Rock Identifier
Rounded gray river cobble, likely basaltic-andesite or andesite (Fine-grained intermediate to mafic volcanic rock; commonly plagioclase ± pyroxene, with possible alteration minerals) — igneous
igneous

Rounded gray river cobble, likely basaltic-andesite or andesite

Fine-grained intermediate to mafic volcanic rock; commonly plagioclase ± pyroxene, with possible alteration minerals

AI-generated identification · may be incorrect

Hardness about 5.5–6.5 Mohs; medium gray, dull to weakly granular luster, massive and nonfoliated, with no obvious cleavage. The smooth rounded shape indicates prolonged water or sediment abrasion.

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Physical properties

Hardness about 5.5–6.5 Mohs; medium gray, dull to weakly granular luster, massive and nonfoliated, with no obvious cleavage. The smooth rounded shape indicates prolonged water or sediment abrasion.

Formation & geological history

Formed when lava cooled at or near Earth’s surface, likely during a relatively young volcanic episode; exact age cannot be determined from the photograph. It was later transported and rounded in a stream, beach, or glacial environment.

Uses & applications

Commonly used as landscaping stone, riprap, aggregate, and construction fill; generally has little jewelry value unless unusually patterned or polished.

Geological facts

The specimen appears dense and fine-grained, with scattered lighter mineral grains and possible weathering spots. A fresh broken surface would better distinguish basalt from andesite.

Field identification & locations

Common in volcanic terrains and river gravels worldwide, including the Pacific Northwest, Iceland, Japan, and the Andes. Field tests include checking for high density, lack of visible quartz, and a streakless surface; a magnet may show weak attraction if magnetite is present.