meteorite

Metallic meteorite fragment (probable stony-iron or iron meteorite)

Undetermined meteoritic Fe–Ni alloy with silicate minerals

AI-generated identification · may be incorrect

Irregular dark gray-brown fragment with a metallic-looking surface and possible fusion-crust remnant; exact hardness, density, magnetism, and crystal structure cannot be established from the photograph. The cavity may reflect weathering or a broken interior.

Identified August 16, 2026More meteorite →

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At a glance

Common name: Metallic meteorite fragment (probable stony-iron or iron meteorite)
Scientific name: Undetermined meteoritic Fe–Ni alloy with silicate minerals
Category: meteorite
Identified: August 16, 2026
Method: Standard

AI Estimated Value

If authenticated: roughly $50–$500+ for a small common fragment; officially classified or attractive specimens may exceed $1,000. If slag or terrestrial metal, usually under $5.

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

Likely formed in an asteroid’s differentiated interior and crystallized billions of years ago, then reached Earth after atmospheric entry. Terrestrial slag or industrial metal remains a possible visual look-alike requiring testing.

Uses & applications

Meteorites are primarily valued for scientific study and collecting; iron-rich specimens may be cut, polished, and displayed. No ordinary construction use is applicable.

Geological facts

A true iron meteorite commonly contains kamacite and taenite and may reveal a Widmanstätten pattern after etching; stony-iron types contain visible silicate crystals.

Field identification & locations

Test with a strong magnet, measure density, inspect for a thin fusion crust, and seek nickel testing or professional classification; ordinary rocks rarely combine strong magnetism with unusually high density. Common finds occur in deserts and Antarctica.