Rock Identifier
Dark mafic rock, likely basalt (Basalt; primarily plagioclase feldspar, pyroxene, and commonly olivine) — igneous
igneous

Dark mafic rock, likely basalt

Basalt; primarily plagioclase feldspar, pyroxene, and commonly olivine

AI-generated identification · may be incorrect

Fine-grained, dark gray to black, dull to weakly vitreous luster; hardness about 5–6, no obvious cleavage, and typically dense (specific gravity ~2.8–3.0). The image suggests a weathered, vesicle-poor fragment, though exact identification requires testing.

Identified More igneous
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Physical properties

Fine-grained, dark gray to black, dull to weakly vitreous luster; hardness about 5–6, no obvious cleavage, and typically dense (specific gravity ~2.8–3.0). The image suggests a weathered, vesicle-poor fragment, though exact identification requires testing.

Formation & geological history

An extrusive igneous rock formed when iron- and magnesium-rich lava cooled rapidly at or near Earth’s surface, commonly in volcanic flows and oceanic crust. Basalt ranges from recent volcanic material to rocks hundreds of millions or billions of years old.

Uses & applications

Used as crushed aggregate, road base, railroad ballast, riprap, building stone, and basalt fiber; attractive polished pieces may be collected but usually have low gem value.

Geological facts

Basalt is the most widespread volcanic rock and forms much of the ocean floor. Magnetic basalt may contain magnetite and can weakly attract a magnet.

Field identification & locations

Look for a uniformly dark, heavy, fine-grained texture; a streak is usually gray, and a fresh break is dark and crystalline. Common worldwide, especially Hawaii, Iceland, oceanic islands, and volcanic provinces.