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Mundrabilla meteorite (Premier Downs meteorite), Mundrabilla Roadhouse, Dundas Shire, Western Australia, Australiai
| Regional Level Types | |
|---|---|
| Mundrabilla meteorite (Premier Downs meteorite) | Meteorite Fall Location |
| Mundrabilla Roadhouse | Community |
| Dundas Shire | Shire |
| Western Australia | State |
| Australia | Country |
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Latitude & Longitude (WGS84):
30° 46' 59'' South , 127° 32' 59'' East
Latitude & Longitude (decimal):
Meteorite Class:
Meteoritical Society Class:
Köppen climate type:
Iron meteorite, Octahedrite with silicate & sulfide inclusions (IAB-ung)
Find 1911, 24 tons.
The largest meteorite that has been found in Australia and, currently, listed as the 8th most massive meteorite in the world (#3 on IAB list).
Early literature titles it the Premier Downs meteorite, after the station the first three fragments were found on, however it is since more commonly known as the Mundrabilla meteorite.
As it burnt through the atmosphere the troilite disappeared leaving pockets and holes in the large fragments. The meteorite has been studied by NASA in 2002 examining natural alloy formation of the iron sulphide and iron nickel. This large meteorite contains an impressive number of reduced extraterrestrial compounds, but weathering products are found both near the surface and in interior veins. It is part of the IAB Group, Mundrabilla duo sub-group which only has five members.
It appears to have disintegrated into fragments as it fell to earth, and these have been found over a wide area of the nullabor desert. The areas remote nature and widespread distribution of fragments has meant their discovery has been a gradual affair.
A small 112gr fragment was found by H. Kent in 1911 on Premier Downs Station, then he found another one at 116gr 13 kilometres further west. A third was found in 1918 at 99gr. Around 1962, a 108gr fragment was found on Loomgana Station by a Mr Harrison, and a further three (94.1, 45 and 38.8gr) by W.A. Crowle 16 kilometres from the Mundrabilla Siding on the Trans-Australian railway line.
In April 1966, two very large iron masses at 9980 and 5440kg were discovered by geologists R.B. Wilson and A.M. Cooney during a geological survey. Discoveries continued with one dealer suggesting over 500 knuckle sized fragments have come onto the market recently. The material is commonly for sale, although laws in Australia make large fragments property of the State. For those who want to find their own piece of Mundrabilla, they will come across a roadhouse, a long straight road and railway line, and alot of flat empty space. Under prepared overseas tourists regularly get into trouble in the Australian outback when they travel to these remote locations.
Many meteorites from separate falls have been found on the Nullabor Plain. Often as widely scattered individual stones or in small groups. Many were recovered by the Carlisle family who were rabbit trappers during the 1960's and 1970's, amongst many other individuals. Whether all meteorites labelled Mundrabilla are from this fall, or are from others, is something collectors need to determine.
Find 1911, 24 tons.
The largest meteorite that has been found in Australia and, currently, listed as the 8th most massive meteorite in the world (#3 on IAB list).
Early literature titles it the Premier Downs meteorite, after the station the first three fragments were found on, however it is since more commonly known as the Mundrabilla meteorite.
As it burnt through the atmosphere the troilite disappeared leaving pockets and holes in the large fragments. The meteorite has been studied by NASA in 2002 examining natural alloy formation of the iron sulphide and iron nickel. This large meteorite contains an impressive number of reduced extraterrestrial compounds, but weathering products are found both near the surface and in interior veins. It is part of the IAB Group, Mundrabilla duo sub-group which only has five members.
It appears to have disintegrated into fragments as it fell to earth, and these have been found over a wide area of the nullabor desert. The areas remote nature and widespread distribution of fragments has meant their discovery has been a gradual affair.
A small 112gr fragment was found by H. Kent in 1911 on Premier Downs Station, then he found another one at 116gr 13 kilometres further west. A third was found in 1918 at 99gr. Around 1962, a 108gr fragment was found on Loomgana Station by a Mr Harrison, and a further three (94.1, 45 and 38.8gr) by W.A. Crowle 16 kilometres from the Mundrabilla Siding on the Trans-Australian railway line.
In April 1966, two very large iron masses at 9980 and 5440kg were discovered by geologists R.B. Wilson and A.M. Cooney during a geological survey. Discoveries continued with one dealer suggesting over 500 knuckle sized fragments have come onto the market recently. The material is commonly for sale, although laws in Australia make large fragments property of the State. For those who want to find their own piece of Mundrabilla, they will come across a roadhouse, a long straight road and railway line, and alot of flat empty space. Under prepared overseas tourists regularly get into trouble in the Australian outback when they travel to these remote locations.
