meteorite

Iron-rich meteorite candidate

Unclassified iron meteorite, possibly an ordinary chondrite or weathered iron oxide-rich meteorite

AI-generated identification · may be incorrect

Dark brown-black, massive, dull to weakly metallic surface with rounded edges and weathering pits; apparent hardness about 5–6, but composition cannot be confirmed visually. A magnet response and streak test are needed; terrestrial ironstone or slag can look similar.

Identified August 9, 2026More meteorite →

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At a glance

Common name: Iron-rich meteorite candidate
Scientific name: Unclassified iron meteorite, possibly an ordinary chondrite or weathered iron oxide-rich meteorite
Category: meteorite
Identified: August 9, 2026
Method: Standard

AI Estimated Value

$0–$20 if terrestrial ironstone or slag; approximately $50–$500+ if authenticated as a common meteorite, 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

If meteoritic, it formed in an asteroid’s differentiated metal-rich interior or primitive parent body and crystallized billions of years ago, commonly about 4.5 billion years old. The photograph alone cannot establish extraterrestrial origin.

Uses & applications

Meteorites are primarily collected and studied; iron meteorites may be cut, polished, and etched to reveal Widmanstätten patterns. Ironstone has limited ornamental or educational use, while slag is industrial waste.

Geological facts

The irregular, dark weathered appearance is compatible with a meteorite but is not diagnostic. Strong magnetism, unusually high density, a thin fusion crust, and absence of abundant vesicles support meteorite identification.

Field identification & locations

Check density, magnetism, and a carefully chosen unglazed-ceramic streak test; meteorites generally do not leave a red-brown streak, unlike hematite-rich rocks. Professional nickel testing and petrographic analysis are recommended.