meteorite

Probable metallic meteorite fragment

Unclassified iron meteorite candidate, chiefly kamacite (α-Fe–Ni alloy)

AI-generated identification · may be incorrect

Small, rounded silver-gray metallic specimen with pits and a dull-to-metallic luster; likely dense and magnetic, with Mohs hardness about 4–5. The holes may be vesicles, corrosion pits, or manufacturing marks, so identification from the image is uncertain.

Identified September 2, 2026More meteorite →

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At a glance

Common name: Probable metallic meteorite fragment
Scientific name: Unclassified iron meteorite candidate, chiefly kamacite (α-Fe–Ni alloy)
Category: meteorite
Identified: September 2, 2026
Method: Standard

AI Estimated Value

If authenticated: roughly $1–$20 per gram for common iron meteorite material; rare or documented specimens can exceed $100 per gram. If terrestrial metal: usually under $1.

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 extraterrestrial, it formed in a differentiated asteroid’s metallic core and survived atmospheric entry; most iron meteorites crystallized billions of years ago. It could instead be industrial metal or lead, requiring testing.

Uses & applications

Meteorites are valued for scientific study and collecting; iron meteorites are cut, polished, and etched to reveal Widmanstätten patterns. Ordinary metal has mainly scrap or craft value.

Geological facts

A strong magnet, unusually high density, fusion crust, and etched crystalline pattern support meteorite identification; a streak test and laboratory nickel analysis are more diagnostic.

Field identification & locations

Common sources include meteorite fields in Antarctica, deserts, and established finds worldwide. Test magnetism, density, streak, and nickel content, and avoid filing valuable material without expert advice.