Many meteorites from separate falls have been found on the Nullabor Plain. Often as widely scattered individual stones or in small groups. Many were recovered by the Carlisle family who were rabbit trappers during the 1960's and 1970's, amongst many other individuals. Whether all meteorites labelled Mundrabilla are from this fall, or are from others, is something collectors need to determine.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsMineral List
15 valid minerals.
Meteorite/Rock Types Recorded
Select Rock List Type
Alphabetical List Tree DiagramDetailed Mineral List:
| ⓘ Alabandite Formula: MnS |
| ⓘ Chalcopyrite Formula: CuFeS2 |
| ⓘ Chromite Formula: Fe2+Cr3+2O4 |
| ⓘ 'Clinopyroxene Subgroup' |
| ⓘ Cohenite Formula: Fe3C |
| ⓘ Daubréelite Formula: Fe2+Cr3+2S4 References: |
| ⓘ 'Fayalite-Forsterite Series' Description: Very magnesian olivine found in inclusions (Fa2.6) |
| ⓘ Graphite Formula: C References: |
| ⓘ Graphite var. Cliftonite Formula: C |
| ⓘ 'Limonite' |
| ⓘ Native Iron Formula: Fe References: |
| ⓘ Native Iron var. Kamacite Formula: (Fe,Ni) References: |
| ⓘ Native Selenium Formula: Se |
| ⓘ Pentlandite Formula: (NixFey)Σ9S8 Description: As weathering alteration veins in Troilite |
| ⓘ 'Plessite' |
| ⓘ Pyrolusite Formula: Mn4+O2 Description: A weathering-induced decomposition product of alabandite. |
| ⓘ 'Pyroxene Group' Formula: ADSi2O6 |
| ⓘ Rutile Formula: TiO2 |
| ⓘ Schreibersite Formula: (Fe,Ni)3P References: |
| ⓘ Sphalerite Formula: ZnS |
| ⓘ Taenite Formula: (Ni,Fe) References: |
| ⓘ 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 | (Ni,Fe) |
| ⓘ | Cohenite | 1.BA.05 | Fe3C |
| ⓘ | Schreibersite | 1.BD.05 | (Fe,Ni)3P |
| ⓘ | Graphite | 1.CB.05a | C |
| ⓘ | var. Cliftonite | 1.CB.05a | C |
| ⓘ | Native Selenium | 1.CC.10 | Se |
| Group 2 - Sulphides and Sulfosalts | |||
| ⓘ | Pentlandite | 2.BB.15 | (NixFey)Σ9S8 |
| ⓘ | Sphalerite | 2.CB.05a | ZnS |
| ⓘ | Chalcopyrite | 2.CB.10a | CuFeS2 |
| ⓘ | Troilite | 2.CC.10 | FeS |
| ⓘ | Alabandite | 2.CD.10 | MnS |
| ⓘ | Daubréelite | 2.DA.05 | Fe2+Cr3+2S4 |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Chromite | 4.BB.05 | Fe2+Cr3+2O4 |
| ⓘ | Pyrolusite | 4.DB.05 | Mn4+O2 |
| ⓘ | Rutile | 4.DB.05 | TiO2 |
| Unclassified | |||
| ⓘ | 'Limonite' | - | |
| ⓘ | 'Clinopyroxene Subgroup' | - | |
| ⓘ | 'Fayalite-Forsterite Series' | - | |
| ⓘ | 'Pyroxene Group' | - | ADSi2O6 |
| ⓘ | 'Plessite' | - | |
List of minerals for each chemical element
Other Regions, Features and Areas containing this locality
Australia
- Bight BasinBasin
- Central Australian ElementCraton
- Eucla BasinBasin
- Officer BasinBasin
Australian PlateTectonic Plate
- South Australian Craton
- Coompana ProvinceShield
This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to
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for access and that you are aware of all safety precautions necessary.
References
Simpson, Edward S. (1938) Some new and little-known meteorites found in Western Australia. Mineralogical Magazine and Journal of the Mineralogical Society, 25 (163) 157-171 doi:10.1180/minmag.1938.025.163.01
DeLaeter, J. R. (1972) The Mundrabilla meteorite shower. Meteoritics, 7 (3). 285-294 doi:10.1111/j.1945-5100.1972.tb00442.x
Laeter, J.R.; Cleverly, W.H. (1983) Further finds from the Mundrabilla meteorite shower. Meteoritics, 18 (1). 29-34 doi:10.1111/j.1945-5100.1983.tb00574.x






Mundrabilla meteorite, Mundrabilla Roadhouse, Dundas Shire, Western Australia, Australia