Rock Identifier
Tumbled dark stone, likely basalt (Basalt; fine-grained mafic volcanic rock, commonly composed of plagioclase, pyroxene, and minor olivine) — igneous
igneous

Tumbled dark stone, likely basalt

Basalt; fine-grained mafic volcanic rock, commonly composed of plagioclase, pyroxene, and minor olivine

AI-generated identification · may be incorrect

Appears smoothly tumbled, dark gray to black, with a dull to slightly vitreous luster and no visible crystals; typical basalt hardness is about 6–6.5 Mohs, with massive texture and no prominent cleavage.

Identified More igneous
Explore Tumbled dark stone, likely basalt in the encyclopedia →

Identify your own rocks.

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

Physical properties

Appears smoothly tumbled, dark gray to black, with a dull to slightly vitreous luster and no visible crystals; typical basalt hardness is about 6–6.5 Mohs, with massive texture and no prominent cleavage.

Formation & geological history

Basalt forms when low-silica lava cools rapidly at or near Earth’s surface, commonly during the Cenozoic or older volcanic episodes. The image alone cannot establish its exact age or locality.

Uses & applications

Used as aggregate, road stone, building stone, landscaping material, and decorative tumbled rock; common pieces generally have little jewelry value.

Geological facts

Its dark color reflects abundant iron- and magnesium-rich minerals. Similar-looking tumbled material may be gabbro, diabase, slag, or dark jasper, which cannot be distinguished confidently from this photograph.

Field identification & locations

Common worldwide in volcanic regions, including oceanic crust, Hawaii, Iceland, India, and the western United States; a fresh streak is usually gray, and basalt is opaque and lacks the glassy transparency of obsidian.