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Kelly meteorite, Logan County, Colorado, USAi
Regional Level Types
Kelly meteoriteMeteorite Fall Location
Logan CountyCounty
ColoradoState
USACountry

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Latitude & Longitude (WGS84):
40° 28' 0'' North , 103° 1' 59'' West
Latitude & Longitude (decimal):
Nearest Settlements:
PlacePopulationDistance
Atwood133 (2011)21.9km
Sterling14,104 (2017)23.0km
Merino283 (2017)26.9km
Fleming403 (2017)28.8km
Iliff259 (2017)32.6km
Mindat Locality ID:
271080
Long-form identifier:
mindat:1:2:271080:1
GUID (UUID V4):
0


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 Elements

Mineral 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 Diagram

Detailed 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.
ⓘ 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.
ⓘ Taenite
Formula: (Fe,Ni)
ⓘ Troilite
Formula: FeS

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
ⓘNative Iron1.AE.05Fe
ⓘvar. Kamacite1.AE.05(Fe,Ni)
ⓘTaenite1.AE.10(Fe,Ni)
Group 2 - Sulphides and Sulfosalts
ⓘIsocubanite2.CB.55bCuFe2S3
ⓘTroilite2.CC.10FeS
Group 4 - Oxides and Hydroxides
ⓘChromite4.BB.05Fe2+Cr3+2O4
ⓘIlmenite4.CB.05Fe2+TiO3
Unclassified
ⓘ'Limonite'-
ⓘ'Fayalite-Forsterite Series'-
ⓘ'Plagioclase'-(Na,Ca)[(Si,Al)AlSi2]O8
ⓘ'Orthopyroxene Subgroup'-

List of minerals for each chemical element

OOxygen
Oⓘ ChromiteFe2+Cr23+O4
Oⓘ IlmeniteFe2+TiO3
Oⓘ Fayalite-Forsterite Series
Oⓘ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
NaSodium
Naⓘ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
MgMagnesium
Mgⓘ Fayalite-Forsterite Series
AlAluminium
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ⓘ IlmeniteFe2+TiO3
Feⓘ Native IronFe
Feⓘ IsocubaniteCuFe2S3
Feⓘ Native Iron var. Kamacite(Fe,Ni)
Feⓘ Taenite(Fe,Ni)
Feⓘ TroiliteFeS
Feⓘ Fayalite-Forsterite Series
NiNickel
Niⓘ Native Iron var. Kamacite(Fe,Ni)
Niⓘ Taenite(Fe,Ni)
CuCopper
Cuⓘ IsocubaniteCuFe2S3

Other Regions, Features and Areas containing this locality


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