Rock Identifier
Rounded gray pebble, likely basalt or andesite (Fine-grained mafic to intermediate volcanic rock; commonly basalt (plagioclase ± pyroxene/olivine)) — igneous
igneous

Rounded gray pebble, likely basalt or andesite

Fine-grained mafic to intermediate volcanic rock; commonly basalt (plagioclase ± pyroxene/olivine)

AI-generated identification · may be incorrect

Dark gray-green, dull to weakly silky, fine-grained and massive, with no obvious cleavage; estimated Mohs hardness 5–6 and specific gravity about 2.7–3.1. Its smooth, rounded shape reflects water or beach abrasion rather than crystal form.

Identified More igneous →
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Physical properties

Dark gray-green, dull to weakly silky, fine-grained and massive, with no obvious cleavage; estimated Mohs hardness 5–6 and specific gravity about 2.7–3.1. Its smooth, rounded shape reflects water or beach abrasion rather than crystal form.

Formation & geological history

Likely formed when lava cooled rapidly at or near Earth’s surface, then weathered into a cobble; volcanic rocks range from ancient to recent, so age cannot be determined visually. The exact identification is uncertain without a fresh surface or testing.

Uses & applications

Used as landscaping gravel, aggregate, road material, and occasionally as a decorative or lapidary stone; this ordinary pebble has little jewelry value.

Geological facts

Basalt is the most abundant volcanic rock on oceanic crust and commonly contains microscopic crystals that require a hand lens to see.

Field identification & locations

Identify it by its uniform fine texture, dark gray color, lack of visible layering, and inability to scratch glass easily; a streak, magnetism test, or thin section can distinguish basalt from andesite and other stones. Common in volcanic terrains, riverbeds, beaches, and imported landscaping gravel.