meteorite

Iron-rich meteorite (probable stony-iron or weathered iron meteorite)

Unclassified meteorite; likely Fe–Ni metal with silicate minerals

AI-generated identification · may be incorrect

Dark brown, heavily weathered, metallic to submetallic luster with scattered reflective grains; apparent hardness about 5–6 for silicates, with irregular fracture and possible magnetic response. The image alone cannot confirm a fusion crust, Widmanstätten pattern, or meteorite composition.

Identified September 10, 2026More meteorite →

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At a glance

Common name: Iron-rich meteorite (probable stony-iron or weathered iron meteorite)
Scientific name: Unclassified meteorite; likely Fe–Ni metal with silicate minerals
Category: meteorite
Identified: September 10, 2026
Method: Standard

AI Estimated Value

If authenticated: roughly $1–$20 per gram for common meteorites, potentially much higher for rare types; as an unverified specimen, usually $0–$20.

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

Potentially extraterrestrial material formed in an asteroid’s differentiated interior roughly 4.5 billion years ago, then altered by terrestrial oxidation after landing. It could also be an Earth rock such as iron-rich basalt, slag, or sulfide-bearing ore, so laboratory testing is essential.

Uses & applications

Authenticated meteorites are collected and studied; iron meteorites may be cut and etched for display or jewelry. Non-meteorite iron-rich rocks generally have limited ornamental or educational value.

Geological facts

A strong magnet, unusually high density, nickel detection, and polished-section analysis help distinguish meteorites from terrestrial rocks. Rust alone is not diagnostic, and slag commonly mimics meteorites.

Field identification & locations

Common meteorite localities include deserts, Antarctica, and dry plains; suspected specimens should be weighed, magnet-tested, and examined for vesicles, but avoid cutting before professional evaluation. Identification requires petrography and elemental analysis.