Rock Identifier
Rounded gray stone, likely basalt or andesite (Fine-grained mafic to intermediate volcanic rock; likely basalt (plagioclase ± pyroxene, possibly olivine)) — igneous
igneous

Rounded gray stone, likely basalt or andesite

Fine-grained mafic to intermediate volcanic rock; likely basalt (plagioclase ± pyroxene, possibly olivine)

AI-generated identification · may be incorrect

Dark gray, dull to slightly subvitreous, fine-grained and compact, with weathered lighter patches; hardness roughly 6–7 Mohs, no visible cleavage, and typically specific gravity 2.7–3.1.

Identified More igneous
Explore Rounded gray stone, likely basalt or andesite in the encyclopedia →

Identify your own rocks.

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

Physical properties

Dark gray, dull to slightly subvitreous, fine-grained and compact, with weathered lighter patches; hardness roughly 6–7 Mohs, no visible cleavage, and typically specific gravity 2.7–3.1.

Formation & geological history

Formed when lava cooled rapidly at or near Earth’s surface, commonly during the Cenozoic or older volcanic episodes; its rounded shape indicates transport and abrasion by water or sediment.

Uses & applications

Used as aggregate, roadstone, riprap, and occasionally building stone; ordinary specimens have little jewelry value.

Geological facts

Basalt is Earth’s most abundant volcanic rock and forms much of the oceanic crust. The image alone cannot reliably distinguish basalt from andesite or weathered fine-grained metamorphic rock.

Field identification & locations

Identify by its uniform fine texture, dark color, heavy feel, and lack of large crystals; a streak, magnet test, acid test, and thin section would improve identification. Common in volcanic regions, riverbeds, beaches, and glacial deposits.