Camel Donga meteorite, Kalgoorlie-Boulder Shire, Western Australia, Australiai
| Regional Level Types | |
|---|---|
| Camel Donga meteorite | Meteorite Fall Location |
| Kalgoorlie-Boulder Shire | Shire |
| Western Australia | State |
| Australia | Country |
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Latitude & Longitude (WGS84):
30° 19' South , 126° 37' East
Latitude & Longitude (decimal):
Meteorite Class:
Meteoritical Society Class:
Köppen climate type:
Eucrite, monomict
1984 Find, ~25 kg
A two-day trip in July 1985 by Brian Mason and W. H. Cleverly to the site of a January 1984 find resulted in 11 additional stones within a kilometer of each other providing a total recovered mass of 2.92 kilograms. The stones were often covered by black fusion crusts, but weathering is quite evident in these and other subsequently recovered stones. The meteorite is composed almost entirely of pyroxene and plagioclase (~3:2 ratio) as angular grains and in matrix. The matrix which also contains quite minor amounts of iron, troilite, ilmenite, and various silica polymorphs. Gabbroic and doleritic clasts are present as well. Pyroxene is mildly Fe-rich; plagioclase is mostly bytownite; iron (Ni-free) accounts for ~2% of the stone. Small amounts of zircon and baddeleyite are also present. These refractory minerals have been especially helpful in leading to additional refinements in establishing a chronology for Camel Donga's journey from its formation on a large, differentiated meteorite (presumably Vesta) until its eventual landfall. Recent iterations of isotopic studies have suggested that almost all of Camel Donga's constituents were formed ~4.56 billion years ago — and that a particular violent impact event ~3.7 billion years ago may represent the ejection of Camel Donga (and its lithological neighbors…) from the original homeworld. After that event, chance, circumstance, more collisions, and gravity lead to its quite recent final collision with the earth [chronological references below].
Notes [Aug 2008)]: Cleverly et al., (1986) provide an excellent review of both the recovery and the overall mineralgy of Camel. Camel Donga is the 5th most massive of the 802 Eucrites listed on the Meteoritical Society's 'Meteoritical Bulletin Database.' All pieces of the original 1984 eucrite find are referred to simply as (pieces of) Camel Donga. A number of separate finds in the same area have been designated Camel Donga 002 thru Camel Donga 053.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsMineral List
11 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:
| ⓘ Anorthite Formula: Ca(Al2Si2O8) |
| ⓘ Anorthite var. Bytownite Formula: (Ca,Na)[Al(Al,Si)Si2O8] |
| ⓘ Augite Formula: (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| ⓘ Augite var. Ferroaugite Formula: (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| ⓘ Baddeleyite Formula: ZrO2 |
| ⓘ Cristobalite Formula: SiO2 |
| ⓘ Ilmenite Formula: Fe2+TiO3 Description: Found as a minor matrix mineral |
| ⓘ Native Iron Formula: Fe Description: Nearly pure [Ni < .1%; Cr < .1%]; May enclose silica grains. |
| ⓘ Pigeonite Formula: (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| ⓘ 'Plagioclase' Formula: (Na,Ca)[(Si,Al)AlSi2]O8 |
| ⓘ 'Pyroxene Group' Formula: ADSi2O6 |
| ⓘ Quartz Formula: SiO2 |
| ⓘ 'Silica' |
| ⓘ Tridymite Formula: SiO2 |
| ⓘ Troilite Formula: FeS Description: Troilite globules sometimes found with coarser-grained Si-rich associates |
| ⓘ Zircon Formula: Zr(SiO4) |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 1 - Elements | |||
|---|---|---|---|
| ⓘ | Native Iron | 1.AE.05 | Fe |
| Group 2 - Sulphides and Sulfosalts | |||
| ⓘ | Troilite | 2.CC.10 | FeS |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Ilmenite | 4.CB.05 | Fe2+TiO3 |
| ⓘ | Quartz | 4.DA.05 | SiO2 |
| ⓘ | Tridymite | 4.DA.10 | SiO2 |
| ⓘ | Cristobalite | 4.DA.15 | SiO2 |
| ⓘ | Baddeleyite | 4.DE.35 | ZrO2 |
| Group 9 - Silicates | |||
| ⓘ | Zircon | 9.AD.30 | Zr(SiO4) |
