Iron
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Native iron is a cubic mineral occurring primarily as metallic gray masses in basaltic lava flows that have assimilated carbonaceous sediments, in reduced metamorphic rocks, and as the dominant component of iron and stony-iron meteorites. It has a Mohs hardness of 4–5 and a bright metallic luster, and terrestrial occurrences include classic localities in Disko Island, Greenland. Meteoritic native iron, particularly in the form of kamacite and taenite, represents the original building material of planetary bodies.