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Eagle Station meteorite, Carroll Co., Kentucky, USAi
Regional Level Types
Eagle Station meteoriteMeteorite Fall Location
Carroll Co.County
KentuckyState
USACountry

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PhotosMapsSearch
Latitude & Longitude (WGS84):
38° 37' North , 84° 58' West
Latitude & Longitude (decimal):
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Sanders236 (2017)4.6km
Sparta266 (2017)8.5km
Worthville184 (2017)8.8km
Bromley776 (2006)10.6km
Owenton1,550 (2017)13.9km


Pallasite, PES
Find 1880, 36.3 kg

Found just over a kilometer from the town of Eagle Station, the Eagle Station meteorite is a Pallasite, but a very unusual one. Apparently, scientists are not the only ones to appreciate Eagle Station's unusual characteristics. Fragments from the same meteorite were apparently buried in the Turner Mounds of the Little Miami Valley in southern Ohio.

Like all Pallasites the Eagle Station Pallasite's primary constituents are olivine (~78 vol%) and Fe-Ni metal(~21vol%). The olivine (Fa20) is, however, richer in iron than most Pallasites, the 'main group' Pallasites. And, its Fe-Ni metal is richer in nickel (15.37% Ni) than the 'main group' Pallasites. Even more important, its oxygen isotope ratios differ so much from the Main Group Pallasites that to most geochemists and meteoriticists it seems almost inconceivable that the Eagle Station Pallasite (and 3 similar Pallasites) would be derived from the same original homeworld. So, in fact, Eagle Station is the prototype for the 'Eagle Station grouplet' [PES = Pallasite, Eagle Station (subtype)]. In addition to the olivine and metal, Eagle Station also has very minor amounts of orthopyroxene, Ca-rich clinopyroxene, sulfates, troilite, and schreibersite. These constituents are not that unusual, but the minor minerals also have additional variations in trace elements which further differentiate the PES Pallasites from the Main Group.

Eagle Station is one of 25 Kentucky meteorites discovered before 2014. The only other Kentucky Pallasite, Mount Vernon, is a Main Group Pallasite. The main mass of the meteorite is held in the Naturhistorisches Museum in Wiens (Vienna)

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


11 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:

