Rock Identifier
Gray volcanic rock, likely basalt (Basalt; primarily plagioclase feldspar, pyroxene, and minor olivine/iron oxides) — igneous
igneous

Gray volcanic rock, likely basalt

Basalt; primarily plagioclase feldspar, pyroxene, and minor olivine/iron oxides

AI-generated identification · may be incorrect

Fine-grained, dark gray, dull to slightly earthy luster, with no obvious large crystals; hardness about 6 on Mohs scale, massive texture, and typically specific gravity 2.8–3.0. The rough, rounded piece may show weathering or a thin vesicular/altered surface.

Identified More igneous
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Physical properties

Fine-grained, dark gray, dull to slightly earthy luster, with no obvious large crystals; hardness about 6 on Mohs scale, massive texture, and typically specific gravity 2.8–3.0. The rough, rounded piece may show weathering or a thin vesicular/altered surface.

Formation & geological history

Basalt forms when low-silica mafic lava cools rapidly at or near Earth’s surface, commonly in volcanic flows and oceanic crust. Most examples range from recent eruptions to rocks hundreds of millions of years old.

Uses & applications

Used as crushed aggregate, road base, railway ballast, building stone, and occasionally polished architectural material; ordinary hand specimens have little jewelry value.

Geological facts

Basalt is the most common volcanic rock and makes up much of the ocean floor. It commonly contains microscopic crystals, so its composition is usually identified by color, density, and geological context rather than visible grains.

Field identification & locations

Look for a dense, dark-gray to black rock with a fine texture that scratches glass but not steel easily; it may be weakly magnetic. Common localities include Hawaii, Iceland, the Deccan Traps, the Columbia River Basalt Group, and oceanic islands.