Rock Identifier
Rounded basalt pebble (Basalt, a fine-grained mafic volcanic rock composed mainly of plagioclase feldspar, pyroxene, and commonly olivine) — igneous
igneous

Rounded basalt pebble

Basalt, a fine-grained mafic volcanic rock composed mainly of plagioclase feldspar, pyroxene, and commonly olivine

AI-generated identification · may be incorrect

Dark gray, fine-grained, dull to faintly subvitreous, with no visible crystals; hardness about 6 Mohs, massive texture, poor or absent cleavage, and specific gravity around 2.8–3.0.

Identified More igneous
Explore Rounded basalt pebble in the encyclopedia →

Identify your own rocks.

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

Physical properties

Dark gray, fine-grained, dull to faintly subvitreous, with no visible crystals; hardness about 6 Mohs, massive texture, poor or absent cleavage, and specific gravity around 2.8–3.0.

Formation & geological history

Formed when iron- and magnesium-rich lava cooled rapidly at or near Earth’s surface, commonly during Cenozoic or older volcanic activity; the smooth shape reflects stream or beach abrasion.

Uses & applications

Used as crushed aggregate, road base, railway ballast, riprap, and dimension stone; rounded specimens are inexpensive geological or landscaping collectibles.

Geological facts

Basalt is the most abundant volcanic rock on oceanic crust and commonly forms lava flows, volcanic islands, and ocean-floor seafloor spreading zones.

Field identification & locations

Identify it by its uniform dark color, fine texture, high density, and lack of layering; a streak test is usually gray, and it should not fizz with dilute hydrochloric acid. Common worldwide near volcanic terrain and river gravels.