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Bison meteorite, Rush County, Kansas, USAi
Regional Level Types
Bison meteoriteMeteorite Fall Location
Rush CountyCounty
KansasState
USACountry

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Latitude & Longitude (WGS84):
38° 18' 24'' North , 99° 42' 36'' West
Latitude & Longitude (decimal):
Kรถppen climate type:
Nearest Settlements:
PlacePopulationDistance
Bazine325 (2017)15.4km
Burdett241 (2017)20.5km
Hanston204 (2017)20.5km
Ness City1,407 (2017)23.6km
Jetmore852 (2017)29.4km
Mindat Locality ID:
271074
Long-form identifier:
mindat:1:2:271074:0
GUID (UUID V4):
0


Ordinary chondrite, impact melt breccia (LL6; S4; W2)
Find, 1938; 11 kg, 2 stones

A 3 kg meteoritic stone was found near Bison in 1958. This discovery prompted the recognition that an even larger stone recovered in 1938 was a fragment of the same fall. Hand specimens reveal a brecciated texture with many rounded clasts (up to 3.5 mm) in a dark chondritic host. Chondrules [POP, PP, RP and BO] within the matrix vary in size (0.1โ€”1.5 mm). Olivine (Fa~30) and orthopyroxene (Fs~25 ) dominate both chondrules and matrix. Clear grains of albitic feldspar (plagioclase) and lesser amounts of accessory chromite and diopside are present. Tiny grains of sporadically distributed Fe-Ni metal and troilite are observed as well. The clasts include dark clasts (up to 3 cm in section) with relic chondrules and lighter, smaller clasts (< 1 cm) which lack chondrules. Shock-blackened matrix, planar fractures and mosaicism in olivine plus undulose extinction in plagioclase are indicative of moderately strong shock (S4 level). The olivine and orthopyroxene in the host matrix seem well-equilibrated in a manner consistent with its formal type LL6 classification. However, components within the clasts are not fully equilibrated with the host matrix suggesting to some that violent heat-producing shock has partially melted some components and that, perhaps, the meteorite should be classified simply as an 'LL impact melt breccia.'

The LL (very low in total iron) ordinary chondrites are the smallest of the three main geochemical groups of ordinary chondrites and account for ~10% of witnessed meteorite falls. The 'well-equilibrated' LL6 type account for approximately half of all LL ordinary chondrites. The largest masses have been retained at the Naturhistorisches Museum in Wiens and the Geological Survey of Canada in Ottawa (1โ€“2 kg range).

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Standard Detailed Gallery Strunz Chemical Elements

Mineral List


4 valid minerals.

Meteorite/Rock Types Recorded

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

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Alphabetical List Tree Diagram

Detailed Mineral List:

โ“˜ Chromite
Formula: Fe2+Cr3+2O4
โ“˜ Diopside
Formula: CaMgSi2O6
โ“˜ 'Fayalite-Forsterite Series'
Description: Olivine composition โ€” Fa31.9 [Meteoritical Bulletin, no. 62]; Fa29.8 [Dominik & Bussy,1994].
โ“˜ 'Feldspar Group'
Description: Albitic feldspar contains up to 23 mol% orthoclase
โ“˜ 'Limonite'
Description: Patches of iron oxide and rust-colored staining of silicates.
โ“˜ 'Meteoritic Iron'
โ“˜ 'Orthopyroxene Subgroup'
Description: Small variations in Fe content (Fs22.7) and Ca content (Wo1-3). 'Hypersthene' in earlier literature.
โ“˜ Pentlandite
Formula: (NixFey)ฮฃ9S8
โ“˜ 'Plagioclase'
Formula: (Na,Ca)[(Si,Al)AlSi2]O8
Description: Plagioclase โ€” Variable plagioclase An5.4-15.6Or0.5-23.2 with mean value An11.9Ab79Or9.
โ“˜ 'Pyroxene Group'
Formula: ADSi2O6
Description: Lo-Ca Pyroxene (Fs24.4Wo1.9) in the Atlas of Meteorites (2015). [Shocked chondrule pyroxenes may not always be orthopyroxene.]
โ“˜ Troilite
Formula: FeS

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 2 - Sulphides and Sulfosalts
โ“˜Pentlandite2.BB.15(NixFey)ฮฃ9S8
โ“˜Troilite2.CC.10FeS
Group 4 - Oxides and Hydroxides
โ“˜Chromite4.BB.05Fe2+Cr3+2O4
Group 9 - Silicates
โ“˜Diopside9.DA.15CaMgSi2O6
Unclassified
โ“˜'Feldspar Group'-
โ“˜'Limonite'-
โ“˜'Fayalite-Forsterite Series'-
โ“˜'Plagioclase'-(Na,Ca)[(Si,Al)AlSi2]O8
โ“˜'Pyroxene Group'-ADSi2O6
โ“˜'Meteoritic Iron'-
โ“˜'Orthopyroxene Subgroup'-

List of minerals for each chemical element

OOxygen
Oโ“˜ ChromiteFe2+Cr23+O4
Oโ“˜ DiopsideCaMgSi2O6
Oโ“˜ Fayalite-Forsterite Series
Oโ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
Oโ“˜ Pyroxene GroupADSi2O6
NaSodium
Naโ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
MgMagnesium
Mgโ“˜ DiopsideCaMgSi2O6
Mgโ“˜ Fayalite-Forsterite Series
AlAluminium
Alโ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
SiSilicon
Siโ“˜ DiopsideCaMgSi2O6
Siโ“˜ Fayalite-Forsterite Series
Siโ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
Siโ“˜ Pyroxene GroupADSi2O6
SSulfur
Sโ“˜ Pentlandite(NixFey)ฮฃ9S8
Sโ“˜ TroiliteFeS
CaCalcium
Caโ“˜ DiopsideCaMgSi2O6
Caโ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
CrChromium
Crโ“˜ ChromiteFe2+Cr23+O4
FeIron
Feโ“˜ ChromiteFe2+Cr23+O4
Feโ“˜ Pentlandite(NixFey)ฮฃ9S8
Feโ“˜ TroiliteFeS
Feโ“˜ Fayalite-Forsterite Series
NiNickel
Niโ“˜ Pentlandite(NixFey)ฮฃ9S8

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