meteorite

Iron-rich meteorite candidate

Probable stony-iron or iron meteorite; exact classification requires testing

AI-generated identification · may be incorrect

Dark gray-black, metallic to dull luster with rusty-red oxidation; irregular, dense-looking fragment. Likely Mohs hardness ~4–6, with possible weak magnetism; crystal structure and specific gravity are undetermined from the image.

Identified August 13, 2026More meteorite →

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Physical properties

Formation & geological history

If genuine, it formed in a differentiated asteroid and crystallized billions of years ago before reaching Earth as a meteorite. The reddish areas likely represent terrestrial weathering of iron-bearing metal.

Uses & applications

Meteorites are primarily scientific and collector specimens; iron meteorites may be cut, polished, and etched to reveal Widmanstätten patterns. No conventional construction use.

Geological facts

A photograph cannot confirm a meteorite: dark terrestrial rocks such as basalt, slag, and magnetite commonly look similar. Strong magnetism, unusually high density, a fusion crust, and nickel detection are important clues.

Field identification & locations

Common meteorite localities include Antarctica, deserts, and known strewn fields worldwide. Test with a magnet, inspect for a thin fusion crust, measure density, and seek nickel/elemental analysis; avoid destructive tests until examined.