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

Likely basalt

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 faintly glassy, compact and fine-grained; typically Mohs 5–6, with no visible cleavage and irregular fracture. The surface appears weathered, so exact identification from the image is approximate.

Identified More igneous
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Physical properties

Dark gray to black, dull to faintly glassy, compact and fine-grained; typically Mohs 5–6, with no visible cleavage and irregular fracture. The surface appears weathered, so exact identification from the image is approximate.

Formation & geological history

Formed when iron- and magnesium-rich lava cooled rapidly at or near Earth’s surface, commonly during Cenozoic or older volcanic events. It is widespread in oceanic crust, lava flows, and volcanic provinces.

Uses & applications

Used as crushed aggregate, road base, riprap, concrete aggregate, and building stone; attractive polished pieces may be sold as decorative specimens. This small unexceptional piece has minimal commercial value.

Geological facts

Basalt is the most abundant volcanic rock and forms much of Earth’s oceanic crust. Vesicles, tiny crystals, or magnetic response are common diagnostic clues, though none are clearly visible here.

Field identification & locations

Look for a uniformly dark, heavy, fine-grained texture and possible attraction to a strong magnet; a hand lens may reveal tiny pale plagioclase crystals. Common localities include Hawaii, Iceland, India’s Deccan Traps, and ocean-floor volcanic regions.