Rock Identifier
Rounded volcanic pebble, likely andesite or basalt (Fine-grained andesite–basalt; chiefly plagioclase feldspar and pyroxene, with possible iron oxides) — igneous
igneous

Rounded volcanic pebble, likely andesite or basalt

Fine-grained andesite–basalt; chiefly plagioclase feldspar and pyroxene, with possible iron oxides

AI-generated identification · may be incorrect

Gray to pinkish-gray, fine-grained and massive, with dull to slightly satin luster and no visible cleavage; estimated Mohs hardness 5–6. Its smooth, rounded shape reflects abrasion in water or sediment.

Identified More igneous →
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Physical properties

Gray to pinkish-gray, fine-grained and massive, with dull to slightly satin luster and no visible cleavage; estimated Mohs hardness 5–6. Its smooth, rounded shape reflects abrasion in water or sediment.

Formation & geological history

An extrusive igneous rock formed when lava cooled rapidly at or near Earth’s surface, generally during a volcanic episode of uncertain age; later transported and rounded in a stream, beach, or glacial environment.

Uses & applications

Common material for aggregate, road stone, landscaping, and decorative pebbles; this ordinary specimen has little jewelry value.

Geological facts

The pink tones may reflect oxidized iron or minor feldspar, while dark patches may be mafic minerals, weathering, or inclusions. Exact identification requires a fresh surface, streak, density, and thin-section or chemical analysis.

Field identification & locations

Look for a very fine crystalline texture, substantial weight, and lack of fizz with dilute acid; basalt is usually darker and denser, whereas andesite is commonly lighter gray. Volcanic pebbles occur widely in stream gravels and coastal deposits.