Chromite
Formula: Fe2+Cr3+2O4
Reference: Farrington, O.C., 1915, Catalogue of the meteorites of North America to January 1, 1909: National Academy of Sciences, Memoir 13, 513 pages.
'Clinopyroxene Subgroup'
Description: Clinopyroxene Ca-rich (Wo45Fs7) in at least one instance.
Reference: Mittlefehldt, D.W., McCoy, T.J., Goodrich, C.A. & Kracher, A. (1998). Non-chondritic meteorites from asteroidal bodies. IN: Papike, J. J. (ed.): Planetary Materials: Mineralogical Society of America, Washington. 195 pages.
Diopside
Formula: CaMgSi2O6
Reference: Davis, A. M., & Olsen, E. J. (1989, March). The origin of phosphate minerals in the Eagle Station and Springwater pallasites. In Lunar and Planetary Science Conference (Vol. 20, p. 220).
Enstatite
Formula: Mg2Si2O6
Reference: Davis, A. M., & Olsen, E. J. (1989, March). The origin of phosphate minerals in the Eagle Station and Springwater pallasites. In Lunar and Planetary Science Conference (Vol. 20, p. 220).
'Fayalite-Forsterite Series'
Description: Olivine (Fa19Fo80)in Mittlefehldt et al., (1998). Olivine (Fa20) according to Grady (2000). Olivine accounts for 75-80% of the silicate inventory.
Reference: Radiation Measurements Volume 25, Issues 1-4, 1995, Pages 329-330 ; Mittlefehldt, D.W., McCoy, T.J., Goodrich, C.A. & Kracher, A. (1998). Non-chondritic meteorites from asteroidal bodies. IN: Papike, J. J. (ed.): Planetary Materials: Mineralogical Society of America, Washington. 195 pages.; Farrington, O.C., 1915, Catalogue of the meteorites of North America to January 1, 1909: National Academy of Sciences, Memoir 13, 513 pages.
Forsterite
Formula: Mg2SiO4
Reference: Davis, A. M., & Olsen, E. J. (1989, March). The origin of phosphate minerals in the Eagle Station and Springwater pallasites. In Lunar and Planetary Science Conference (Vol. 20, p. 220).
Iron
Formula: Fe
Reference: Buseck, P. R. (1977) Pallasite meteorites—mineralogy, petrology, and geochemistry. Geochimica et Cosmochimica Acta 41: 711-740. ; Mason, B. (1962) The Pallasites: American Museum Novitates, #2163. 19 pages . (Dec 1963)
Iron var. Kamacite
Formula: (Fe,Ni)
Reference: Buseck, P. R. (1977) Pallasite meteorites—mineralogy, petrology, and geochemistry. Geochimica et Cosmochimica Acta 41: 711-740. ; Mason, B. (1962) The Pallasites: American Museum Novitates, #2163. 19 pages . (Dec 1963)
Merrillite
Formula: Ca9NaMg(PO4)7
Reference: www.lpi.usra.edu/meetings/metsoc2003/pdf/5007.pdf.
'Orthopyroxene Subgroup'
Reference: Mittlefehldt, D.W., McCoy, T.J., Goodrich, C.A. & Kracher, A. (1998). Non-chondritic meteorites from asteroidal bodies. IN: Papike, J. J. (ed.): Planetary Materials: Mineralogical Society of America, Washington. 195 pages.
'Plessite'
Reference: Mason, B. (1962) The Pallasites: American Museum Novitates, #2163. 19 pages . (Dec 1963)
Schreibersite
Formula: (Fe,Ni)3P
Description: Quite minor
Reference: Farrington, O.C., 1915, Catalogue of the meteorites of North America to January 1, 1909: National Academy of Sciences, Memoir 13, 513 pages.; Buseck, P.R. (1977) Pallasite meteorites-mineralogy, petrology, and geochemistry. Geochim Cosmochim Acta 41:711-740.
Stanfieldite
Formula: Ca4Mg5(PO4)6
Reference: www.lpi.usra.edu/meetings/metsoc2003/pdf/5007.pdf.; Davis, A. M., & Olsen, E. J. (1989, March). The origin of phosphate minerals in the Eagle Station and Springwater pallasites. In Lunar and Planetary Science Conference (Vol. 20, p. 220).
Taenite
Formula: (Fe,Ni)
Reference: Farrington, O.C., 1915, Catalogue of the meteorites of North America to January 1, 1909: National Academy of Sciences, Memoir 13, 513 pages.; Mason, B. (1962) The Pallasites: American Museum Novitates, #2163. 19 pages . (Dec 1963)
Troilite
Formula: FeS
Reference: Clayton, R. N., Mayeda, T. K., & Epstein, S. (1978). Isotopic fractionation of silicon in Allende inclusions. In Lunar and Planetary Science Conference Proceedings (Vol. 9, pp. 1267-1278).; Davis, A. M., & Olsen, E. J. (1989, March). The origin of phosphate minerals in the Eagle Station and Springwater pallasites. In Lunar and Planetary Science Conference (Vol. 20, p. 220).
Whitlockite
Formula: Ca9Mg(PO4)6(PO3OH)
Reference: Davis, A. M., & Olsen, E. J. (1989, March). The origin of phosphate minerals in the Eagle Station and Springwater pallasites. In Lunar and Planetary Science Conference (Vol. 20, p. 220).

