Rock Identifier
Likely basalt (Basalt; fine-grained mafic volcanic rock, typically rich in plagioclase, pyroxene, and olivine) — igneous
igneous

Likely basalt

Basalt; fine-grained mafic volcanic rock, typically rich in plagioclase, pyroxene, and olivine

AI-generated identification · may be incorrect

Dark gray to black, dense, and fine-grained with a dull to slightly vitreous luster; hardness about 5–6 Mohs, no obvious cleavage, and specific gravity roughly 2.8–3.0. The granular sparkle may reflect tiny crystals or a weathered surface.

Identified More igneous
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Physical properties

Dark gray to black, dense, and fine-grained with a dull to slightly vitreous luster; hardness about 5–6 Mohs, no obvious cleavage, and specific gravity roughly 2.8–3.0. The granular sparkle may reflect tiny crystals or a weathered surface.

Formation & geological history

Forms when basaltic lava cools rapidly at or near Earth’s surface, commonly in oceanic crust, volcanic fields, and lava flows; specimens may range from recent to Precambrian in age. The photograph alone cannot establish a precise locality or age.

Uses & applications

Used extensively as crushed aggregate, road base, railway ballast, building stone, and occasionally as architectural facing or decorative cobbles. Ordinary hand specimens generally have minimal collector value.

Geological facts

Basalt is Earth’s most abundant volcanic rock and commonly forms the ocean floor. It may be confused with gabbro, which has visibly larger crystals, or slag, which is often vesicular and unusually lightweight.

Field identification & locations

Identify it by its black, compact, heavy appearance and tiny interlocking crystals; a streak test is usually gray, and it commonly does not react with dilute acid. Common localities include Hawaii, Iceland, the Deccan Traps, oceanic islands, and volcanic regions worldwide.