Rock Identifier
Possible basalt pebble (Basalt; fine-grained mafic volcanic rock, chiefly plagioclase and pyroxene) — igneous
igneous

Possible basalt pebble

Basalt; fine-grained mafic volcanic rock, chiefly plagioclase and pyroxene

AI-generated identification · may be incorrect

Dark gray-green, rounded and apparently weathered, with a dull to faintly granular luster and tiny pale mineral grains. Typically hardness 5–6 Mohs, massive with no cleavage, and specific gravity about 2.8–3.0; the image alone cannot confirm composition.

Identified More igneous
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Physical properties

Dark gray-green, rounded and apparently weathered, with a dull to faintly granular luster and tiny pale mineral grains. Typically hardness 5–6 Mohs, massive with no cleavage, and specific gravity about 2.8–3.0; the image alone cannot confirm composition.

Formation & geological history

Basalt forms when iron- and magnesium-rich lava rapidly cools at or near Earth’s surface, commonly in oceanic crust, lava flows, and volcanic islands. Most specimens are geologically young relative to continental rocks, though basalt occurs from Archean to present.

Uses & applications

Used as crushed aggregate, road stone, riprap, and occasionally building or landscaping stone; ordinary pebbles have little jewelry value.

Geological facts

Its rounded shape indicates transport and abrasion, likely in a river, beach, or glacial deposit. The small bright flecks may be feldspar, pyroxene, or weathering minerals.

Field identification & locations

Test for a dark streak, high density, and lack of visible layering; a steel file may scratch it, while it should not fizz with dilute hydrochloric acid. Common worldwide, especially volcanic regions and river gravels.