meteorite

Iron-rich meteorite candidate

Undetermined stony-iron or iron meteorite; possible weathered iron meteorite

AI-generated identification · may be incorrect

Dark brown, irregular, heavily weathered surface with possible metallic flecks; likely dense and weakly magnetic. Mineralogy, hardness, crystal structure, and specific gravity cannot be confirmed from the image alone; test magnetism and streak, and inspect a cut face for metal.

Identified August 14, 2026More meteorite →

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Physical properties

Formation & geological history

If extraterrestrial, it formed in a differentiated asteroid and may contain iron–nickel metal and silicate minerals, dating to Solar System formation about 4.56 billion years ago. Terrestrial iron-rich slag, limonite, or sulfide ore are important alternatives.

Uses & applications

Authentic meteorites are mainly valued by collectors and researchers; iron-rich terrestrial rocks may have limited use as ore specimens. Do not cut or acid-test a potentially rare specimen before professional examination.

Geological facts

The shape and brown fusion-like crust are suggestive but not diagnostic; weathered terrestrial rocks and industrial slag can look similar. A laboratory nickel test, thin section, and elemental analysis are needed for confirmation.

Field identification & locations

Common meteorite indicators include unusual density, strong magnetism, a thin fusion crust, regmaglypts, and no bubbly vesicles; a fresh interior may show metal. Possible meteorites occur worldwide, especially in dry deserts and Antarctica, but identification requires a university, museum, or qualified meteorite laboratory.