meteorite

Iron meteorite fragment (likely metallic meteorite)

Fe–Ni kamacite/taenite alloy; exact identification requires testing

AI-generated identification · may be incorrect

Small irregular gray-metallic fragment with a dull-to-slightly reflective luster; apparent hardness about 4–6, no visible cleavage, and likely high density. The image alone cannot distinguish meteorite metal from industrial slag or ordinary iron-bearing rock.

Identified August 25, 2026More meteorite →

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At a glance

Common name: Iron meteorite fragment (likely metallic meteorite)
Scientific name: Fe–Ni kamacite/taenite alloy; exact identification requires testing
Category: meteorite
Identified: August 25, 2026
Method: Standard

AI Estimated Value

Unverified suspected fragment: $0–$20; authenticated ordinary iron meteorite: roughly $1–$10 per gram, with rare types substantially higher.

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 genuine, it formed in a differentiated asteroid’s metallic core and crystallized billions of years ago, commonly 4.5 billion years old, before falling to Earth. Its rough shape may reflect atmospheric breakup or terrestrial weathering.

Uses & applications

Authentic meteorites are primarily collector and research specimens; iron meteorites may be cut, etched, and displayed. Value depends strongly on verified classification, mass, provenance, and aesthetics.

Geological facts

A magnet attraction, unusually high density, and a fused dark crust can support identification, but are not conclusive. Many suspected meteorites are slag, rusted industrial metal, or furnace byproducts.

Field identification & locations

Check for strong magnetism, density, a thin fusion crust, and absence of abundant bubbles; avoid grinding until tested. Professional analysis using nickel content and microscopy is required; common finds occur in deserts and Antarctica.