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Veevers meteorite, Veevers Crater, Gibson desert, Western Australia, Australia

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Latitude & Longitude (WGS84): 22° 58' 12'' South , 125° 22' 21'' East
Latitude & Longitude (decimal): -22.97003,125.37267
GeoHash:G#: qgcjkfmtf
Locality type:Meteorite Fall Location
Meteorite Class:IIAB iron meteorite
Meteoritical Society Class:Iron, IIAB
Metbull:View entry in Meteoritical Bulletin Database
Köppen climate type:BWh : Hot deserts climate


Veevers crater is an impact crater located on a flat desert plain between the Great Sandy and Gibson Deserts in the center of the state of Western Australia, Australia. The site is very remote and difficult to visit.

The iron meteorite fragments collected around the crater are classified as a coarse octahedrite belonging to chemical class IIAB; the fragments show considerable evidence of deformation presumably related to the impact explosion.[7] It has been inferred that the original meteorite was in the size range of 100-1000 tonnes, probably closer to the latter, now dispersed as fragments within the crater breccia and ejecta.


Mineral List


2 valid minerals.

Meteorite/Rock Types Recorded

Note: this is a very new system on mindat.org and data is currently VERY limited. Please bear with us while we work towards adding this information!

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Regional Geology

This geological map and associated information on rock units at or nearby to the coordinates given for this locality is based on relatively small scale geological maps provided by various national Geological Surveys. This does not necessarily represent the complete geology at this locality but it gives a background for the region in which it is found.

Click on geological units on the map for more information. Click here to view full-screen map on Macrostrat.org

Cenozoic
0 - 66 Ma



ID: 928046
sand plain 38499

Age: Cenozoic (0 - 66 Ma)

Description: Sand or gravel plains; may include some residual alluvium; quartz sand sheets commonly with ferruginous pisoliths or pebbles; local clay, calcrete, laterite, silcrete, silt, colluvium

Comments: regolith; synthesis of multiple published descriptions

Lithology: Regolith

Reference: Raymond, O.L., Liu, S., Gallagher, R., Zhang, W., Highet, L.M. Surface Geology of Australia 1:1 million scale dataset 2012 edition. Commonwealth of Australia (Geoscience Australia). [5]

Cretaceous
66 - 145 Ma



ID: 3185296
Mesozoic sedimentary rocks

Age: Cretaceous (66 - 145 Ma)

Comments: Canning Basin

Lithology: Conglomerate,siltstone,shale,sandstone

Reference: Chorlton, L.B. Generalized geology of the world: bedrock domains and major faults in GIS format: a small-scale world geology map with an extended geological attribute database. doi: 10.4095/223767. Geological Survey of Canada, Open File 5529. [154]

Data and map coding provided by Macrostrat.org, used under Creative Commons Attribution 4.0 License



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 visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders for access and that you are aware of all safety precautions necessary.

References

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Earth Impact Database. University of New Brunswick. Retrieved 2009-08-20.
Bevan A, McNamara K (1993). Australia's Meteorite Craters. Western Australian Museum. ISBN 0-7309-5926-0
Yeates AN, Crowe, RWA, Towner RR (1976). "The Veevers crater; a possible meteoritic feature". BMR Journal of Australian Geology & Geophysics 1: 77–8.
Shoemaker EM, Shoemaker CS (1985). "Impact structures of Western Australia". Meteoritics 20: 754–6. PDF
Shoemaker EM, Macdonald FA, Shoemaker CS (2005). "Geology of five small Australian impact craters". Australian Journal of Earth Sciences 52 (4-5): 529–44. Bibcode:2005AuJES..52..529S. doi:10.1080/08120090500180921. Abstract
Bevan AWR (1996). "Australian crater-forming meteorites". AGSO Journal of Australian Geology & Geophysics 16: 421–9.

 
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