meteorite

Possible iron-rich meteorite or hematite-rich terrestrial stone

Unconfirmed; candidates include iron meteorite (Fe–Ni alloy) or hematite/magnetite (Fe₂O₃/Fe₃O₄)

AI-generated identification · may be incorrect

Dark gray-black, smooth and weakly metallic-looking with rounded edges; apparent hardness about 5–6, but the photograph cannot establish composition, magnetism, density, or crystal structure. A genuine iron meteorite commonly has high specific gravity (~7–8), strong magnetism, and a nickel-iron composition.

Identified September 3, 2026More meteorite →

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At a glance

Common name: Possible iron-rich meteorite or hematite-rich terrestrial stone
Scientific name: Unconfirmed; candidates include iron meteorite (Fe–Ni alloy) or hematite/magnetite (Fe₂O₃/Fe₃O₄)
Category: meteorite
Identified: September 3, 2026
Method: Standard

AI Estimated Value

$0–$20 if ordinary terrestrial ironstone or slag; roughly $1–$10 per gram for an authenticated common iron meteorite, with exceptional specimens worth much more.

Not an official valuation

AI estimate for general interest only — not an appraisal. Actual value depends on condition, provenance, and market demand. Verify with a professional before buying, selling, or insuring.

This identification was generated by AI and may contain errors. Verify important details before relying on them — and never use an AI result to judge whether a specimen is safe to handle. Read the full disclaimer

Physical properties

Formation & geological history

If meteoritic, it formed in a differentiated asteroid and may be billions of years old; its rounded surface could reflect atmospheric ablation and terrestrial weathering. If terrestrial, it may be weathered ironstone, hematite, magnetite, or industrial slag.

Uses & applications

Iron meteorites are mainly collectible; hematite and magnetite are iron ores, while slag has industrial origin but little geological value.

Geological facts

The surface does not clearly show diagnostic regmaglypts or a fusion crust, so visual identification is unreliable. A streak test, magnet test, specific-gravity measurement, and laboratory nickel analysis are needed.

Field identification & locations

Check for strong magnetism, an unglazed reddish-brown/gray streak, unusually high density, and a thin polished window; avoid destructive testing until examined by a meteorite specialist. Common meteorite finds occur in deserts and Antarctica.