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Kelly meteorite, Logan County, Colorado, USAi
| Regional Level Types | |
|---|---|
| Kelly meteorite | Meteorite Fall Location |
| Logan County | County |
| Colorado | State |
| USA | Country |
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Latitude & Longitude (WGS84):
40° 28' 0'' North , 103° 1' 59'' West
Latitude & Longitude (decimal):
Meteorite Class:
Meteoritical Society Class:
Köppen climate type:
INTRODUCTION
Ordinary chondrite, brecciated & xenolithic (LL4,br; S3; W2)
Find,1937; 44.3 kg, single stone
A single mass was found with both chondritic and recrystallized textures set within an almost completely recrystallized matrix. Within the matrix host olivine (Fa27-32, av. 29) and orthopyroxene dominate along with minor albitic plagioclase. Chondrules include usually well-defined barred olivine (BO) types as well as more poorly defined relic porphyritic olivine (PO) types. Small blebs of Fe-Ni metal and troilite are scattered throughout the meteorite. Several additional minor and accessory opaques were observed by Ramdohr (1973). Different clasts have experienced different levels of shock (e.g., undulose extinction in many, but not all olivines). Low-level and moderate weathering is pervasive.
Kelly was one of the first meteorites to receive critical attention after the first moon rocks were returned by the Apollo astronauts. Its complex and pervasive brecciation structure were described as that of a 'metabreccia' in an oft-cited article by Bunch & Stöffler (1974). The parallels between the battered regolith features of lunar rocks and meteorites are not as startling today as they were four decades ago, but they remain complex and only partially explained.
The LL chondrites (very low in total iron) are the smallest group of ordinary chondrites (~10% of the classified witnessed falls) with the LL4 subgroup falls accounting for only 10% of all LL falls. Kelly's cosmic ray exposure (CRE) age of 13.6 Ma, similar to the ~15 Ma CRE ages of many other LL chondrites, may indicate a recent shared disruptive impact event for many LL chondrites.
Kelly itself is the 2nd most massive of the 300 meteorites and meteorite fragments classified exactly as 'LL4' chondrites at the Meteoritical Bulletin Database (in May 2016). Moderate-sized masses in the 1-5 kg range have been held by the Denver Museum of Nature and Science, the United States National Museum (Washington, DC), Field Museum of Natural History in (Chicago), and Senckenberg-Museum (Frankfurt, Germany).
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsMineral List
6 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:
| ⓘ Chromite Formula: Fe2+Cr3+2O4 |
| ⓘ 'Fayalite-Forsterite Series' Description: Ave. composition [Fa29] from Mason & Wiik,1964. Range [Fa27-32] from Grady et al.,2015. References: |
| ⓘ Ilmenite Formula: Fe2+TiO3 |
| ⓘ Isocubanite Formula: CuFe2S3 |
| ⓘ 'Limonite' Description: Iron oxides and rust-colored stains are present. |
| ⓘ Native Iron Formula: Fe |
| ⓘ Native Iron var. Kamacite Formula: (Fe,Ni) |
| ⓘ 'Orthopyroxene Subgroup' |
| ⓘ 'Plagioclase' Formula: (Na,Ca)[(Si,Al)AlSi2]O8 Description: Plagioclase Composition —An10.3 Ab88.4 Or1.3 from Van Schmus & Ribbe,1968. References: |
| ⓘ Taenite Formula: (Fe,Ni) |
| ⓘ Troilite Formula: FeS |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 1 - Elements | |||
|---|---|---|---|
| ⓘ | Native Iron | 1.AE.05 | Fe |
| ⓘ | var. Kamacite | 1.AE.05 | (Fe,Ni) |
| ⓘ | Taenite | 1.AE.10 | (Fe,Ni) |
| 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 |
| ⓘ | Ilmenite | 4.CB.05 | Fe2+TiO3 |
| Unclassified | |||
| ⓘ | 'Limonite' | - | |
| ⓘ | 'Fayalite-Forsterite Series' | - | |
| ⓘ | 'Plagioclase' | - | (Na,Ca)[(Si,Al)AlSi2]O8 |
| ⓘ | 'Orthopyroxene Subgroup' | - | |
List of minerals for each chemical element
| O | Oxygen | |
|---|---|---|
| O | ⓘ Chromite | Fe2+Cr23+O4 |
| O | ⓘ Ilmenite | Fe2+TiO3 |
| O | ⓘ Fayalite-Forsterite Series | |
| O | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Na | Sodium | |
| Na | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Mg | Magnesium | |
| Mg | ⓘ Fayalite-Forsterite Series | |
| Al | Aluminium | |
| Al | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Si | Silicon | |
| Si | ⓘ Fayalite-Forsterite Series | |
| Si | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| S | Sulfur | |
| S | ⓘ Isocubanite | CuFe2S3 |
| S | ⓘ Troilite | FeS |
| Ca | Calcium | |
| Ca | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Ti | Titanium | |
| Ti | ⓘ Ilmenite | Fe2+TiO3 |
| Cr | Chromium | |
| Cr | ⓘ Chromite | Fe2+Cr23+O4 |
| Fe | Iron | |
| Fe | ⓘ Chromite | Fe2+Cr23+O4 |
| Fe | ⓘ Ilmenite | Fe2+TiO3 |
| Fe | ⓘ Native Iron | Fe |
| Fe | ⓘ Isocubanite | CuFe2S3 |
| Fe | ⓘ Native Iron var. Kamacite | (Fe,Ni) |
| Fe | ⓘ Taenite | (Fe,Ni) |
| Fe | ⓘ Troilite | FeS |
| Fe | ⓘ Fayalite-Forsterite Series | |
| Ni | Nickel | |
| Ni | ⓘ Native Iron var. Kamacite | (Fe,Ni) |
| Ni | ⓘ Taenite | (Fe,Ni) |
| Cu | Copper | |
| Cu | ⓘ Isocubanite | CuFe2S3 |
Other Regions, Features and Areas containing this locality
North AmericaContinent
North America PlateTectonic Plate
- Denver BasinBasin
- Great Plains DomainDomain
- Yavapai TerraneVolcanic Arc
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