Rock Identifier
Dark gray stream-worn cobble, likely basalt or andesite (Fine-grained mafic to intermediate volcanic rock; commonly basalt (plagioclase ± pyroxene ± olivine)) — igneous
igneous

Dark gray stream-worn cobble, likely basalt or andesite

Fine-grained mafic to intermediate volcanic rock; commonly basalt (plagioclase ± pyroxene ± olivine)

AI-generated identification · may be incorrect

Hardness about 5.5–6.5 Mohs; dark gray-brown, dull to faintly subvitreous, massive and fine-grained, with no visible cleavage. Rounded shape indicates abrasion by water or glacial transport; exact identification requires a fresh surface or testing.

Identified More igneous
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Physical properties

Hardness about 5.5–6.5 Mohs; dark gray-brown, dull to faintly subvitreous, massive and fine-grained, with no visible cleavage. Rounded shape indicates abrasion by water or glacial transport; exact identification requires a fresh surface or testing.

Formation & geological history

Formed when lava cooled rapidly at or near Earth’s surface, generally from the Cenozoic or older volcanic activity, then became rounded in a stream, beach, or glacial deposit.

Uses & applications

Used as aggregate, road base, riprap, landscaping stone, and occasionally decorative material; this ordinary cobble has little jewelry value.

Geological facts

Basalt is Earth’s most abundant volcanic rock and commonly forms oceanic crust and extensive lava flows.

Field identification & locations

Look for a dense, fine-grained dark interior, lack of foliation, and occasional tiny feldspar or olivine grains; a streak test, magnetism check, and fresh break help distinguish basalt from andesite or dark metamorphic rocks. Common worldwide in volcanic and glacial regions.