| ⓘ | Pigeonite | 9.DA.10 | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| ⓘ | Augite | 9.DA.15 | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| ⓘ | var. Ferroaugite | 9.DA.15 | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| ⓘ | Anorthite | 9.FA.35 | Ca(Al2Si2O8) |
| ⓘ | var. Bytownite | 9.FA.35 | (Ca,Na)[Al(Al,Si)Si2O8] |
| Unclassified | |||
| ⓘ | 'Plagioclase' | - | (Na,Ca)[(Si,Al)AlSi2]O8 |
| ⓘ | 'Pyroxene Group' | - | ADSi2O6 |
| ⓘ | 'Silica' | - | |
List of minerals for each chemical element
| O | Oxygen | |
|---|---|---|
| O | ⓘ Anorthite | Ca(Al2Si2O8) |
| O | ⓘ Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| O | ⓘ Baddeleyite | ZrO2 |
| O | ⓘ Anorthite var. Bytownite | (Ca,Na)[Al(Al,Si)Si2O8] |
| O | ⓘ Cristobalite | SiO2 |
| O | ⓘ Ilmenite | Fe2+TiO3 |
| O | ⓘ Pigeonite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| O | ⓘ Quartz | SiO2 |
| O | ⓘ Tridymite | SiO2 |
| O | ⓘ Zircon | Zr(SiO4) |
| O | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| O | ⓘ Pyroxene Group | ADSi2O6 |
| O | ⓘ Augite var. Ferroaugite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| Na | Sodium | |
| Na | ⓘ Anorthite var. Bytownite | (Ca,Na)[Al(Al,Si)Si2O8] |
| Na | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Mg | Magnesium | |
| Mg | ⓘ Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| Mg | ⓘ Pigeonite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| Mg | ⓘ Augite var. Ferroaugite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| Al | Aluminium | |
| Al | ⓘ Anorthite | Ca(Al2Si2O8) |
| Al | ⓘ Anorthite var. Bytownite | (Ca,Na)[Al(Al,Si)Si2O8] |
| Al | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Si | Silicon | |
| Si | ⓘ Anorthite | Ca(Al2Si2O8) |
| Si | ⓘ Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| Si | ⓘ Anorthite var. Bytownite | (Ca,Na)[Al(Al,Si)Si2O8] |
| Si | ⓘ Cristobalite | SiO2 |
| Si | ⓘ Pigeonite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| Si | ⓘ Quartz | SiO2 |
| Si | ⓘ Tridymite | SiO2 |
| Si | ⓘ Zircon | Zr(SiO4) |
| Si | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Si | ⓘ Pyroxene Group | ADSi2O6 |
| Si | ⓘ Augite var. Ferroaugite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| S | Sulfur | |
| S | ⓘ Troilite | FeS |
| Ca | Calcium | |
| Ca | ⓘ Anorthite | Ca(Al2Si2O8) |
| Ca | ⓘ Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| Ca | ⓘ Anorthite var. Bytownite | (Ca,Na)[Al(Al,Si)Si2O8] |
| Ca | ⓘ Pigeonite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| Ca | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Ca | ⓘ Augite var. Ferroaugite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| Ti | Titanium | |
| Ti | ⓘ Ilmenite | Fe2+TiO3 |
| Fe | Iron | |
| Fe | ⓘ Augite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| Fe | ⓘ Ilmenite | Fe2+TiO3 |
| Fe | ⓘ Native Iron | Fe |
| Fe | ⓘ Pigeonite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| Fe | ⓘ Troilite | FeS |
| Fe | ⓘ Augite var. Ferroaugite | (CaxMgyFez)(Mgy1Fez1)Si2O6 |
| Zr | Zirconium | |
| Zr | ⓘ Baddeleyite | ZrO2 |
| Zr | ⓘ Zircon | Zr(SiO4) |
Other Regions, Features and Areas containing this locality
Australia
- Bight BasinBasin
- Central Australian ElementCraton
- Eucla BasinBasin
- Western Australia
- Canning BasinBasin
Australian PlateTectonic Plate
- South Australian Craton
- Madura ProvinceShield
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References
Cleverly, W.H.; Jarosewich, Eugene; Mason, Brian (1986) Camel Donga meteorite, a new eucrite from the Nullarbor Plain, Western Australia. Meteoritics, 21 (3). 263-269 doi:10.1111/j.1945-5100.1986.tb00870.x
Palme, H., Wlotzka, F., Spettel, B., Dreibus, G., Weber, H. (1988) Camel Donga: A Eucrite with High Metal Content. Meteoritics, 23 (1) 49-57 doi:10.1111/j.1945-5100.1988.tb00896.x
Kennedy, Trudi, Jourdan, Fred, Bevan, Alex W.R., Mary Gee, M.A., Frew, Adam (2013) Impact history of the HED parent body(ies) clarified by new 40Ar/39Ar analyses of four HED meteorites and one anomalous basaltic achondrite. Geochimica et Cosmochimica Acta, 115. 162-182 doi:10.1016/j.gca.2013.03.040