Rock Identifier
Tumbled dark gray stone, possibly basalt or andesite (Fine-grained mafic to intermediate volcanic rock; exact mineralogy cannot be confirmed from the photograph) — igneous
igneous

Tumbled dark gray stone, possibly basalt or andesite

Fine-grained mafic to intermediate volcanic rock; exact mineralogy cannot be confirmed from the photograph

AI-generated identification · may be incorrect

Hardness about 5.5–6.5 Mohs; dark gray with pale weathering spots, dull to weakly vitreous luster, and no visible crystals or cleavage. Likely composed mainly of plagioclase, pyroxene, and possibly magnetite.

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Physical properties

Hardness about 5.5–6.5 Mohs; dark gray with pale weathering spots, dull to weakly vitreous luster, and no visible crystals or cleavage. Likely composed mainly of plagioclase, pyroxene, and possibly magnetite.

Formation & geological history

Probably formed when volcanic lava cooled rapidly at or near Earth’s surface; such rocks range from young lava flows to Precambrian material. The rounded shape appears human-tumbled or naturally water-worn.

Uses & applications

Used as aggregate, road stone, landscaping material, and occasionally as a low-cost polished specimen; generally has little jewelry value.

Geological facts

Basalt is the most abundant volcanic rock on oceanic crust, while andesite commonly forms at volcanic arcs. A magnet may attract it weakly if magnetite is present.

Field identification & locations

Look for a fine-grained, heavy, nonfoliated texture and a dark streak or pale gray interior; a streak, magnet, and hardness test help distinguish it from slag or soft sedimentary rock. Common worldwide, especially volcanic regions and stream gravels.