Grady (1937) meteorite, Curry County, New Mexico, USAi
| Regional Level Types | |
|---|---|
| Grady (1937) meteorite | Meteorite Fall Location |
| Curry County | County |
| New Mexico | State |
| USA | Country |
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Latitude & Longitude (WGS84):
34° 47' 59'' North , 103° 19' 0'' West
Latitude & Longitude (decimal):
Meteorite Class:
Meteoritical Society Class:
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Grady | 106 (2017) | 2.4km |
| San Jon | 203 (2017) | 34.2km |
| Cannon Air Force Base | 2,245 (2013) | 44.8km |
| Clovis | 39,480 (2017) | 45.1km |
| Melrose | 644 (2017) | 50.2km |
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 ElementsMineral 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 DiagramDetailed Mineral List:
| ⓘ 'Chrome-Spinel (of Dana)' References: |
| ⓘ Chromite Formula: Fe2+Cr3+2O4 References: |
| ⓘ '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: Mason, Brian (1963) Olivine composition in chondrites. Geochimica et Cosmochimica Acta, 27 (10) 1011-1023 doi:10.1016/0016-7037(63)90062-0 |
| ⓘ Graphite Formula: C References: |
| ⓘ Graphite var. Cliftonite Formula: C |
| ⓘ Ilmenite Formula: Fe2+TiO3 References: |
| ⓘ Iron Formula: Fe |
| ⓘ Iron var. Kamacite Formula: (Fe,Ni) Description: Neumann bands, Lambert et al.,1981. References: |
| ⓘ Isocubanite Formula: CuFe2S3 |
| ⓘ 'Limonite' Description: Limonite in fractures and, sometimes, in strings. |
| ⓘ Maghemite Formula: (Fe3+0.67◻0.33)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 References: |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 1 - Elements | |||
|---|---|---|---|
| ⓘ | Iron | 1.AE.05 | Fe |
| ⓘ | var. Kamacite | 1.AE.05 | (Fe,Ni) |
| ⓘ | Taenite | 1.AE.10 | (Fe,Ni) |
| ⓘ | Cohenite | 1.BA.05 | Fe3C |
| ⓘ | Graphite | 1.CB.05a | C |
| ⓘ | var. Cliftonite | 1.CB.05a | C |
| ⓘ | Diamond | 1.CB.10a | C |
| Group 2 - Sulphides and Sulfosalts | |||
| ⓘ | Isocubanite | 2.CB.55b | CuFe2S3 |
| ⓘ | Troilite | 2.CC.10 | FeS |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Chromite | 4.BB.05 | Fe2+Cr3+2O4 |
| ⓘ | Magnetite | 4.BB.05 | Fe2+Fe3+2O4 |
| ⓘ | Spinel | 4.BB.05 | MgAl2O4 |
| ⓘ | Maghemite | 4.BB.15 | (Fe3+0.67◻0.33)Fe3+2O4 |
| ⓘ | Ilmenite | 4.CB.05 | Fe2+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
Other Regions, Features and Areas containing this locality
North AmericaContinent
North America PlateTectonic Plate
- Mazatzal DomainDomain
- Mazatzal TerraneVolcanic Arc
- Tucumcari BasinBasin
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References
Mason, Brian (1963) Olivine composition in chondrites. Geochimica et Cosmochimica Acta, 27 (10) 1011-1023 doi:10.1016/0016-7037(63)90062-0