Rock Identifier
Black basalt or dark volcanic rock fragment (Likely basalt, composed chiefly of plagioclase feldspar and pyroxene, with possible magnetite) — igneous
igneous

Black basalt or dark volcanic rock fragment

Likely basalt, composed chiefly of plagioclase feldspar and pyroxene, with possible magnetite

AI-generated identification · may be incorrect

Fine-grained, dark gray to black, generally dull to weakly vitreous; hardness about 5–6 Mohs, massive texture, no obvious cleavage, and relatively high density (~2.8–3.1 g/cm³). The image is somewhat blurry, so exact identification is limited.

Identified More igneous
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Physical properties

Fine-grained, dark gray to black, generally dull to weakly vitreous; hardness about 5–6 Mohs, massive texture, no obvious cleavage, and relatively high density (~2.8–3.1 g/cm³). The image is somewhat blurry, so exact identification is limited.

Formation & geological history

Basalt forms when mafic lava rapidly cools at or near Earth’s surface, commonly in oceanic crust, volcanic fields, and flood-basalt provinces. Specimen age cannot be determined from the image; basalt ranges from ancient Precambrian to modern.

Uses & applications

Used widely as crushed aggregate, roadstone, concrete material, building stone, and decorative landscaping rock; attractive polished pieces may be collected but usually have modest value.

Geological facts

Basalt is the most common volcanic rock and makes up much of the ocean floor. It may be weakly magnetic if it contains abundant magnetite.

Field identification & locations

Look for a uniformly fine-grained black surface, high density, and lack of visible large crystals; a streak, magnetism test, and fresh fracture help distinguish it from coal, slag, or shale. Common worldwide, especially volcanic regions.