meteorite

Possible iron meteorite

Iron meteorite, likely kamacite–taenite alloy

AI-generated identification · may be incorrect

Dark metallic-gray, irregular specimen with rusty oxidation along edges and possible shallow regmaglypts; metallic luster. Typical iron meteorites have Mohs hardness about 4–5, high density (7–8 g/cm³), and no cleavage; identification cannot be confirmed from the image alone.

Identified August 16, 2026More meteorite →

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Physical properties

Formation & geological history

Formed in the differentiated metallic core of an asteroid and crystallized over geological time, commonly producing iron–nickel alloys. It reached Earth as a meteorite after atmospheric entry; terrestrial age is unknown.

Uses & applications

Primarily collected as a meteorite; cut and polished slices may display Widmanstätten patterns and are used in jewelry and scientific study. Value depends strongly on verified extraterrestrial origin, classification, and mass.

Geological facts

The dark fusion crust and heavy-looking metallic body are consistent with a meteorite, but ordinary terrestrial iron-rich rocks can look similar. A magnet, density measurement, nickel test, and laboratory classification are needed.

Field identification & locations

Common candidates are found in deserts, Antarctica, and cultivated fields; this beach setting also permits terrestrial slag or ironstone contamination. Test for strong magnetism, unusually high density, and lack of vesicles, then seek an accredited meteorite laboratory.