Rock Identifier
Likely weathered basalt (Basalt; fine-grained mafic volcanic rock composed mainly of plagioclase and pyroxene, often with olivine) — igneous
igneous

Likely weathered basalt

Basalt; fine-grained mafic volcanic rock composed mainly of plagioclase and pyroxene, often with olivine

AI-generated identification · may be incorrect

Dark gray-brown, dull to subtly granular, dense, and massive with irregular fracture; typically Mohs 5–6 and specific gravity about 2.8–3.0. The image’s weathered surface makes crystal size and exact composition uncertain.

Identified More igneous
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Physical properties

Dark gray-brown, dull to subtly granular, dense, and massive with irregular fracture; typically Mohs 5–6 and specific gravity about 2.8–3.0. The image’s weathered surface makes crystal size and exact composition uncertain.

Formation & geological history

Basalt forms when iron- and magnesium-rich lava cools rapidly at or near Earth’s surface, commonly in volcanic fields, oceanic crust, and flood-basalt provinces. Its age cannot be determined from the photograph; weathering has produced the brown coating.

Uses & applications

Used as crushed aggregate, road base, railroad ballast, riprap, and building stone; attractive polished pieces may be collected, though this specimen appears ordinary.

Geological facts

Basalt is the most abundant volcanic rock and makes up much of the ocean floor. It commonly weathers to brown or reddish iron-oxide surfaces.

Field identification & locations

Look for high density, dark color, fine grain, and possible tiny pale plagioclase specks; it should not fizz in dilute hydrochloric acid. Common worldwide, especially volcanic regions; a laboratory test or fresh broken surface is needed to distinguish it from andesite or weathered gabbro.