Rock Identifier
Dark rounded pebble, likely basalt (Basalt (fine-grained mafic volcanic rock; commonly plagioclase, pyroxene, and olivine)) — igneous
igneous

Dark rounded pebble, likely basalt

Basalt (fine-grained mafic volcanic rock; commonly plagioclase, pyroxene, and olivine)

AI-generated identification · may be incorrect

Dark gray-green, smooth and rounded from abrasion, with a dull to faintly subvitreous luster and tiny pale mineral grains. Typical basalt hardness is about Mohs 6, with no obvious cleavage and specific gravity around 2.8–3.0.

Identified More igneous
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Physical properties

Dark gray-green, smooth and rounded from abrasion, with a dull to faintly subvitreous luster and tiny pale mineral grains. Typical basalt hardness is about Mohs 6, with no obvious cleavage and specific gravity around 2.8–3.0.

Formation & geological history

Basalt forms when iron- and magnesium-rich lava cools rapidly at or near Earth’s surface, commonly in volcanic fields and oceanic crust. Its exact age cannot be determined from the photograph; the pebble may have been transported and naturally polished by water or ice.

Uses & applications

Used as crushed aggregate, roadstone, riprap, paving stone, and occasionally decorative landscaping material. This ordinary pebble has little commercial or collector value.

Geological facts

The specimen’s rounded shape indicates mechanical weathering and transport, while its dark color suggests mafic composition. Similar-looking rocks can include greenstone, diabase, or dark metamorphic rocks.

Field identification & locations

Look for a dense, fine-grained texture, dark color, lack of visible large crystals, and weak magnetism in some specimens. Common in volcanic regions, river gravels, beaches, and glacial deposits.