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

Rounded basalt pebble

Basalt, a fine-grained mafic volcanic rock composed mainly of plagioclase feldspar and pyroxene, with possible olivine

AI-generated identification · may be incorrect

Dark gray-green, dull to weakly granular, and smoothly water-worn; typically Mohs hardness 5–6, dense, with very fine crystals and no obvious cleavage. The image is insufficient to confirm exact mineralogy.

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Physical properties

Dark gray-green, dull to weakly granular, and smoothly water-worn; typically Mohs hardness 5–6, dense, with very fine crystals and no obvious cleavage. The image is insufficient to confirm exact mineralogy.

Formation & geological history

Formed when mafic lava cooled rapidly at or near Earth’s surface, commonly during the Cenozoic or older volcanic episodes; its rounded shape indicates stream, beach, or glacial transport.

Uses & applications

Used as crushed aggregate, road base, riprap, railroad ballast, and occasionally decorative stone; this small pebble has negligible commercial value.

Geological facts

Basalt is the most abundant volcanic rock on oceanic crust and commonly forms seafloor lava flows, including pillow basalts.

Field identification & locations

Look for a dark, heavy, fine-grained rock that does not fizz with dilute acid and may show tiny vesicles or scattered olivine grains. Common worldwide in volcanic terrains and alluvial gravels.