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| Abstract: | The 15.5‐ton main mass of the Willamette iron on display at the American Museum of Natural History in New York. The deep cavities are characteristic of one side of the meteorite; they were produced by corrosion. Alan Rubin et al. discuss shock effects in the meteorite in their paper on pp. 1984–1994. Image © 2007 Darryl Pitt/Macovich. |
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