meteorite

Likely iron meteorite fragment

Fe–Ni metallic meteorite, possibly an octahedrite (kamacite–taenite alloy)

AI-generated identification · may be incorrect

Dark, irregular, heavily textured metallic specimen; fresh iron meteorites are dense, magnetic, and typically have a metallic luster. Mohs hardness is about 4–5, with specific gravity commonly 7.3–7.8; the blue lighting obscures true color and surface details.

Identified September 7, 2026More meteorite →

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At a glance

Common name: Likely iron meteorite fragment
Scientific name: Fe–Ni metallic meteorite, possibly an octahedrite (kamacite–taenite alloy)
Category: meteorite
Identified: September 7, 2026
Method: Standard

AI Estimated Value

About $10–$100 for an unverified iron-like fragment; $100–$1,000+ for authenticated, attractive meteorite material depending on mass and provenance.

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

Formed in the metallic core of a differentiated asteroid roughly 4.5 billion years ago, then released by impact and surviving atmospheric entry. Sculpted or pitted surfaces may reflect ablation, weathering, or handling.

Uses & applications

Primarily a collector specimen; cut and etched pieces may display Widmanstätten patterns. It has little practical industrial use at specimen scale.

Geological facts

Identification cannot be confirmed visually from this image alone; terrestrial iron slag, magnetite, or weathered metal can look similar. A nickel test, strong magnet response, density measurement, and laboratory analysis are useful.

Field identification & locations

Common sources include Northwest Africa, Antarctica, and historically Campo del Cielo and Sikhote-Alin. Look for fusion crust, regmaglypts, unusual density, magnetism, and a non-rusty metallic interior; obtain certified provenance.