Rock Identifier
Likely basalt (Basalt; chiefly plagioclase feldspar, pyroxene, and often olivine) — igneous
igneous

Likely basalt

Basalt; chiefly plagioclase feldspar, pyroxene, and often olivine

AI-generated identification · may be incorrect

Dark gray-black, fine-grained to subtly crystalline, with dull to weakly glassy luster; Mohs hardness about 6, no obvious cleavage, and typical specific gravity 2.8–3.0. The image suggests a dense, irregular, possibly vesicle-poor specimen.

Identified More igneous
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Physical properties

Dark gray-black, fine-grained to subtly crystalline, with dull to weakly glassy luster; Mohs hardness about 6, no obvious cleavage, and typical specific gravity 2.8–3.0. The image suggests a dense, irregular, possibly vesicle-poor specimen.

Formation & geological history

An extrusive mafic igneous rock formed when iron- and magnesium-rich lava rapidly cooled at or near Earth’s surface; specimens may range from recent volcanic material to Precambrian flows billions of years old.

Uses & applications

Widely used as crushed aggregate, road metal, railway ballast, riprap, and occasionally building stone; attractive polished pieces are used decoratively but have limited gemstone value.

Geological facts

Basalt is the most abundant volcanic rock on Earth and forms much of the oceanic crust, especially at mid-ocean ridges and hotspots.

Field identification & locations

Identify by its uniformly dark color, fine texture, high density, and lack of visible large crystals; common worldwide in volcanic regions, including Hawaii, Iceland, India, and the Pacific Northwest. A field test cannot exclude closely similar rocks such as diabase or andesite.