The Shoemaker Meteorite Impact crater was previously known as the Lake Teague Ring Structure but was renamed the Shoemaker impact structure in honour of the late Gene Shoemaker and as a tribute to his and Caroline Shoemaker’s work on Australian impact structures. The structure has a diameter of about 30km.
The structure covers the southern part of the Western Proterozoic Earaheedy Basin which overlies the Archaean Yilgarn Craton to the south. Iron formation of the Frere Formation has been mapped on the tenements, and rock chip sampling by Galaxy has returned values up to 58.8%Fe. |