The following are some general guidelines, but do not replace specimen examination by a meteoriticist. Please note, the CGS does not provide meteorite testing or appraisal services.
There are a few simple tests to help determine if what you have could be a meteorite:
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What color is the sample? Meteorites are usually dark brown or black.
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Does the sample contain vesicles (small holes formed by gases escaping during solidification of the rock)? Meteorites typically lack vesicles.
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Does the sample have a fusion crust? Most meteorites have a dark, ash like crust on the surface, which is darker than the interior.
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Is the sample magnetic? Meteorites are almost always magnetic.
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Is the sample relatively heavy for its size? Most meteorites are very dense, about 3 times denser than a typical earth rock.
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Is the sample smooth? Meteorites are typically smooth. They may have shallow depressions on the surface known as “regmaglypts”, which should not be mistaken for
vesicles.
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Is the sample angular or rounded? Meteorites are generally angular.
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Are metallic specks present on a freshly broken surface? Iron-nickel meteorites typically have metallic specks on freshly broken surfaces--as opposed to entirely metallic surfaces.
Here are additional resources to help you determine if your find is a meteorite:
Gem and mineral shows, as well as your local gem and mineral club, can be great resources for meteorite identification as well.
Web page by:
California Geological Survey - Mineral Resources Program