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
Iron1.AE.05Fe
var. Kamacite1.AE.05(Fe,Ni)
Schreibersite1.BD.05(Fe,Ni)3P
Taenite1.AE.10(Fe,Ni)
Group 2 - Sulphides and Sulfosalts
Troilite2.CC.10FeS
Group 4 - Oxides and Hydroxides
Chromite4.BB.05Fe2+Cr3+2O4
Group 8 - Phosphates, Arsenates and Vanadates
Merrillite8.AC.45Ca9NaMg(PO4)7
Stanfieldite8.AC.70Ca4Mg5(PO4)6
Whitlockite8.AC.45Ca9Mg(PO4)6(PO3OH)
Group 9 - Silicates
Diopside9.DA.15CaMgSi2O6
Enstatite9.DA.05Mg2Si2O6
Forsterite9.AC.05Mg2SiO4
Unclassified Minerals, Rocks, etc.
'Clinopyroxene Subgroup'-
'Fayalite-Forsterite Series'-
'Orthopyroxene Subgroup'-
'Plessite'-

List of minerals for each chemical element

HHydrogen
H WhitlockiteCa9Mg(PO4)6(PO3OH)
OOxygen
O ChromiteFe2+Cr23+O4
O MerrilliteCa9NaMg(PO4)7
O StanfielditeCa4Mg5(PO4)6
O WhitlockiteCa9Mg(PO4)6(PO3OH)
O DiopsideCaMgSi2O6
O EnstatiteMg2Si2O6
O ForsteriteMg2SiO4
NaSodium
Na MerrilliteCa9NaMg(PO4)7
MgMagnesium
Mg MerrilliteCa9NaMg(PO4)7
Mg StanfielditeCa4Mg5(PO4)6
Mg WhitlockiteCa9Mg(PO4)6(PO3OH)
Mg DiopsideCaMgSi2O6
Mg EnstatiteMg2Si2O6
Mg ForsteriteMg2SiO4
SiSilicon
Si DiopsideCaMgSi2O6
Si EnstatiteMg2Si2O6
Si ForsteriteMg2SiO4
PPhosphorus
P Schreibersite(Fe,Ni)3P
P MerrilliteCa9NaMg(PO4)7
P StanfielditeCa4Mg5(PO4)6
P WhitlockiteCa9Mg(PO4)6(PO3OH)
SSulfur
S TroiliteFeS
CaCalcium
Ca MerrilliteCa9NaMg(PO4)7
Ca StanfielditeCa4Mg5(PO4)6
Ca WhitlockiteCa9Mg(PO4)6(PO3OH)
Ca DiopsideCaMgSi2O6
CrChromium
Cr ChromiteFe2+Cr23+O4
FeIron
Fe TroiliteFeS
Fe Schreibersite(Fe,Ni)3P
Fe ChromiteFe2+Cr23+O4
Fe Taenite(Fe,Ni)
Fe Iron var. Kamacite(Fe,Ni)
Fe IronFe
NiNickel
Ni Schreibersite(Fe,Ni)3P
Ni Taenite(Fe,Ni)
Ni Iron var. Kamacite(Fe,Ni)

References

Sort by

Year (asc) Year (desc) Author (A-Z) Author (Z-A)
Farrington, O.C., 1915, Catalogue of the meteorites of North America to January 1, 1909: National Academy of Sciences, Memoir 13, 513 pages.
Mason, B. (1962) The Pallasites: American Museum Novitates, #2163. 19 pages . (Dec 1963)
Bunch, T. E. & Keil, K. (1968) Chromite and Ilmenite in non-chondritic meteorites. American Mineralogist 56 (1&2):146-157. (Jan-Feb 1968)
Buseck, P.R. & Holdsworth, E. (1977) Phosphate minerals in pallasite meteorites. Mineralogical Magazine 41 (317): 91-102. (March 1977)
Buseck, P. R. (1977) Pallasite meteorites—mineralogy, petrology, and geochemistry. Geochimica et Cosmochimica Acta 41: 711-740.
Davis, A. M., & Olsen, E. J. (1989, March). The origin of phosphate minerals in the Eagle Station and Springwater pallasites. In Lunar and Planetary Science Conference (Vol. 20, p. 220).
Mittlefehldt, D.W., McCoy, T.J., Goodrich, C.A. & Kracher, A. (1998). Non-chondritic meteorites from asteroidal bodies. IN: Papike, J. J. (ed.): Planetary Materials: Mineralogical Society of America, Washington. 195 pages.
Grady, M. M. (2000) Catalogue of Meteorites (5/e). Cambridge University Press: Cambridge, London, New York, Oakleigh, Madrid. 689 pages.

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