meteorite

Iron meteorite (probable)

Fe–Ni metallic meteorite, possibly an ordinary chondrite or iron-rich meteorite

AI-generated identification · may be incorrect

Dark brown-black, rounded, weathered surface with metallic patches; likely high density and magnetic, with Mohs hardness about 4–5. Exact crystal structure, nickel content, and Widmanstätten pattern cannot be determined from the image.

Identified August 11, 2026More meteorite →

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At a glance

Common name: Iron meteorite (probable)
Scientific name: Fe–Ni metallic meteorite, possibly an ordinary chondrite or iron-rich meteorite
Category: meteorite
Identified: August 11, 2026
Method: Standard

AI Estimated Value

If authenticated: roughly $1–$20 per gram for common material, or $50–$500+ for a small documented specimen; if terrestrial slag or concretion, usually under $10.

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

Formed in an asteroid parent body, likely more than 4.5 billion years ago, then melted or brecciated and delivered to Earth; its rounded shape may reflect atmospheric ablation and terrestrial weathering.

Uses & applications

Primarily a collector specimen; verified iron meteorites can be cut, polished, etched, or used in educational displays and jewelry. It is not normally used as construction material.

Geological facts

A genuine iron meteorite commonly shows fusion crust, regmaglypts, strong magnetism, and a nickel-bearing metal interior. Terrestrial iron-rich slag and limonite concretions can look similar.

Field identification & locations

Field checks include a strong magnet response, unusually high weight for size, and a thin streak or nickel test; laboratory analysis and meteoritical authentication are required. Common finds occur in deserts, Antarctica, and dry plains.