Rock Identifier
Likely weathered iron-rich meteorite (Unclassified stony-iron or iron meteorite candidate; confirmation requires laboratory testing) — meteorite
meteorite

Likely weathered iron-rich meteorite

Unclassified stony-iron or iron meteorite candidate; confirmation requires laboratory testing

AI-generated identification · may be incorrect

Dark gray-brown, strongly weathered, irregularly rounded specimen with possible fusion-crust-like surface and metallic-looking patches. Suspected meteorites are typically dense, magnetic, and may show a nickel-iron matrix; hardness is roughly 4–6, but these features are not diagnostic from an image.

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Physical properties

Dark gray-brown, strongly weathered, irregularly rounded specimen with possible fusion-crust-like surface and metallic-looking patches. Suspected meteorites are typically dense, magnetic, and may show a nickel-iron matrix; hardness is roughly 4–6, but these features are not diagnostic from an image.

Formation & geological history

If genuine, it formed in an asteroid body and crystallized billions of years ago before falling to Earth; terrestrial weathering has produced the rusty brown coating. Appearance alone cannot exclude slag, basalt, or iron-rich industrial debris.

Uses & applications

Meteorites are valued for scientific study and collecting; verified specimens may be cut and polished for display or jewelry. Unverified finds have little market value.

Geological facts

The apparent melted-looking exterior may represent fusion crust, but slag commonly looks similar. A magnet test, density measurement, streak test, and nickel/elemental analysis are needed.

Field identification & locations

Check for strong magnetism, unusually high density, a thin continuous fusion crust, and interior metal flecks; avoid destructive testing before professional examination. Common finds occur in deserts and Antarctica.