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More model informationThis rock, a meteorwrong, shows some interesting features, such as small fractures at the surface that one could interpret at contraction cracks of a fusion crust. On places the outer layer is broken off, but this layer is too thick for a fusion crust. Its interior is also fine-grained and flaky. Overall this object would be a terrestrial rock, likely well rounded due to fluvial transport, but it is not a meteorite.
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