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Cullison meteorite, Pratt Co., Kansas, USAi
Regional Level Types
Cullison meteoriteMeteorite Fall Location
Pratt Co.County
KansasState
USACountry

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Latitude & Longitude (WGS84):
37° 37' North , 98° 55' West
Latitude & Longitude (decimal):
Meteorite Class:
Meteoritical Society Class:
KΓΆppen climate type:
Nearest Settlements:
PlacePopulationDistance
Cullison102 (2017)1.8km
Pratt6,849 (2017)16.1km
Haviland695 (2017)16.7km
Iuka165 (2017)20.3km
Sawyer126 (2017)24.5km


Ordinary chondrite, brecciated (H4,br)
Find, 1911; 10 kg

A meteoritic stone was found in 1911, but was believed by many to have fallen on 22 December 1902. Inspections reveal distinct chondrules and chondrule fragments within a somewhat blackened and weathered matrix. Mostly equilibrated olivine (Fa18) and nearly equilibrated low Ca-orthopyroxene are characteristic of H4 chondrites. Mineralogically the meteorite consists primarily of dominant olivine accompanied by orthopyroxene along with minor troilite and Fe-Ni metal. Plagioclase is present, but scanty. Accessory chromite, chromspinel, copper, diopside, ilmenite, and spinel have also been reported.

A relatively brief cosmic ray exposure (CRE) age of 1.9 Ma was reported by Graf and Marti (1995). In a later article, Eugster et al. (2007) argued that Cullison appeared to have experienced a rather complex sequence of events with a chondrule CRE age of 2.1 Ma slightly older than the matrix CRE age of 1.64 Ma. These differences may, perhaps, reflect two separate collisional events.

Moderately large masses (m> 1kg) were obtained by the United States National Museum, the Natural History Museum ( London) and The Center for Meteorite Studies at Arizona State University (Tempe) with several smaller masses elsewhere.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


8 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“˜ 'Chrome-Spinel (of Dana)'
Reference: Krot, A., Ivanova, M.A. & Wasson, J.T. (1993) The origin of chromitic chondrules and the volatility of Cr under a range of nebular conditions: Earth and Planetary Science Letters 119 (4): 569-584. (Oct 1993).
β“˜ Chromite
Formula: Fe2+Cr3+2O4
Reference: Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages.
β“˜ Copper
Formula: Cu
Reference: Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages.
β“˜ Diopside
Formula: CaMgSi2O6
Description: More precisely, mildly variable diopsidic pyroxene.
Reference: Krot, A., Ivanova, M.A. & Wasson, J.T. (1993) The origin of chromitic chondrules and the volatility of Cr under a range of nebular conditions: Earth and Planetary Science Letters 119 (4): 569-584. (Oct 1993).
β“˜ 'Fayalite-Forsterite Series'
Description: Olivine composition (Fa18) characteristic of H chondrite chemical group.
Reference: Merrill, G.P. (1913). Proceedings of the United States National Museum 44: p. 325.; Mason, B. (1963) Olivine Composition in Chondrites: Geochimica et Cosmochimica Acta 27(9): 1011-1023. (Sept 1963).; Taylor, G.J. (1968) On the Thermal History of Chondrites: Master's Thesis: Rice University. 73 pages.
β“˜ Ilmenite
Formula: Fe2+TiO3
Reference: Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages.; Krot, A., Ivanova, M.A. & Wasson, J.T. (1993) The origin of chromitic chondrules and the volatility of Cr under a range of nebular conditions: Earth and Planetary Science Letters 119 (4): 569-584. (Oct 1993).
β“˜ Iron
Formula: Fe
Reference: Taylor, G.J. (1968) On the Thermal History of Chondrites: Master's Thesis: Rice University. 73 pages.
β“˜ Iron var. Kamacite
Formula: (Fe,Ni)
Reference: Taylor, G.J. (1968) On the Thermal History of Chondrites: Master's Thesis: Rice University. 73 pages.; Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages.
β“˜ 'Orthopyroxene Subgroup'
Reference: Merrill, G.P. (1913). Proceedings of the United States National Museum 44: p. 325.
β“˜ 'Plagioclase'
Formula: (Na,Ca)[(Si,Al)AlSi2]O8
Reference: Merrill, G.P. (1913). Proceedings of the United States National Museum 44: p. 325.; Krot, A., Ivanova, M.A. & Wasson, J.T. (1993) The origin of chromitic chondrules and the volatility of Cr under a range of nebular conditions: Earth and Planetary Science Letters 119 (4): 569-584. (Oct 1993).
β“˜ 'Plessite'
Reference: Taylor, G.J. (1968) On the Thermal History of Chondrites: Master's Thesis: Rice University. 73 pages.
β“˜ Spinel
Formula: MgAl2O4
Reference: Krot, A., Ivanova, M.A. & Wasson, J.T. (1993) The origin of chromitic chondrules and the volatility of Cr under a range of nebular conditions: Earth and Planetary Science Letters 119 (4): 569-584. (Oct 1993).
β“˜ Taenite
Formula: (Fe,Ni)
Reference: Taylor, G.J. (1968) On the Thermal History of Chondrites: Master's Thesis: Rice University. 73 pages.
β“˜ Troilite
Formula: FeS
Reference: Taylor, G.J. (1968) On the Thermal History of Chondrites: Master's Thesis: Rice University. 73 pages.; Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages.

