Vote for your favorite mineral in #MinCup26!
-
Quartz
vs.
Asagiite
It's a classic vs a newbie as the most common named mineral in the crust Quartz is up against an exceedingly-rare sea foam-green mineral discovered just a few years ago Asagiite.
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Photography
Fayalite-Forsterite Series
from
Arapahoe meteorite, Cheyenne County, Colorado, USA
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Predictive Mineralogy
Locality type:
Meteorite Fall Location
Classification
Species:
'Fayalite-Forsterite Series' (not an IMA approved species)
Comments:
Olivine composition (Fa23)— Mason,1963. Pervasive brecciation noted by Lambert
et al.
,1981
Confirmation
Validity:
Believed Valid
Data
Mineral Data:
Click here to view Fayalite-Forsterite Series data
Locality Data:
Click here to view Arapahoe meteorite, Cheyenne County, Colorado, USA
Data Identifiers
Mindat Occurrence Record ID:
1105382
Long-form Identifier:
1:3:1105382:2
GUID (
UUID V4
):
0
Nearest other occurrences of Fayalite-Forsterite Series
49.2km (30.6 miles)
ⓘ
Rush Creek meteorite, Kiowa County, Colorado, USA
53.2km (33.1 miles)
ⓘ
Ladder Creek meteorite, Greeley County, Kansas, USA
61.8km (38.4 miles)
ⓘ
Horace meteorite, Greeley County, Kansas, USA
76.5km (47.6 miles)
ⓘ
Goodland meteorite, Sherman County, Kansas, USA
References
Mason, Brian (1963) Olivine composition in chondrites.
Geochimica et Cosmochimica Acta
, 27 (10) 1011-1023
doi:10.1016/0016-7037(63)90062-0
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).
Lambert, P., Lewis, C. & Moore, C.B. (1981) Comparative Shock Metamorphism Study in 12 Chondrites (Abstract.): Lunar & Planetary Science XII: 583-585.
Graham, A. L., Bevan, A. W. R., Hutchison, R. (1985)
Catalogue of Meteorites
- With Special Reference to those Represented in the Collection of the British Museum (Natural History) (4th ed.) British Museum (Natural History), London.
Search for references including Fayalite-Forsterite Series Arapahoe meteorite, Cheyenne County, Colorado, USA
and/or
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