Rock Identifier
Rounded basalt pebble (Basalt; fine-grained mafic volcanic rock composed mainly of plagioclase and pyroxene, commonly with olivine) — igneous
igneous

Rounded basalt pebble

Basalt; fine-grained mafic volcanic rock composed mainly of plagioclase and pyroxene, commonly with olivine

AI-generated identification · may be incorrect

Dark brown to gray-black, dense, fine-grained, and mostly dull to subtly waxy from weathering; hardness about 5–6 Mohs, no visible cleavage, and specific gravity roughly 2.8–3.0. Its smooth shape indicates prolonged water or sediment abrasion.

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Physical properties

Dark brown to gray-black, dense, fine-grained, and mostly dull to subtly waxy from weathering; hardness about 5–6 Mohs, no visible cleavage, and specific gravity roughly 2.8–3.0. Its smooth shape indicates prolonged water or sediment abrasion.

Formation & geological history

Basalt forms when iron- and magnesium-rich lava cools rapidly at or near Earth’s surface, commonly in oceanic crust, volcanic fields, and flood-basalt provinces. The specimen’s exact age and source cannot be determined from the photograph.

Uses & applications

Used as crushed aggregate, road base, railway ballast, riprap, and building stone; attractive polished pieces are sold as landscape or decorative specimens. This rounded pebble has little jewelry value.

Geological facts

The brown surface likely reflects oxidation of iron-bearing minerals. A magnet may show weak attraction if the basalt contains magnetite.

Field identification & locations

Common along volcanic shorelines, rivers draining volcanic terrain, and glacial deposits. Confirm with a fresh break: basalt should be compact, fine-grained, dark, and heavier than many ordinary sedimentary pebbles; avoid confusing it with slag or dark chert.