meteorite

Small metallic meteorite fragment (probable chondrite)

Unclassified ordinary chondrite; composition chiefly Fe–Ni metal, olivine, and pyroxene

AI-generated identification · may be incorrect

Irregular dark gray-brown fragment with metallic-looking flecks and possible fusion crust; typical meteorite hardness is about 6–7 Mohs, dense, opaque, and weakly to strongly magnetic. The image is insufficient for reliable mineral or meteorite confirmation.

Identified August 9, 2026More meteorite →

Explore Small metallic meteorite fragment (probable chondrite) in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

App Store Google Play

At a glance

Common name: Small metallic meteorite fragment (probable chondrite)
Scientific name: Unclassified ordinary chondrite; composition chiefly Fe–Ni metal, olivine, and pyroxene
Category: meteorite
Identified: August 9, 2026
Method: Standard

AI Estimated Value

Unverified suspect fragment: $0–$20; authenticated ordinary chondrite: roughly $1–$10 per gram, with rare types worth substantially 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 the early Solar System about 4.56 billion years ago and later survived atmospheric entry as a meteorite fragment. Its terrestrial location and geological classification cannot be determined visually.

Uses & applications

Primarily used for scientific study and collecting; attractive authenticated specimens may be sold as display pieces or jewelry components. It has no ordinary construction use.

Geological facts

Most suspected meteorites are terrestrial slag, ironstone, or weathered rock. Confirmation requires density, magnetic response, nickel testing, petrographic examination, and ideally laboratory classification.

Field identification & locations

Possible indicators include unusually high density, a thin dark fusion crust, rounded aerodynamic edges, and magnetism; a fresh cut surface may show metal grains or chondrules. Do not rely on appearance alone.