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Grady (1937) meteorite, Curry County, New Mexico, USAi
Regional Level Types
Grady (1937) meteoriteMeteorite Fall Location
Curry CountyCounty
New MexicoState
USACountry

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Latitude & Longitude (WGS84):
34° 47' 59'' North , 103° 19' 0'' West
Latitude & Longitude (decimal):
Nearest Settlements:
PlacePopulationDistance
Grady106 (2017)2.4km
San Jon203 (2017)34.2km
Cannon Air Force Base2,245 (2013)44.8km
Clovis39,480 (2017)45.1km
Melrose644 (2017)50.2km
Mindat Locality ID:
291348
Long-form identifier:
mindat:1:2:291348:6
GUID (UUID V4):
0


Unequilibrated ordinary chondrite, xenolithic (H3.7,br)
Found, 1937; 9.3 kg

A weathered and shocked meteoritic stone was recovered. Inspections reveal distinct chondrules and chondrule fragments within a largely unequilibrated, graphitized, and xenolithic matrix Compositionally, bulk iron contents (Fe 26.23 wt%), nearly equilibrated olivine (Fa15) and variable low Ca-clinopyroxene are characteristic of H3.7 chondrites. Mineralogically the meteorite consists primarily of olivine and pyroxene accompanied by minor troilite and Fe-Ni metal. Accessory chromite, ilmenite, and other minor phases are also reported. Graphite, often aggregated, is found as cliftonite, in metal, and associated with troilite. Minute (nanoscale) pre-solar diamonds, graphite, and SiC have been identified among the disparate phases present in the matrix. Shock indicators include undulating extinction in the (sometimes) fractured olivine grains, Neumann bands in kamacite, veins, and various xenoliths. Extensive weathering is also evident. In addition to pervasive limonite strings and stains, a significant portion of the original kamacite and ilmenite have been weathered into magnetite. A cosmic ray exposure (CRE) age of 6.5 Ma is suggestive of, perhaps, shared collisional histories with other H chondrites with similar CREs.

The H (relatively high in total iron) chondrites are, marginally, the largest group of recovered ordinary chondrites, representing roughly 40% of recognized and properly classified meteorites. However, the H3 (or, unequilibrated) chondrites account for less than 10% of the recovered H-group meteorites. Moderately large specimens are at the Center for Meteorite Studies at Arizona State University [1892.53 g in 2016] and the United States National Museum in Washington [667.4 g in early 2017].

What's in a name? Grady (1937) is but one of 3 ordinary chondrites found relatively near each other in Curry County, largely due to the efforts of Harvey H. Nininger and Glenn Huss. The others are Grady (1933), an L3-6 chondrite, and Grady (c), an H4 chondrite found in 1970. Other meteorites — Clovis (no. 1), Clovis (no. 1), Melrose (a), and Melrose (b) — have also been recovered from slightly more distant locations in the county.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


12 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:

'Chrome-Spinel (of Dana)'
Chromite
Formula: Fe2+Cr3+2O4
'Clinopyroxene Subgroup'
Cohenite
Formula: Fe3C
Diamond
Formula: C
'Fayalite-Forsterite Series'
Description: Olivine composition [Fa15, Mason(1962); Fa15.3, Rubin,(1990] is near the low end for H-chondrite Fayalite content.
References:
Graphite
Formula: C
Graphite var. Cliftonite
Formula: C
Ilmenite
Formula: Fe2+TiO3
Iron
Formula: Fe
Iron var. Kamacite
Formula: (Fe,Ni)
Description: Neumann bands, Lambert et al.,1981.
Isocubanite
Formula: CuFe2S3
'Limonite'
Description: Limonite in fractures and, sometimes, in strings.
Maghemite
Formula: (Fe3+0.670.33)Fe3+2O4
Description: Only in very small amounts (magnetite is more often the predominate weatherate here). See Figure F1 in Ramdohr (1973).
Magnetite
Formula: Fe2+Fe3+2O4
Description: Magnetite apparently both pre-terrestrial and a terrestrial weatherate according to Ramdohr, 1973.
'Plagioclase'
Formula: (Na,Ca)[(Si,Al)AlSi2]O8
'Plessite'
Spinel
Formula: MgAl2O4
Taenite
Formula: (Fe,Ni)
Troilite
Formula: FeS

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
Iron1.AE.05Fe
var. Kamacite1.AE.05(Fe,Ni)
Taenite1.AE.10(Fe,Ni)
Cohenite1.BA.05Fe3C
Graphite1.CB.05aC
var. Cliftonite1.CB.05aC
Diamond1.CB.10aC
Group 2 - Sulphides and Sulfosalts
Isocubanite2.CB.55bCuFe2S3
Troilite2.CC.10FeS
Group 4 - Oxides and Hydroxides
Chromite4.BB.05Fe2+Cr3+2O4
Magnetite4.BB.05Fe2+Fe3+2O4
Spinel4.BB.05MgAl2O4
Maghemite4.BB.15(Fe3+0.670.33)Fe3+2O4
Ilmenite4.CB.05Fe2+TiO3
Unclassified
'Limonite'-
'Clinopyroxene Subgroup'-
'Fayalite-Forsterite Series'-
'Plagioclase'-(Na,Ca)[(Si,Al)AlSi2]O8
'Chrome-Spinel (of Dana)'-
'Plessite'-

List of minerals for each chemical element

CCarbon
C CoheniteFe3C
C DiamondC
C GraphiteC
C Graphite var. CliftoniteC
OOxygen
O ChromiteFe2+Cr23+O4
O IlmeniteFe2+TiO3
O Maghemite(Fe3+0.670.33)Fe23+O4
O MagnetiteFe2+Fe23+O4
O SpinelMgAl2O4
O Fayalite-Forsterite Series
O Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
NaSodium
Na Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
MgMagnesium
Mg SpinelMgAl2O4
Mg Fayalite-Forsterite Series
AlAluminium
Al SpinelMgAl2O4
Al Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
SiSilicon
Si Fayalite-Forsterite Series
Si Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
SSulfur
S IsocubaniteCuFe2S3
S TroiliteFeS
CaCalcium
Ca Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
TiTitanium
Ti IlmeniteFe2+TiO3
CrChromium
Cr ChromiteFe2+Cr23+O4
FeIron
Fe ChromiteFe2+Cr23+O4
Fe CoheniteFe3C
Fe IlmeniteFe2+TiO3
Fe IronFe
Fe IsocubaniteCuFe2S3
Fe Iron var. Kamacite(Fe,Ni)
Fe Maghemite(Fe3+0.670.33)Fe23+O4
Fe MagnetiteFe2+Fe23+O4
Fe Taenite(Fe,Ni)
Fe TroiliteFeS
Fe Fayalite-Forsterite Series
NiNickel
Ni Iron var. Kamacite(Fe,Ni)
Ni Taenite(Fe,Ni)
CuCopper
Cu IsocubaniteCuFe2S3

Other Regions, Features and Areas containing this locality


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