Rock Identifier
Likely tumbled dark igneous stone (Probably basalt or fine-grained gabbro; exact identification is uncertain from the blue-tinted photograph) — igneous
igneous

Likely tumbled dark igneous stone

Probably basalt or fine-grained gabbro; exact identification is uncertain from the blue-tinted photograph

AI-generated identification · may be incorrect

Small rounded specimen with black to dark gray color, subdued vitreous-to-dull luster, and irregular lighter gray internal patches or faces. Likely hardness about 5–6.5 Mohs, massive texture, no obvious cleavage, and specific gravity roughly 2.8–3.1.

Identified More igneous
Explore Likely tumbled dark igneous stone in the encyclopedia →

Identify your own rocks.

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

Physical properties

Small rounded specimen with black to dark gray color, subdued vitreous-to-dull luster, and irregular lighter gray internal patches or faces. Likely hardness about 5–6.5 Mohs, massive texture, no obvious cleavage, and specific gravity roughly 2.8–3.1.

Formation & geological history

Basalt forms when mafic lava cools rapidly at or near Earth’s surface; gabbro is its slower-cooled intrusive equivalent. These rocks are mostly geologically young in volcanic settings but can occur at any age.

Uses & applications

Commonly used as aggregate, road stone, ballast, and decorative gravel; polished pieces are inexpensive ornamental or teaching specimens.

Geological facts

The apparent blue cast is probably caused by the intense blue lighting or fabric reflection rather than the stone’s true color. Basalt commonly contains plagioclase, pyroxene, and sometimes olivine.

Field identification & locations

In neutral daylight, look for a dense black-gray body, very fine grains, and absence of visible quartz or strong layering; a streak test, magnet test, and specific-gravity measurement would help. Common worldwide in volcanic regions and oceanic crust.