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Molteno meteorite, Enoch Mgijima Local Municipality, Chris Hani District Municipality, Eastern Cape, South Africai
| Regional Level Types | |
|---|---|
| Molteno meteorite | Meteorite Fall Location |
| Enoch Mgijima Local Municipality | Municipality |
| Chris Hani District Municipality | Municipality |
| Eastern Cape | Province |
| South Africa | Country |
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Latitude & Longitude (WGS84):
31° 15' South , 26° 28' East
Latitude & Longitude (decimal):
Meteorite Class:
Meteoritical Society Class:
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Molteno | 10,078 (2012) | 19.1km |
| Burgersdorp | 12,548 (2012) | 31.0km |
Howardite (HED achondrite)
Fell, April or May 1953; 150 g
After detonations a small stone with an unusual two-component fusion crust was recovered, one of the only 16 witnessed Howardite falls of the 19th and 20th centuries. Howardites are breccias composed primarily of fragmented Eucritic and Diogenitic materials assembled from both crustal and plutonic regions, respectively, on one or more ancient large asteroids. Thus, unsurprisingly, Molteno contains variable pyroxenes (>90 vol%), plagioclase (~5 vol%, sometimes intergrown with troilite), and several other minor silicates and opaques. In this particular case, Molteno consist primarily of Diogenitic pyroxenites mingled with a significant quantity of accessory Eucritic clasts (plagioclase-pyroxene). An extra boon — especially in such a small stone — is that Molteno contains small quantities of quite variable olivine. This suggests the intriguing possibility that Molteno may contain components from a deeper source within the first homeworld than even the orthopyroxene-rich Diogenites.
Over the past four decades contemporary planetary scientists have combined astronomical and mineralogical findings and have gradually concluded that the brightest asteroid, 4 Vesta is the Original Planet Body (OPB) for most or even almost all of the HED meteorites (Howardites-Eucrites-Diogenites). And combining the mineralogical information referenced here with findings from the recently completed DAWN Spacecraft Mission to Vesta, we might reasonably expect that Vesta would indeed be Molteno's Original Planet Body.
A caveat. Recent studies — including new very high-resolution O-isotope findings — have also presented seemingly irrefutable evidence that several HED meteorites are not fragments from the same OPB as most 'normal' HEDs. (Most notable are a few 'anomalous' Eucrites). For now, at least, we must wait a little longer before we can definitively assign Molteno and/or other HED meteorites to Vesta or some other presently unidentified original homeworld.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsMineral List
5 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] |
| ⓘ Chromite Formula: Fe2+Cr3+2O4 |
| ⓘ 'Clinopyroxene Subgroup' Description: Clinopyroxene - Ca-rich clinopyroxene present, Ca-rich content reaches Wo41Fs26En33 |
| ⓘ 'Fayalite-Forsterite Series' Description: Olivine has unusual compositional range (Fa 11-56) |
| ⓘ Ilmenite Formula: Fe2+TiO3 |
| ⓘ Iron Formula: Fe Description: Kamacite (4%Ni) is at the low end for normal Ni content in meteoritic iron. |
| ⓘ Iron var. Kamacite Formula: (Fe,Ni) Description: Kamacite (4%Ni) is at the low end for normal Ni content in meteoritic iron. |
| ⓘ 'Orthopyroxene Subgroup' Description: Mildly ferroan (Fs 57) |
| ⓘ 'Plagioclase' Formula: (Na,Ca)[(Si,Al)AlSi2]O8 Description: Plagioclase - Often found in myrmekitic intergrowths with Troilite, composition (An 84) is that of Bytownite |
| ⓘ 'Pyroxene Group' Formula: ADSi2O6 Description: Ca-poor Pyroxene range (Wo2Fs22En76—Wo4Fs58En38) |
| ⓘ Troilite Formula: FeS |
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) |
| Group 2 - Sulphides and Sulfosalts | |||
| ⓘ | Troilite | 2.CC.10 | FeS |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Chromite | 4.BB.05 | Fe2+Cr3+2O4 |
| ⓘ | Ilmenite | 4.CB.05 | Fe2+TiO3 |
| Group 9 - Silicates | |||
| ⓘ | Anorthite | 9.FA.35 | Ca(Al2Si2O8) |
| ⓘ | var. Bytownite | 9.FA.35 | (Ca,Na)[Al(Al,Si)Si2O8] |
| Unclassified | |||
| ⓘ | 'Clinopyroxene Subgroup' | - | |
| ⓘ | 'Fayalite-Forsterite Series' | - | |
| ⓘ | 'Plagioclase' | - | (Na,Ca)[(Si,Al)AlSi2]O8 |
| ⓘ | 'Pyroxene Group' | - | ADSi2O6 |
| ⓘ | 'Orthopyroxene Subgroup' | - | |
List of minerals for each chemical element
| O | Oxygen | |
|---|---|---|
| O | ⓘ Anorthite | Ca(Al2Si2O8) |
| O | ⓘ Anorthite var. Bytownite | (Ca,Na)[Al(Al,Si)Si2O8] |
| O | ⓘ Chromite | Fe2+Cr23+O4 |
| O | ⓘ Ilmenite | Fe2+TiO3 |
| O | ⓘ Fayalite-Forsterite Series | |
| O | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| O | ⓘ Pyroxene Group | ADSi2O6 |
| Na | Sodium | |
| Na | ⓘ Anorthite var. Bytownite | (Ca,Na)[Al(Al,Si)Si2O8] |
| Na | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Mg | Magnesium | |
| Mg | ⓘ Fayalite-Forsterite Series | |
| 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 | ⓘ Anorthite var. Bytownite | (Ca,Na)[Al(Al,Si)Si2O8] |
| Si | ⓘ Fayalite-Forsterite Series | |
| Si | ⓘ Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
| Si | ⓘ Pyroxene Group | ADSi2O6 |
| S | Sulfur | |
| S | ⓘ Troilite | FeS |
| Ca | Calcium | |
| Ca | ⓘ Anorthite | Ca(Al2Si2O8) |
| Ca | ⓘ Anorthite var. Bytownite | (Ca,Na)[Al(Al,Si)Si2O8] |
| 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 | ⓘ Iron | Fe |
| Fe | ⓘ Iron var. Kamacite | (Fe,Ni) |
| Fe | ⓘ Troilite | FeS |
| Fe | ⓘ Fayalite-Forsterite Series | |
| Ni | Nickel | |
| Ni | ⓘ Iron var. Kamacite | (Fe,Ni) |
Other Regions, Features and Areas containing this locality
AfricaContinent
African PlateTectonic Plate
- Karoo basinBasin
- Namaqua-Natal BeltOrogenic Belt
South Africa
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References
McSween, Harry Y.; Binzel, Richard P.; De Sanctis, M. Cristina; Ammannito, Eleonora; Prettyman, Thomas H.; Beck, Andrew W.; Reddy, Vishnu; Le Corre, Lucille; Gaffey, Michael J.; McCord, Thomas B.; et al. (2013) Dawn; the Vesta–HED connection; and the geologic context for eucrites, diogenites, and howardites. Meteoritics & Planetary Science, 48 (11). 2090-2104 doi:10.1111/maps.12108