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

Polished basalt cobble

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

AI-generated identification · may be incorrect

Typically dark gray to black, fine-grained, and dull to slightly vitreous; hardness about 5–6 Mohs, massive texture, no visible cleavage, and specific gravity approximately 2.8–3.0. The orange-brown patches are likely iron-oxide weathering or surface alteration.

Identified More igneous
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Physical properties

Typically dark gray to black, fine-grained, and dull to slightly vitreous; hardness about 5–6 Mohs, massive texture, no visible cleavage, and specific gravity approximately 2.8–3.0. The orange-brown patches are likely iron-oxide weathering or surface alteration.

Formation & geological history

Forms when basaltic lava rapidly cools at or near Earth’s surface, commonly in oceanic crust, volcanic islands, and continental lava flows. Most specimens are geologically young to Mesozoic or older, depending on locality.

Uses & applications

Used as crushed aggregate, road stone, riprap, railway ballast, paving, and dimension stone; polished cobbles are decorative or collectible but generally low value.

Geological facts

Basalt is the most abundant volcanic rock and makes up much of the ocean floor. Its fine texture reflects rapid cooling that prevented large crystals from forming.

Field identification & locations

Identify it by its heavy, uniformly fine-grained black appearance, magnetic response in some examples, and resistance to scratching by a steel knife. Common worldwide, especially near volcanic regions and stream gravels.