Rock Identifier
Rounded gray river pebble, likely basaltic/volcanic rock (Probable basalt or andesite; exact identification requires a fresh surface and tests) — igneous
igneous

Rounded gray river pebble, likely basaltic/volcanic rock

Probable basalt or andesite; exact identification requires a fresh surface and tests

AI-generated identification · may be incorrect

Dark gray, fine-grained, dull to slightly waxy luster, rounded by abrasion, with possible small vesicles or weathered mineral grains. Typical hardness is about 5–6 Mohs; no obvious cleavage; specific gravity roughly 2.7–3.0.

Identified More igneous
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Physical properties

Dark gray, fine-grained, dull to slightly waxy luster, rounded by abrasion, with possible small vesicles or weathered mineral grains. Typical hardness is about 5–6 Mohs; no obvious cleavage; specific gravity roughly 2.7–3.0.

Formation & geological history

Likely formed when mafic to intermediate lava cooled rapidly at or near Earth’s surface, then became rounded in a stream or shoreline. Basaltic rocks range from Precambrian to modern, so age cannot be determined visually.

Uses & applications

Commonly used as aggregate, road stone, landscaping rock, riprap, and occasionally for small carvings or polished specimens; this ordinary pebble has little commercial value.

Geological facts

Its smooth shape records prolonged transport and repeated impact in moving water or surf. A magnet test may show weak attraction if the rock contains magnetite.

Field identification & locations

Look for a uniformly fine texture, dark gray color, high density, and possible tiny holes; basalt is usually darker and denser than andesite. Common in volcanic regions and gravel beds worldwide; a streak, magnet, hardness, and thin-section test would improve identification.