Rock Identifier
Weathered vesicular basalt (probable) (Basalt; primarily plagioclase, pyroxene, and often olivine) — igneous
igneous

Weathered vesicular basalt (probable)

Basalt; primarily plagioclase, pyroxene, and often olivine

AI-generated identification · may be incorrect

Dark gray to rusty brown, fine-grained, rough, and locally vesicular with weathering cavities; typically dull to weakly lustered. Hardness about 5–6 Mohs, no obvious cleavage, and specific gravity roughly 2.8–3.0.

Identified More igneous
Explore Weathered vesicular basalt (probable) in the encyclopedia →

Identify your own rocks.

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

Physical properties

Dark gray to rusty brown, fine-grained, rough, and locally vesicular with weathering cavities; typically dull to weakly lustered. Hardness about 5–6 Mohs, no obvious cleavage, and specific gravity roughly 2.8–3.0.

Formation & geological history

An extrusive volcanic rock formed when mafic lava cooled rapidly at or near the surface, likely during the Cenozoic or younger, though the image cannot establish age. The brown coloration and cavities reflect oxidation and weathering.

Uses & applications

Used as crushed aggregate, road stone, riprap, building stone, and occasionally as landscaping or lapidary material; this weathered specimen has limited jewelry value.

Geological facts

Its holes may be vesicles formed by gas bubbles in lava; some cavities can later be filled with zeolite, calcite, or quartz. The irregular surface is consistent with substantial chemical weathering.

Field identification & locations

Common in volcanic regions worldwide, including Hawaii, Iceland, the Pacific Northwest, India, and oceanic crust. Confirm with a fresh broken surface, dark fine grain, hardness near window glass, and lack of strong acid reaction; a magnet may show weak attraction if iron-rich.