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

Dark volcanic rock, likely basalt

Basalt; predominantly plagioclase feldspar and pyroxene, commonly with minor olivine and magnetite

AI-generated identification · may be incorrect

Appears dark gray-brown, massive, fine-grained, and dull to weakly vitreous, with irregular weathering and no obvious cleavage. Typical hardness is about 6 Mohs and specific gravity about 2.8–3.0; the surface may be weathered or coated, reducing diagnostic reliability.

Identified More igneous
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Physical properties

Appears dark gray-brown, massive, fine-grained, and dull to weakly vitreous, with irregular weathering and no obvious cleavage. Typical hardness is about 6 Mohs and specific gravity about 2.8–3.0; the surface may be weathered or coated, reducing diagnostic reliability.

Formation & geological history

Basalt forms when mafic lava rapidly cools at or near Earth’s surface, commonly in volcanic flows, oceanic crust, and flood-basalt provinces. Its exact age cannot be determined from the photograph; basalt ranges from ancient Archean rocks to modern eruptions.

Uses & applications

Crushed basalt is widely used for road aggregate, concrete, rail ballast, and rock wool; attractive dense pieces may be collected or used decoratively, but this specimen is not visibly gem-grade.

Geological facts

The rounded shape may result from water transport or weathering rather than original volcanic form. A fresh broken surface would reveal its characteristic fine crystalline texture.

Field identification & locations

Common worldwide, including oceanic islands, mid-ocean ridges, India’s Deccan Traps, Iceland, and the western United States. Confirm with a fresh surface, streak (usually gray), magnetism from iron oxides, and absence of fizz with dilute acid.