Rock Identifier
Vesicular basalt (lava rock) (Basalt, a fine-grained mafic volcanic rock; chiefly plagioclase, pyroxene, and possibly olivine) — igneous
igneous

Vesicular basalt (lava rock)

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

AI-generated identification · may be incorrect

Dark gray, rough, and highly vesicular, with holes left by escaping gas; typically Mohs 5–6, dull to slightly glassy, and without visible cleavage. The specimen’s precise mineral makeup cannot be determined from the photo alone.

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Physical properties

Dark gray, rough, and highly vesicular, with holes left by escaping gas; typically Mohs 5–6, dull to slightly glassy, and without visible cleavage. The specimen’s precise mineral makeup cannot be determined from the photo alone.

Formation & geological history

Forms when gas-rich basaltic lava cools rapidly at or near the surface. Basalt is common throughout geologic time; this specimen’s age and locality are unknown.

Uses & applications

Basalt is widely used as crushed aggregate, road stone, and construction material; porous lava rock is also used in landscaping and grilling. This large, ordinary specimen has limited collector value.

Geological facts

The cavities are vesicles, not fossils; their presence records gas bubbles trapped in cooling lava.

Field identification & locations

Look for a dark, dense volcanic matrix with abundant rounded or elongated holes. Common in volcanic regions and lava fields; a photo alone cannot establish its exact locality or distinguish every vesicular volcanic rock.