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ISS028-E-14782

ISS028-E-14782         Click the photo number to access all resolutions available and the database record.

Shoemaker Impact Structure, Western Australia: The Shoemaker (formerly Teague) Impact Structure—located in Western Australia to the southeast of the Carnarvon Range—presents an other-worldly appearance in this astronaut photograph. The Shoemaker impact site is approximately 30 kilometers (19 miles) in diameter and clearly defined by concentric ring structures formed in sedimentary rocks (brown to dark brown, image center). The rocks were deformed by the impact event approximately 1.63 billion years ago (as reported by the Earth Impact Database). Other age-dating analyses of granitic rocks at the core of the structure call this age into question (Pirajno et al. 2003). Several saline and ephemeral lakes—Nabberu, Teague, Shoemaker, and numerous smaller ponds—occupy the land surface between the ring structures. Differences in color result from both water depth and from suspended sediments, with some bright salt crusts visible around the edges of smaller ponds (image center). A Landsat 7 view of the Shoemaker structure illustrates the extent of these ephemeral lakes, or playas, in the region. The Teague Impact Structure was renamed Shoemaker in honor of Dr. Eugene M. Shoemaker (1928-1997), a pioneer in impact crater studies and planetary geology, as well as the founder of the Astrogeology Branch of the U.S. Geological Survey. Reference Pirajno F., Hawke, P., Glikson, A.Y., Haines, P.W., and Uysal, T. (2003). Shoemaker impact structure, Western Australia. Australian Journal of Earth Sciences, 50:775-796.

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