Rock Identifier
Iron-rich meteorite candidate (Probable ordinary chondrite or iron meteorite fragment; identification requires testing) — meteorite
meteorite

Iron-rich meteorite candidate

Probable ordinary chondrite or iron meteorite fragment; identification requires testing

AI-generated identification · may be incorrect

Dark gray-black, weakly metallic-looking surface with rusty yellow-brown weathering; apparent fusion crust or oxidation rind. Hardness likely about 5–6, but density, magnetism, and nickel content are needed for confirmation; no clear crystal structure is visible.

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Physical properties

Dark gray-black, weakly metallic-looking surface with rusty yellow-brown weathering; apparent fusion crust or oxidation rind. Hardness likely about 5–6, but density, magnetism, and nickel content are needed for confirmation; no clear crystal structure is visible.

Formation & geological history

If extraterrestrial, it formed in an asteroid and survived atmospheric entry, producing a dark fusion crust; terrestrial weathering caused the rusty patches. The image alone cannot establish its age or authenticity.

Uses & applications

Primarily a collector specimen; confirmed meteorites can have scientific and commercial value, while ordinary terrestrial slag or basalt has little value.

Geological facts

Potential indicators include unusual density, strong magnetism, rounded aerodynamic edges, and a thin dark fusion crust. Metallic flecks and rusty staining can also occur in terrestrial basalt, ironstone, or industrial slag.

Field identification & locations

Test with a magnet, measure density, inspect a cut face for chondrules or metal, and obtain a nickel test or laboratory classification; avoid destructive testing before expert review. Estimated value: $0–$10 if terrestrial slag/rock, roughly $1–$5 per gram if a common confirmed chondrite, and substantially more for rare types.