meteorite

Iron-rich meteorite candidate

Unclassified stony-iron or iron meteorite; requires testing

AI-generated identification · may be incorrect

Dark brown-black, metallic to earthy luster with rusty weathering and an irregular rounded shape. Likely dense and magnetic; hardness roughly 5–6 if stony, or 4–5 if mainly iron-nickel; visible metal grains may occur, but no diagnostic crystal structure is confirmed from the image.

Identified September 4, 2026More meteorite →

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Physical properties

Formation & geological history

If genuine, it formed from differentiated material in an asteroid and survived atmospheric entry, acquiring a fusion crust and terrestrial oxidation; its age would be approximately 4.56 billion years. The appearance could also represent terrestrial iron-rich slag or weathered ore, so laboratory confirmation is essential.

Uses & applications

Meteorites are primarily collectible and scientifically valuable; iron meteorites are cut and etched to reveal Widmanstätten patterns. Terrestrial iron ore may be used industrially, while slag generally has little commercial use.

Geological facts

Useful tests include a strong magnet, streak (meteorites usually leave little or no streak), density, nickel testing, and thin-section or elemental analysis. A true meteorite commonly shows a thin fusion crust, regmaglypts, and unusually high density.

Field identification & locations

Common meteorite candidates include ordinary chondrites, irons, and stony-irons from hot deserts and Antarctica. The specimen’s bubbly/granular texture and heavy oxidation are also consistent with slag, making an unverified identification impossible from the photograph alone.