Rock Identifier
Basalt cobble (Basalt; fine-grained mafic volcanic rock, chiefly plagioclase and clinopyroxene with possible olivine and magnetite) — igneous
igneous

Basalt cobble

Basalt; fine-grained mafic volcanic rock, chiefly plagioclase and clinopyroxene with possible olivine and magnetite

AI-generated identification · may be incorrect

Dark gray-black, dense, dull to faintly vitreous, and fine-grained; likely Mohs 5–6, with no visible cleavage or large crystals. The rounded, weathered surface may reflect water transport or human tumbling.

Identified More igneous
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Physical properties

Dark gray-black, dense, dull to faintly vitreous, and fine-grained; likely Mohs 5–6, with no visible cleavage or large crystals. The rounded, weathered surface may reflect water transport or human tumbling.

Formation & geological history

Forms when iron- and magnesium-rich lava cools rapidly at or near Earth’s surface, commonly in volcanic flows and oceanic crust. Basalt ranges from Archean to Recent in age and is still forming today.

Uses & applications

Used as crushed aggregate, road stone, riprap, paving, and dimension stone; attractive polished pieces are sold as decorative specimens. Typical value is about $2–$20 for a common cobble, or $20–$75 if unusually shaped or polished.

Geological facts

Its dark color and high density distinguish it from most granite and sandstone. Some basalt contains vesicles, but this specimen appears notably massive and non-vesicular.

Field identification & locations

Common worldwide, especially in volcanic regions, oceanic islands, flood-basalt provinces, and river gravels. Confirm with a fresh edge: it should show a dark fine-grained interior, resist scratching by a steel knife, and often attract a weak magnet if magnetite-rich.