Rock Identifier
Likely vesicular basalt (scoria-like pebble) (Basalt; predominantly plagioclase, pyroxene, and possibly olivine) — igneous
igneous

Likely vesicular basalt (scoria-like pebble)

Basalt; predominantly plagioclase, pyroxene, and possibly olivine

AI-generated identification · may be incorrect

Dark reddish-brown, fine-grained, dull to slightly earthy luster, with numerous small gas vesicles; hardness about 5–6 Mohs, no obvious cleavage, and typically specific gravity around 2.7–3.0 (lower if highly vesicular).

Identified More igneous
Explore Likely vesicular basalt (scoria-like pebble) in the encyclopedia →

Identify your own rocks.

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

Physical properties

Dark reddish-brown, fine-grained, dull to slightly earthy luster, with numerous small gas vesicles; hardness about 5–6 Mohs, no obvious cleavage, and typically specific gravity around 2.7–3.0 (lower if highly vesicular).

Formation & geological history

An extrusive volcanic rock formed when fluid basaltic lava cooled rapidly, trapping bubbles; commonly Cenozoic to recent, though basalt occurs throughout geological time.

Uses & applications

Used as aggregate, roadstone, landscaping rock, and occasionally as a decorative or lapidary material; ordinary pebbles have little commercial value.

Geological facts

The reddish coloration usually reflects oxidation of iron-bearing minerals. Its pores distinguish it from most dense basalt and may indicate scoria if the specimen is notably lightweight.

Field identification & locations

Identify it by its dark mafic color, fine texture, iron staining, and vesicles; common in volcanic regions, lava flows, and beaches derived from basalt. The image alone cannot exclude weathered scoria or another vesicular volcanic rock.