meteorite

Iron-rich meteorite candidate

Unclassified meteoritic iron–stone material; possible stony-iron meteorite or terrestrial ironstone

AI-generated identification · may be incorrect

Dark brown-gray, irregular, granular surface with metallic-looking flecks; apparent hardness roughly 5–7, but composition and true properties cannot be determined visually. A weak magnetic response, fusion crust, unusually high density, and lack of vesicles would support a meteorite identification.

Identified August 16, 2026More meteorite →

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At a glance

Common name: Iron-rich meteorite candidate
Scientific name: Unclassified meteoritic iron–stone material; possible stony-iron meteorite or terrestrial ironstone
Category: meteorite
Identified: August 16, 2026
Method: Standard

AI Estimated Value

$0–$20 unverified; approximately $1–$10 per gram for a confirmed common meteorite, with rare authenticated types worth far more.

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 an asteroid’s parent body and may contain metal-rich phases such as kamacite and taenite, dating from Solar System formation about 4.56 billion years ago. Its appearance can also be produced by terrestrial ironstone, slag, or weathered sulfide-bearing rock.

Uses & applications

Confirmed meteorites are primarily valued by collectors and researchers; rare iron-stone specimens may be cut and polished. Unverified material has little commercial value.

Geological facts

The image alone cannot distinguish a meteorite from ordinary terrestrial rock or industrial slag; polished stone beneath it provides no diagnostic scale or context.

Field identification & locations

Check for strong magnetism, unusually high density, a thin dark fusion crust, and a streak that is not reddish-brown; avoid destructive tests. Professional classification requires petrographic examination and elemental/isotopic analysis.