Rock Identifier
Rounded basalt pebble (Basalt; fine-grained mafic volcanic rock, typically plagioclase + clinopyroxene ± olivine and magnetite) — igneous
igneous

Rounded basalt pebble

Basalt; fine-grained mafic volcanic rock, typically plagioclase + clinopyroxene ± olivine and magnetite

AI-generated identification · may be incorrect

Hardness about 6–6.5 Mohs; dark brown to black, weathered/rust-stained surface, dull to faintly silky luster, very fine-grained massive texture, no visible cleavage. The smooth shape indicates water tumbling or abrasion.

Identified More igneous
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Physical properties

Hardness about 6–6.5 Mohs; dark brown to black, weathered/rust-stained surface, dull to faintly silky luster, very fine-grained massive texture, no visible cleavage. The smooth shape indicates water tumbling or abrasion.

Formation & geological history

Basalt forms when iron- and magnesium-rich lava rapidly cools at or near Earth’s surface, commonly in oceanic crust, volcanic fields, and flood-basalt provinces. Its exact geological age cannot be determined from the photograph; weathering produced the brown coating.

Uses & applications

Used as crushed aggregate, road base, riprap, ballast, and dimension stone; attractive polished pieces are collected or used decoratively. This small common pebble has minimal commercial value.

Geological facts

Magnetite may cause weak magnetism, and iron oxidation commonly produces the brown coloration. A streak, density, and thin-section examination would be needed for confident identification.

Field identification & locations

Look for a dense, dark, fine-grained rock with tiny scattered crystals, irregular fracture, and no layering or strong foliation; a steel file generally scratches it only with difficulty. Common in volcanic regions and stream or beach gravels worldwide.