Rock Identifier
Vesicular basalt (possibly scoriaceous basalt) (Vesicular basalt; chiefly plagioclase, pyroxene, and iron-rich oxides) — igneous
igneous

Vesicular basalt (possibly scoriaceous basalt)

Vesicular basalt; chiefly plagioclase, pyroxene, and iron-rich oxides

AI-generated identification · may be incorrect

Dark purplish-brown, fine-grained volcanic rock with rounded gas-bubble cavities (vesicles); typically Mohs 5–6, dull to slightly vitreous, with no obvious cleavage. The image alone cannot establish its exact composition or whether the cavities are natural.

Identified More igneous →
Explore Vesicular basalt (possibly scoriaceous basalt) in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Dark purplish-brown, fine-grained volcanic rock with rounded gas-bubble cavities (vesicles); typically Mohs 5–6, dull to slightly vitreous, with no obvious cleavage. The image alone cannot establish its exact composition or whether the cavities are natural.

Formation & geological history

Forms when basaltic lava cools quickly while trapped gas escapes, leaving vesicles; commonly associated with relatively recent volcanic flows, though a specimen’s age cannot be determined from appearance.

Uses & applications

Used as decorative stone, landscaping material, and occasionally lightweight aggregate; porous specimens are also collected.

Geological facts

Vesicles are the frozen remnants of gas bubbles in lava; mineral-filled cavities are called amygdales.

Field identification & locations

Look for a dense, dark volcanic groundmass containing scattered rounded holes; distinguish it from industrial slag by geological context and consistent natural texture. Basalt occurs worldwide in volcanic regions.