Rock Identifier
Likely basalt (Basalt, a fine-grained mafic volcanic rock composed mainly of plagioclase feldspar, pyroxene, and commonly olivine) — igneous
igneous

Likely basalt

Basalt, a fine-grained mafic volcanic rock composed mainly of plagioclase feldspar, pyroxene, and commonly olivine

AI-generated identification · may be incorrect

Dark gray to black, fine-grained, dull to weakly vitreous, with massive texture and no obvious cleavage; hardness about 5–6 Mohs and specific gravity roughly 2.8–3.0. The specimen may also be a fine-grained metamorphic mafic rock, such as metabasalt, but the image is insufficient for certainty.

Identified More igneous
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Physical properties

Dark gray to black, fine-grained, dull to weakly vitreous, with massive texture and no obvious cleavage; hardness about 5–6 Mohs and specific gravity roughly 2.8–3.0. The specimen may also be a fine-grained metamorphic mafic rock, such as metabasalt, but the image is insufficient for certainty.

Formation & geological history

Basalt forms when iron- and magnesium-rich lava rapidly cools at or near Earth’s surface, commonly in oceanic crust, lava flows, and volcanic islands. It ranges from ancient Precambrian rocks to modern eruptions.

Uses & applications

Used widely as crushed aggregate, roadstone, railroad ballast, riprap, building stone, and basalt fiber; attractive polished pieces may be sold as decorative stone.

Geological facts

Basalt is Earth’s most abundant volcanic rock and makes up much of the ocean floor. Vesicles, magnetic response, or tiny visible olivine crystals can help distinguish it from similar dark rocks.

Field identification & locations

Identify it by its black-gray color, dense fine grain, lack of obvious layering, and occasional weak attraction to a magnet; a streak test is usually gray. Common locations include Hawaii, Iceland, oceanic islands, and continental volcanic provinces.