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Edeowie glass
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Edeowie glass is a , or , found in the Australian state of . It is -like, opaque material found as vesicular free forms or sheet-like/ropy masses. It is located throughout a semi-continuous swath in baked pod-like in an area of about long by along the western side of the near Parachilna and east of . The region in which this glass is found is mostly restricted to concentrations correlated to the ancient shoreline terrace sequence at the locality. It is typically black in appearance, but can occur as variegated grey-green with various streak-like impurities. Pale grey and red-brownish surfaces can be caused by chemical weathering (, mineralization) and .Haines, P.W., R.J.F. Jenkins, and S.P. Kelley, 2001, Pleistocene glass in the Australian desert: The case for an impact origin. Geology. v. 29, no. 10, pp. 899–902.Macdonald, F.A., K. Mitchell, and S.E. Cina, 2004, Evidence for a Lightning-Strike Origin of the Edeowie Glass. 35th Lunar and Planetary Science Conference, March 15–19, 2004, League City, Texas, abstract no.1406.Gifford, A. C., 1999, Journal of the Royal Society of Western Australia, 82:165–168, 1999


Origin
Proposed origins for Edeowie and other similar lechatelierites include grassland fires, strikes, or hypervelocity impact by one or several or . Some features, such as planar deformation features () in quartz crystals found within and associated with Edeowie glass, are usually caused by extreme pressures and temperatures.


Interval of formation
Edeowie glass yields dates spanning 0.67–0.07 mya (~670,000–70,000 BP), but some outlier dates are as recent as the middle .


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