Rock Identifier
Black-and-white bicolored pebble (Likely basalt with a pale felsic or carbonate coating/inclusion; exact identification requires testing) — igneous
igneous

Black-and-white bicolored pebble

Likely basalt with a pale felsic or carbonate coating/inclusion; exact identification requires testing

AI-generated identification · may be incorrect

Dark gray, fine-grained, rounded and water-worn, with sparkly granular crystals; the white portion is matte and porous-looking. Estimated hardness is 5–7 for the dark material and possibly 3–6 for the white material; cleavage is not evident.

Identified More igneous
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Physical properties

Dark gray, fine-grained, rounded and water-worn, with sparkly granular crystals; the white portion is matte and porous-looking. Estimated hardness is 5–7 for the dark material and possibly 3–6 for the white material; cleavage is not evident.

Formation & geological history

Most likely a river or beach pebble formed from volcanic rock, with the white area representing attached calcite-rich material, weathered vein material, or a contrasting rock fragment. Its geological age cannot be determined visually.

Uses & applications

Primarily a landscaping, craft, or common specimen stone; it has little jewelry or industrial value unless testing reveals an unusual mineral or meteorite-like composition.

Geological facts

The rounded shape indicates prolonged abrasion by moving water or waves. A magnet, streak, acid, and specific-gravity tests would help distinguish basalt from other dark rocks and identify the white material.

Field identification & locations

Commonly found in stream gravels, beaches, and glacial deposits; basalt typically has tiny visible crystals, a dark streak, and may be weakly magnetic. The white area may fizz in dilute hydrochloric acid if it is calcite.