Rock Identifier
Possible basaltic volcanic rock or iron-rich meteorite (Likely basalt (plagioclase–pyroxene rock); meteorite status cannot be confirmed visually) — igneous
igneous

Possible basaltic volcanic rock or iron-rich meteorite

Likely basalt (plagioclase–pyroxene rock); meteorite status cannot be confirmed visually

AI-generated identification · may be incorrect

Dark gray-black, fine-grained, dull to weakly submetallic surface with irregular weathering and a possible pale mineral vein. Basalt typically has Mohs hardness 6, no cleavage, and specific gravity about 2.8–3.1; metallic meteorites are much denser and magnetic.

Identified More igneous
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Physical properties

Dark gray-black, fine-grained, dull to weakly submetallic surface with irregular weathering and a possible pale mineral vein. Basalt typically has Mohs hardness 6, no cleavage, and specific gravity about 2.8–3.1; metallic meteorites are much denser and magnetic.

Formation & geological history

Basalt forms when mafic lava cools rapidly at or near Earth’s surface, commonly in volcanic fields and oceanic crust. The rounded, weathered shape may also be anthropogenic or glacial; no geological age can be assigned from the image.

Uses & applications

Basalt is used as aggregate, roadstone, dimension stone, and occasionally in carvings. If meteoritic, value depends on verified extraterrestrial origin and classification.

Geological facts

The specimen’s shape and texture are not diagnostic of a meteorite; many terrestrial basalt fragments look similar. A magnet test, streak test, fresh cut surface, and laboratory elemental/isotopic analysis are needed for confirmation.

Field identification & locations

Check for vesicles, a gray-white streak, and abundant tiny crystals—features favoring basalt; a strong magnetic response, fusion crust, and nickel-iron metal favor meteorite. Common basalt sources include volcanic regions worldwide; submit suspected meteorites to a recognized laboratory.