Rock Identifier
Dark gray rock fragment, likely basalt (Basalt; fine-grained mafic volcanic rock composed mainly of plagioclase and pyroxene, commonly with olivine) — igneous
igneous

Dark gray rock fragment, likely basalt

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

AI-generated identification · may be incorrect

Hardness about 6 on the Mohs scale; dark gray to black, dull to faintly glassy, with a fine-grained interlocking crystal structure. Cleavage is not visible in the rock mass; density is typically 2.8–3.0 g/cm³.

Identified More igneous
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Physical properties

Hardness about 6 on the Mohs scale; dark gray to black, dull to faintly glassy, with a fine-grained interlocking crystal structure. Cleavage is not visible in the rock mass; density is typically 2.8–3.0 g/cm³.

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 recent eruptions to rocks billions of years old.

Uses & applications

Used as crushed aggregate, roadstone, railway ballast, riprap, and building stone; attractive polished pieces may be used decoratively. This small fragment has negligible commercial value.

Geological facts

The image shows a small angular, dark fragment with a fine texture consistent with basalt, though lighting and resolution prevent definitive identification. Similar-looking alternatives include andesite, dense slag, or dark sedimentary rock.

Field identification & locations

Identify basalt by its uniform fine grain, dark color, hardness, and lack of obvious layers or large crystals; a hand lens and streak/magnet tests can help distinguish it from slag. Common worldwide, especially in volcanic regions and oceanic crust.