Rock Identifier
Likely rough metallic meteorite fragment (Unclassified iron or stony-iron meteorite; identification is uncertain from the image alone) — meteorite
meteorite

Likely rough metallic meteorite fragment

Unclassified iron or stony-iron meteorite; identification is uncertain from the image alone

AI-generated identification · may be incorrect

Small gray-brown, heavily weathered piece with metallic-looking reflective surfaces and irregular texture; hardness likely around 5–6+, with potentially high specific gravity and weak magnetism if iron-rich. No reliable crystal structure, cleavage, or luster can be confirmed visually.

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Physical properties

Small gray-brown, heavily weathered piece with metallic-looking reflective surfaces and irregular texture; hardness likely around 5–6+, with potentially high specific gravity and weak magnetism if iron-rich. No reliable crystal structure, cleavage, or luster can be confirmed visually.

Formation & geological history

Possible extraterrestrial material formed in an asteroidal body and delivered by impact, but terrestrial slag, metal-rich rock, or industrial debris can look similar. Geological age would typically exceed 4.5 billion years if genuinely meteoritic.

Uses & applications

Meteorites are primarily collectible and scientifically valuable; iron-rich pieces may be cut, polished, or displayed as specimens. Commercial value depends strongly on verified classification and provenance.

Geological facts

A visible metallic appearance is not diagnostic: slag and hematite-rich rocks commonly mimic meteorites. Confirmation requires a strong magnet test, density measurement, nickel/iron analysis, and ideally laboratory classification.

Field identification & locations

Check for an unusually high density, fusion crust, regmaglypts, and attraction to a magnet; avoid cutting before testing. Common meteorite finds occur in deserts and Antarctica, whereas this appearance alone cannot establish locality.