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

Dark volcanic rock, likely basalt

Basalt; chiefly plagioclase feldspar, pyroxene, and commonly olivine

AI-generated identification · may be incorrect

Fine-grained, dark gray to black, dull to slightly vitreous luster; typically massive with no visible cleavage. Mohs hardness about 5–6 and specific gravity about 2.8–3.0; the specimen may also be scoria if its apparent pores are genuine.

Identified More igneous
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Physical properties

Fine-grained, dark gray to black, dull to slightly vitreous luster; typically massive with no visible cleavage. Mohs hardness about 5–6 and specific gravity about 2.8–3.0; the specimen may also be scoria if its apparent pores are genuine.

Formation & geological history

An extrusive igneous rock formed when mafic lava cooled rapidly at or near Earth’s surface, commonly during Cenozoic or older volcanic eruptions. Exact age cannot be determined from the photograph.

Uses & applications

Used extensively as crushed aggregate, road base, railway ballast, riprap, and building stone; attractive polished basalt is used decoratively. Common pieces have little collector value.

Geological facts

Basalt is the most abundant volcanic rock on Earth and forms much of the oceanic crust. Its dark color reflects abundant iron- and magnesium-rich minerals.

Field identification & locations

Identify it by its uniform dark color, fine texture, and substantial weight; a streak test is usually gray, and a magnet may show weak attraction if iron minerals are present. Common worldwide in volcanic regions and oceanic settings.