Rock Identifier
Polished dark stone, likely basalt (Basalt; chiefly plagioclase feldspar, pyroxene, and commonly olivine) — igneous
igneous

Polished dark stone, likely basalt

Basalt; chiefly plagioclase feldspar, pyroxene, and commonly olivine

AI-generated identification · may be incorrect

Fine-grained, dark gray to black, with a glassy-to-dull polished luster; hardness about 5–6 Mohs, no visible cleavage, and typical specific gravity 2.8–3.0. The rounded shape indicates tumbling or water wear.

Identified More igneous
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Physical properties

Fine-grained, dark gray to black, with a glassy-to-dull polished luster; hardness about 5–6 Mohs, no visible cleavage, and typical specific gravity 2.8–3.0. The rounded shape indicates tumbling or water wear.

Formation & geological history

Basalt forms when mafic lava rapidly cools at or near Earth’s surface, commonly in volcanic fields and oceanic crust. It may range from recent lava to ancient specimens billions of years old.

Uses & applications

Used widely as crushed aggregate, roadstone, building stone, and occasionally as polished decorative or worry stones; it has little jewelry value.

Geological facts

Its dark color comes from iron- and magnesium-rich minerals. A magnet may show weak attraction if the basalt contains magnetite.

Field identification & locations

Identify it by its uniformly fine texture, high density, dark color, and lack of obvious crystals; it can resemble polished slag, jasper, or dark glass, so a streak and hardness test can help. Common worldwide, especially near volcanic regions.