
meteorite
Iron meteorite candidate
Likely an iron-rich meteorite, possibly a weathered octahedrite (Fe–Ni alloy); identification is uncertain from the image alone
AI-generated identification · may be incorrectDark brown-black, rounded and strongly weathered surface with metallic-looking exposed patches and cavities; likely dense, magnetic, and metallic-lustered. Iron meteorites typically have Mohs hardness about 4–5 and specific gravity 7–8.
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Physical properties
Dark brown-black, rounded and strongly weathered surface with metallic-looking exposed patches and cavities; likely dense, magnetic, and metallic-lustered. Iron meteorites typically have Mohs hardness about 4–5 and specific gravity 7–8.
Formation & geological history
Forms from differentiated asteroid cores and may be billions of years old, commonly ~4.5 billion years. Atmospheric melting produces a fusion crust, while terrestrial weathering creates rust, pits, and a brown coating.
Uses & applications
Collectors value genuine meteorites; iron meteorites are also studied for planetary differentiation and metallurgy. They have no ordinary construction use.
Geological facts
The appearance is compatible with a meteorite but cannot confirm one; slag, industrial iron, or hematite-rich rock can look similar. A nickel test, density measurement, magnetic response, and polished/etched examination are needed.
Field identification & locations
Check for strong magnetism, unusual density, a thin fusion crust, and no vesicles; test any suspected specimen with a meteorite laboratory rather than filing it extensively. Common iron meteorites include Campo del Cielo and Sikhote-Alin.