Rock Identifier
Basalt cobble (Basalt; predominantly plagioclase feldspar, pyroxene, and commonly olivine) — igneous
igneous

Basalt cobble

Basalt; predominantly plagioclase feldspar, pyroxene, and commonly olivine

AI-generated identification · may be incorrect

Dark gray-black, fine-grained, massive, and dull to slightly vitreous; Mohs hardness about 6, with no visible cleavage and typical specific gravity of 2.8–3.0. The rounded, smooth surface indicates prolonged water or sediment abrasion, possibly with minor weathering or a thin coating.

Identified More igneous
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Physical properties

Dark gray-black, fine-grained, massive, and dull to slightly vitreous; Mohs hardness about 6, with no visible cleavage and typical specific gravity of 2.8–3.0. The rounded, smooth surface indicates prolonged water or sediment abrasion, possibly with minor weathering or a thin coating.

Formation & geological history

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

Uses & applications

Used as aggregate, road ballast, riprap, paving stone, and occasionally as a landscaping or ornamental stone; generally has low collector value.

Geological facts

Basalt is the most widespread volcanic rock on Earth and forms much of the oceanic crust. A strong magnet may attract it weakly if it contains abundant magnetite.

Field identification & locations

Identify it by its uniformly dark color, fine texture, substantial weight, and lack of layering or large crystals; a streak test is usually gray-black, and acid produces no reaction. Common worldwide in volcanic regions, river gravels, and beaches.