Rock Identifier
Rounded gray river pebble, likely basalt or andesite (Fine-grained mafic to intermediate volcanic rock; exact identification requires testing) — igneous
igneous

Rounded gray river pebble, likely basalt or andesite

Fine-grained mafic to intermediate volcanic rock; exact identification requires testing

AI-generated identification · may be incorrect

Dark gray-brown, smooth and water-worn, dull to weakly vitreous luster, with no visible crystals or cleavage; likely Mohs hardness about 5–6 and specific gravity roughly 2.7–3.0.

Identified More igneous
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Physical properties

Dark gray-brown, smooth and water-worn, dull to weakly vitreous luster, with no visible crystals or cleavage; likely Mohs hardness about 5–6 and specific gravity roughly 2.7–3.0.

Formation & geological history

Probably formed from rapidly cooled volcanic lava, then eroded and rounded in a stream, beach, or glacial environment. Its precise geological age cannot be determined from the photograph.

Uses & applications

Common material for landscaping, decorative pebble collections, aquarium substrates, and aggregate; generally little commercial or jewelry value.

Geological facts

The pale spot may be a weathered mineral grain, abrasion mark, or surface coating rather than a distinctive mineral. Basalt is typically magnetic to some degree because it commonly contains magnetite.

Field identification & locations

Look for a uniformly fine-grained dark interior, lack of layering, and possible attraction to a magnet; a streak, hardness, density, and fresh fracture would distinguish basalt from andesite, chert, or slag. Common worldwide in volcanic regions and river deposits.