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

Dark mafic rock, likely basalt

Basalt; primarily plagioclase feldspar, pyroxene, and commonly olivine or iron oxides

AI-generated identification · may be incorrect

Fine-grained, dark gray to brown, dull to weakly vitreous luster; hardness about 5–6, generally massive with no obvious cleavage. The image is insufficient to confirm texture or density.

Identified More igneous
Explore Dark mafic rock, likely basalt in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Fine-grained, dark gray to brown, dull to weakly vitreous luster; hardness about 5–6, generally massive with no obvious cleavage. The image is insufficient to confirm texture or density.

Formation & geological history

Extrusive igneous rock formed when mafic lava cooled rapidly at or near Earth’s surface, commonly during the Cenozoic or older volcanic episodes.

Uses & applications

Used as crushed aggregate, road base, railroad ballast, building stone, and occasionally decorative material; ordinary pieces have little jewelry value.

Geological facts

Basalt is the most abundant volcanic rock on Earth and forms much of the oceanic crust, including seafloor and many volcanic islands.

Field identification & locations

Identify by its dark color, heavy feel, fine texture, and lack of visible large crystals; magnetic response may occur from iron oxides. Common worldwide in volcanic regions and oceanic crust.