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

Likely basalt fragment

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

AI-generated identification · may be incorrect

Dark gray to black, dull to weakly vitreous, fine-grained and irregularly weathered; hardness about 5–6 Mohs, typically dense, with no visible cleavage or crystals at this scale.

Identified More igneous
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Physical properties

Dark gray to black, dull to weakly vitreous, fine-grained and irregularly weathered; hardness about 5–6 Mohs, typically dense, with no visible cleavage or crystals at this scale.

Formation & geological history

Formed when iron- and magnesium-rich lava cooled rapidly at or near Earth’s surface, commonly during volcanic eruptions; individual age cannot be determined from the image.

Uses & applications

Used as crushed aggregate, road base, riprap, building stone, and occasionally as a decorative or lapidary material; this small weathered piece has negligible commercial value.

Geological facts

Basalt is the most abundant volcanic rock on Earth and forms much of the oceanic crust, including large lava plateaus and seafloor pillow lavas.

Field identification & locations

The specimen’s dark color, fine texture, and dense appearance support basalt, but scale and lighting prevent certainty; test for a nonmetallic streak and compare density, while a magnet may respond weakly if iron-rich. Common localities include Hawaii, Iceland, oceanic islands, and continental volcanic regions.