Rock Identifier
Weathered basalt pebble (Basalt, a fine-grained mafic volcanic rock composed mainly of plagioclase, pyroxene, and commonly olivine or iron oxides) — igneous
igneous

Weathered basalt pebble

Basalt, a fine-grained mafic volcanic rock composed mainly of plagioclase, pyroxene, and commonly olivine or iron oxides

AI-generated identification · may be incorrect

Typically dark gray to brown, fine-grained, dull to subtly granular, with no visible cleavage; hardness about 5–6 Mohs and specific gravity roughly 2.8–3.0. The rounded shape and brown surface indicate abrasion and weathering, possibly with iron-oxide staining.

Identified More igneous
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Physical properties

Typically dark gray to brown, fine-grained, dull to subtly granular, with no visible cleavage; hardness about 5–6 Mohs and specific gravity roughly 2.8–3.0. The rounded shape and brown surface indicate abrasion and weathering, possibly with iron-oxide staining.

Formation & geological history

Formed when mafic lava cooled rapidly at or near Earth’s surface, commonly in oceanic crust, volcanic fields, and flood-basalt provinces; individual cooling ages range from recent to billions of years.

Uses & applications

Used as crushed aggregate, road stone, riprap, and sometimes architectural stone; this small, ordinary pebble has minimal jewelry or collector value.

Geological facts

Basalt is the most abundant volcanic rock and makes up much of the ocean floor. It may be weakly magnetic if it contains magnetite.

Field identification & locations

Identify it by its dark color, compact fine texture, heavy feel, and lack of obvious quartz or large crystals; a streak, magnet, and fresh-break examination would help confirm it. Common worldwide in volcanic and river environments.