series) 43: 65-67.
Keil, K. & 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).
Buseck, P. & Keil, K. (1966) Meteoritic Rutile: American Mineralogist 51(9&10): 1506-1515. (Sept-Oct 1966).
Buseck, P., Mason, B. & Wiik, H.B. (1966) The Farmington meteorite. Geochimica et Cosmochimica Acta, vol. 30; Issue 1; Pages 1-8. (Jan 1966).
Binns, R. A. (1967) Farmington meteorite: Cristobalite xenoliths and blackening. Science 156: 1222- 1226.
Fuchs, L.H. (1969) The Phosphate Mineralogy of Meteorites: IN: Meteoritic Research: Millman, P.M.-Ed.: pp. 683-695. D. Reidel Publishing Company: Dordrecht-Holland.
Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages.
Bunch, T.E., Keil, K. & Snetsinger, K.G. (1967) Chromite composition in relation to chemistry and texture of ordinary chondrites. Geochimica et Cosmochimica Acta 31(10): 1569-1582. (Oct 1967).
Smith, B. A. & Goldstein, J. I. (1977) The metallic microstructures and thermal histories of severely reheated chondrites: Geochimica et Cosmochimica Acta 41: 1061-1072. (Aug. 1977).
Dodd, R.T. & Jarosewich, E. (1979) Incipient melting in and shock classification of L-Group chondrites: Earth and Planetary Science Letters 44(2):335-340. (Aug 1979).
Olsen, E. (1981) Vugs in ordinary chondrites: Meteoritics 16 (1): 45-59. (Mar., 1981).
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.

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