meteorite

Polished star-shaped meteorite slice (likely iron meteorite)

Iron meteorite, principally kamacite (α-Fe–Ni) with taenite (γ-Fe–Ni)

AI-generated identification · may be incorrect

Dark metallic brown-gray, highly reflective polished surface, dense and opaque; Mohs hardness about 4–5, metallic luster, cubic metallic crystal structure, and no cleavage. The star shape appears human-cut, not natural crystal morphology.

Identified September 6, 2026More meteorite →

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At a glance

Common name: Polished star-shaped meteorite slice (likely iron meteorite)
Scientific name: Iron meteorite, principally kamacite (α-Fe–Ni) with taenite (γ-Fe–Ni)
Category: meteorite
Identified: September 6, 2026
Method: Standard

AI Estimated Value

About $20–$100 for an unverified decorative iron piece; approximately $100–$1,000+ for a documented, attractive iron meteorite slice.

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 from a differentiated asteroid’s metallic core and crystallized as it cooled over millions of years, commonly producing Widmanstätten patterns when etched. Most iron meteorites formed roughly 4.5 billion years ago.

Uses & applications

Used as collectible specimens, jewelry, display pieces, and scientific samples; value depends strongly on verified meteorite identity, locality, weight, and etched pattern.

Geological facts

The image alone cannot confirm extraterrestrial origin: polished iron or steel can look similar. A genuine iron meteorite is unusually heavy and typically reveals interlocking Widmanstätten figures after careful etching.

Field identification & locations

Check for very high density, nickel by laboratory analysis, and a fusion crust or etched Widmanstätten pattern; a magnet is attracted, but many terrestrial irons also attract magnets. Common sources include Campo del Cielo, Sikhote-Alin, and Canyon Diablo.