Rock Identifier
Weathered gray rock, likely basalt or andesite (Fine-grained mafic to intermediate volcanic rock; likely basalt (plagioclase ± pyroxene, possibly altered)) — igneous
igneous

Weathered gray rock, likely basalt or andesite

Fine-grained mafic to intermediate volcanic rock; likely basalt (plagioclase ± pyroxene, possibly altered)

AI-generated identification · may be incorrect

Dark gray, dull to weakly submetallic surface with pronounced weathering and cavities; likely hardness 5–6, massive fine-grained texture, and specific gravity about 2.7–3.0. The apparent layered lines may be surface fractures or adhered weathered material rather than true foliation.

Identified More igneous
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Physical properties

Dark gray, dull to weakly submetallic surface with pronounced weathering and cavities; likely hardness 5–6, massive fine-grained texture, and specific gravity about 2.7–3.0. The apparent layered lines may be surface fractures or adhered weathered material rather than true foliation.

Formation & geological history

Formed when lava cooled at or near Earth’s surface, generally during the Cenozoic or older depending on locality; the specimen has subsequently undergone oxidation, abrasion, and chemical weathering.

Uses & applications

Common basalt and andesite are used as crushed aggregate, roadstone, riprap, and occasionally building stone; this heavily weathered piece has mainly educational or decorative value.

Geological facts

Volcanic rocks can develop vesicles that later fill with secondary minerals, producing pits and irregular textures like those visible here.

Field identification & locations

Identify basalt by its dark color, fine grain, lack of visible quartz, and high density; a hand lens and streak, hardness, and magnetism tests would help distinguish basalt from andesite or altered industrial slag. Common worldwide in volcanic regions.