Rock Identifier
Vesicular basalt (likely weathered lava rock) (Basalt; fine-grained mafic volcanic rock composed chiefly of plagioclase, pyroxene, and commonly olivine) — igneous
igneous

Vesicular basalt (likely weathered lava rock)

Basalt; fine-grained mafic volcanic rock composed chiefly of plagioclase, pyroxene, and commonly olivine

AI-generated identification · may be incorrect

Dark gray to black, dull to weakly glassy, with irregular vesicles and weathered cavities; hardness about 5–6 Mohs, no visible cleavage, fine-grained interlocking crystal structure, and specific gravity roughly 2.8–3.0.

Identified More igneous
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Physical properties

Dark gray to black, dull to weakly glassy, with irregular vesicles and weathered cavities; hardness about 5–6 Mohs, no visible cleavage, fine-grained interlocking crystal structure, and specific gravity roughly 2.8–3.0.

Formation & geological history

Forms when basaltic lava cools rapidly at or near Earth’s surface, trapping gas bubbles; specimens may range from modern flows to Precambrian volcanic rocks, depending on locality.

Uses & applications

Used as crushed aggregate, roadstone, riprap, ballast, and landscaping rock; attractive polished pieces are occasionally collected but are rarely used as gemstones.

Geological facts

The rounded shape and surface cavities suggest abrasion and weathering, possibly from a lava flow, beach, or river environment. A magnet may attract it weakly if it contains abundant magnetite.

Field identification & locations

Identify it by its dark color, fine texture, vesicles, and absence of sedimentary layering; distinguish it from slag by its natural mineral texture and lack of metallic glassy flow features. Common worldwide in volcanic regions, including Hawaii, Iceland, India, and the Pacific Northwest.