Narellan meteorite, Camden County, New South Wales, Australiai
| Regional Level Types | |
|---|---|
| Narellan meteorite | Meteorite Fall Location |
| Camden County | County |
| New South Wales | State |
| Australia | Country |
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Latitude & Longitude (WGS84):
34° 2' 59'' South , 150° 41' 29'' East
Latitude & Longitude (decimal):
Meteorite Class:
Meteoritical Society Class:
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Elderslie | 4,252 (2018) | 2.1km |
| Brownlow Hill | 379 (2012) | 2.9km |
| Camden South | 4,343 (2015) | 3.7km |
| Narellan | 7,350 (2018) | 3.8km |
| Cobbitty | 1,162 (2015) | 4.0km |
Nearest Clubs:
Local clubs are the best way to get access to collecting localities
Local clubs are the best way to get access to collecting localities
| Club | Location | Distance |
|---|---|---|
| Campbelltown and Districts Lapidary Club | Ingleburn, New South Wales | 17km |
| Fairfield & Districts Gemstone Club | Wakeley, New South Wales | 28km |
| Nepean District Lapidary Club Inc | St Marys, New South Wales | 32km |
| Bankstown and Districts Lapidary Club Inc | Bankstown, New South Wales | 34km |
| Rooty Hill and District Lapidary Club | Rooty Hill , New South Wales | 34km |
Ordinary chondrite (L6)
Fell, 8 April 1928, 17:15 hrs; 367.5 g
A small stone fell and was recovered. Olivine (Fa25.3) and low Ca-orthopyroxene (Fs21.4) compositions are characteristic of the L-chondrite geochemical group. Mineralogically the meteorite consists primarily of olivine and orthopyroxene accompanied by minor albitic plagioclase, troilite, and Fe-Ni metal. Accessory chromite and other minor opaques (copper, ilmenite and isocubanite) have also been reported. Chemical analysis suggests that other mineral phases may also be present. However, in the mid 20th century such phases would not always have been readily detected — even with larger meteorites — using the destructive wet-chemical techniques used in decades following the meteorite's fall. Chromite aggregates appear to be the product of pre-terrestrial shock. A Pb,Th:He gas release age of 3.21 Ga is probably another indication of at least one major post-formational collision.
The L-group of ordinary chondrites (relatively low in total iron) are the largest group of classified witnessed meteorite falls and account for ~45% of all well-classified meteorite falls. The L6 petrologic type account for ~ 70% of the group. 272 meteorite falls are currently classified exactly as 'L6' chondrites [June 2017].
189 g, approximately half of the original mass, has been kept at the Australian Museum in Sydney.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsMineral List
7 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 Description: Shock-produced chromite aggregates present. References: |
| ⓘ 'Fayalite-Forsterite Series' Description: Olivine composition [Fa25.3] @Mason,1974, |
| ⓘ Ilmenite Formula: Fe2+TiO3 |
| ⓘ Isocubanite Formula: CuFe2S3 |
| ⓘ Native Copper Formula: Cu |
| ⓘ Native Iron Formula: Fe |
| ⓘ Native Iron var. Kamacite Formula: (Fe,Ni) |
| ⓘ 'Orthopyroxene Subgroup' Description: Orthopyroxene composition [Fs21.4] @Mason,1974. |
| ⓘ 'Plagioclase' Formula: (Na,Ca)[(Si,Al)AlSi2]O8 |
| ⓘ Taenite Formula: (Fe,Ni) |
| ⓘ Troilite Formula: FeS |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 1 - Elements | |||
|---|---|---|---|
| ⓘ | Native Copper | 1.AA.05 | Cu |
| ⓘ | 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 | |||
| ⓘ | '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 | ⓘ Native Copper | Cu |
| Cu | ⓘ Isocubanite | CuFe2S3 |
Other Regions, Features and Areas containing this locality
Australia
- Lachlan OrogenOrogen
- Eastern ProvinceGeologic Province
- New South Wales
- ⭔CamdenCouncil
- ⭔SydneyCity
- Sydney BasinBasin
Australian PlateTectonic Plate
- Sydney-Surat BasinVolcanic Arc
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