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)
Group 2 - Sulphides and Sulfosalts
β“˜Troilite2.CC.10FeS
Group 4 - Oxides and Hydroxides
β“˜Chromite4.BB.05Fe2+Cr3+2O4
β“˜Ilmenite4.CB.05Fe2+TiO3
β“˜Spinel4.BB.05MgAl2O4
Group 9 - Silicates
β“˜Diopside9.DA.15CaMgSi2O6
Unclassified Minerals, Rocks, etc.
β“˜'Chrome-Spinel (of Dana)'-
β“˜'Fayalite-Forsterite Series'-
β“˜'Orthopyroxene Subgroup'-
β“˜'Plagioclase'-(Na,Ca)[(Si,Al)AlSi2]O8
β“˜'Plessite'-

List of minerals for each chemical element

OOxygen
Oβ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
Oβ“˜ ChromiteFe2+Cr23+O4
Oβ“˜ IlmeniteFe2+TiO3
Oβ“˜ DiopsideCaMgSi2O6
Oβ“˜ SpinelMgAl2O4
NaSodium
Naβ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
MgMagnesium
Mgβ“˜ DiopsideCaMgSi2O6
Mgβ“˜ SpinelMgAl2O4
AlAluminium
Alβ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
Alβ“˜ SpinelMgAl2O4
SiSilicon
Siβ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
Siβ“˜ DiopsideCaMgSi2O6
SSulfur
Sβ“˜ TroiliteFeS
CaCalcium
Caβ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
Caβ“˜ DiopsideCaMgSi2O6
TiTitanium
Tiβ“˜ IlmeniteFe2+TiO3
CrChromium
Crβ“˜ ChromiteFe2+Cr23+O4
FeIron
Feβ“˜ Iron var. Kamacite(Fe,Ni)
Feβ“˜ Taenite(Fe,Ni)
Feβ“˜ TroiliteFeS
Feβ“˜ IronFe
Feβ“˜ ChromiteFe2+Cr23+O4
Feβ“˜ IlmeniteFe2+TiO3
NiNickel
Niβ“˜ Iron var. Kamacite(Fe,Ni)
Niβ“˜ Taenite(Fe,Ni)
CuCopper
Cuβ“˜ CopperCu

References

Sort by

Year (asc) Year (desc) Author (A-Z) Author (Z-A)
Merrill, G.P. (1913). Proceedings of the United States National Museum 44: p. 325.
Nininger, H.H. & Nininger, A.D. (1950) The Nininger Collection of Meteorites. A Catalogue and a History. Winslow, Arizona. 144 pp.
Mason, B. (1963) Olivine Composition in Chondrites: Geochimica et Cosmochimica Acta 27(9): 1011-1023. (Sept 1963).
Taylor, G.J. (1968) On the Thermal History of Chondrites: Master's Thesis: Rice University. 73 pages.
Ramdohr, P. (1973). The Opaque Minerals in Stony Meteorites. Elsevier Publishing Company: Amsterdam; London: New York. 245 pages.
Krot, A.,Ivanova, M.A. & Wasson, J.T. (1993) The origin of chromitic chondrules and the volatility of Cr under a range of nebular conditions: Earth and Planetary Science Letters 119 (4): 569-584. (Oct 1993).
Graf, Th. & Marti, K. (1995) Collisional history of H chondrites. J. Geophys. Res. (Planets) 100, 21247–21263.
Herzog, G.F. et al. (1997) Complex exposure histories for meteorites with 'short' exposure ages: Meteoritics & Planetary Science 32(3): 413-422. (May 1997).
Grady, M.M. (2000). Catalogue of Meteorites (5/e). Cambridge University Press: Cambridge; New York; Oakleigh; Madrid; Cape Town. 689 pages.
Eugster, O., Lorenzetti, S., KrΓ€henbΓΌhl, U., & Marti, K. (2007) Comparison of cosmic-ray exposure ages and trapped noble gases in chondrule and matrix samples of ordinary, enstatite, and carbonaceous chondrites: Meteoritics & Planetary Science 42 (7/8): 1351-1371. (Jul/Aug 2007).

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