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Farmington meteorite, Washington County, Kansas, USAi
| Regional Level Types | |
|---|---|
| Farmington meteorite | Meteorite Fall Location |
| Washington County | County |
| Kansas | State |
| USA | Country |
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Latitude & Longitude (WGS84):
39° 45' 0'' North , 97° 1' 59'' West
Latitude & Longitude (decimal):
Meteorite Class:
Meteoritical Society Class:
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Greenleaf | 312 (2017) | 5.4km |
| Washington | 1,085 (2017) | 7.7km |
| Linn | 398 (2017) | 8.9km |
| Barnes | 154 (2017) | 14.2km |
| Morrowville | 150 (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 ElementsMineral 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 DiagramDetailed Mineral List:
| ⓘ Albite Formula: Na(AlSi3O8) Description: Instances of nearly pure albite within a few vugs. |
| ⓘ Chromite Formula: Fe2+Cr3+2O4 Description: Chromite found as aggregates and in chromite-plagioclase assemblages. |
| ⓘ 'Clinopyroxene Subgroup' Description: Within vugs (rare). |
| ⓘ Cristobalite Formula: SiO2 |
| ⓘ Diopside Formula: CaMgSi2O6 |
| ⓘ 'Fayalite-Forsterite Series' |
| ⓘ Ilmenite Formula: Fe2+TiO3 |
| ⓘ Isocubanite Formula: CuFe2S3 |
| ⓘ Magnetite Formula: Fe2+Fe3+2O4 Description: Apparently primary (pre-terrestrial) according to Ramdohr (1973). |
| ⓘ 'Maskelynite' Description: In some regions most of the plagioclase has been converted into maskelynite. |
| ⓘ Merrillite Formula: Ca9NaMg(PO4)7 Description: Within vugs. |
| ⓘ Native Copper Formula: Cu |
| ⓘ Native Iron Formula: Fe |
| ⓘ Native Iron var. Kamacite Formula: (Fe,Ni) |
| ⓘ Native Iron var. Martensite Formula: Fe |
| ⓘ 'Orthopyroxene Subgroup' References: |
| ⓘ '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. |
| ⓘ Rutile Formula: TiO2 Description: As lamellae in ilmenite. |
| ⓘ Spinel Formula: MgAl2O4 |
| ⓘ Taenite Formula: (Fe,Ni) |
| ⓘ Troilite Formula: FeS |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 1 - Elements | |||
|---|---|---|---|
| ⓘ | Native Copper | 1.AA.05 | Cu |
| ⓘ | Native Iron | 1.AE.05 | Fe |
| ⓘ | var. Kamacite | 1.AE.05 | (Fe,Ni) |
| ⓘ | var. Martensite | 1.AE.05 | Fe |
| ⓘ | Taenite | 1.AE.10 | (Fe,Ni) |
| Group 2 - Sulphides and Sulfosalts | |||
| ⓘ | Isocubanite | 2.CB.55b | CuFe2S3 |
| ⓘ | Troilite | 2.CC.10 | FeS |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Chromite | 4.BB.05 | Fe2+Cr3+2O4 |
| ⓘ | Magnetite | 4.BB.05 | Fe2+Fe3+2O4 |
| ⓘ | Spinel | 4.BB.05 | MgAl2O4 |
| ⓘ | Ilmenite | 4.CB.05 | Fe2+TiO3 |
| ⓘ | Cristobalite | 4.DA.15 | SiO2 |
| ⓘ | Rutile | 4.DB.05 | TiO2 |
| Group 8 - Phosphates, Arsenates and Vanadates | |||
| ⓘ | Merrillite | 8.AC.45 | Ca9NaMg(PO4)7 |
| Group 9 - Silicates | |||
| ⓘ | Diopside | 9.DA.15 | CaMgSi2O6 |
| ⓘ | Albite | 9.FA.35 | Na(AlSi3O8) |
| Unclassified | |||
| ⓘ | 'Clinopyroxene Subgroup' | - | |
| ⓘ | 'Maskelynite' | - | |
| ⓘ | 'Fayalite-Forsterite Series' | - | |
| ⓘ | 'Plagioclase' | - | (Na,Ca)[(Si,Al)AlSi2]O8 |
| ⓘ | 'Orthopyroxene Subgroup' | - | |
List of minerals for each chemical element
Other Regions, Features and Areas containing this locality
North AmericaContinent
North America PlateTectonic Plate
- Mid-continent DomainDomain
- Mid-continent RiftNarrow Rift
USA
- Midcontinent RiftGeologic Province
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References
Buseck, Peter E, Mason, Brian, Wiik, H.B (1966) The Farmington meteorite. Mineralogy and chemistry. Geochimica et Cosmochimica Acta, 30 (1) 1-8 doi:10.1016/0016-7037(66)90087-1
Binns, R. A. (1967) Farmington Meteorite: Cristobalite Xenoliths and Blackening. Science, 156 (3779). 1222-1226 doi:10.1126/science.156.3779.1222
Bunch, T.E., Keil, Klaus, Snetsinger, K.G. (1967) Chromite composition in relation to chemistry and texture of ordinary chondrites. Geochimica et Cosmochimica Acta, 31 (10). 1569-1582 doi:10.1016/0016-7037(67)90105-6
Buseck, Peter R., Keil, Klaus (1967) Meteoritic rutile: a correction. American Mineralogist, 52 (5-6) 924
Smith, B.A., Goldstein, J.I. (1977) The metallic microstructures and thermal histories of severely reheated chondrites. Geochimica et Cosmochimica Acta, 41 (8) 1061-1072 doi:10.1016/0016-7037(77)90100-4