Rock Identifier
Weathered basalt boulder (Basalt; fine-grained mafic volcanic rock, chiefly plagioclase and pyroxene with possible olivine) — igneous
igneous

Weathered basalt boulder

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

AI-generated identification · may be incorrect

Dark gray-brown, massive, fine-grained, and weakly lustrous from weathering; typical hardness is about Mohs 6, with no visible cleavage or large crystals. The rusty-brown rind likely represents oxidation and surface weathering.

Identified More igneous
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Physical properties

Dark gray-brown, massive, fine-grained, and weakly lustrous from weathering; typical hardness is about Mohs 6, with no visible cleavage or large crystals. The rusty-brown rind likely represents oxidation and surface weathering.

Formation & geological history

Formed when basaltic lava cooled rapidly at or near Earth’s surface, commonly during volcanic eruptions. Its exact age cannot be determined from the photograph; transport and prolonged weathering may have rounded the boulder.

Uses & applications

Used widely as crushed aggregate, road base, railway ballast, riprap, paving stone, and occasionally architectural facing; generally little jewelry value.

Geological facts

Basalt is the most abundant volcanic rock on oceanic crust and commonly forms lava flows, dikes, and ocean-floor pillow lavas.

Field identification & locations

Identify it by its heavy, dark, compact appearance, fine texture, and resistance to scratching; a steel file may scratch it only weakly, while it can scratch glass. Confirm with a fresh broken surface or thin section, since dark weathered rocks can also be andesite, diabase, or iron-rich sedimentary rock.