Rock Identifier
Likely weathered basalt or andesite fragment (Fine-grained mafic to intermediate volcanic rock; commonly plagioclase ± pyroxene ± olivine) — igneous
igneous

Likely weathered basalt or andesite fragment

Fine-grained mafic to intermediate volcanic rock; commonly plagioclase ± pyroxene ± olivine

AI-generated identification · may be incorrect

Dark brown-black, dull to faintly earthy luster, massive and fine-grained with irregular fracture; estimated Mohs hardness 5–6 and specific gravity about 2.7–3.1. The image is low-resolution, so vesicles, crystals, and exact mineralogy are not discernible.

Identified More igneous
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Physical properties

Dark brown-black, dull to faintly earthy luster, massive and fine-grained with irregular fracture; estimated Mohs hardness 5–6 and specific gravity about 2.7–3.1. The image is low-resolution, so vesicles, crystals, and exact mineralogy are not discernible.

Formation & geological history

Formed when lava cooled relatively quickly at or near Earth’s surface, producing microscopic crystals; its precise age and volcanic source cannot be determined from the photograph.

Uses & applications

Typically used as crushed aggregate, roadstone, riprap, and occasionally dimension stone; an ordinary fragment generally has negligible jewelry or collector value.

Geological facts

Basalt is the most abundant volcanic rock in oceanic crust, while andesite commonly forms at volcanic arcs above subduction zones. Brown coloration likely reflects surface weathering and iron oxidation.

Field identification & locations

Look for a dense, dark, fine-grained texture, hardness sufficient to scratch glass, and possible tiny plagioclase crystals or vesicles; magnetism can support a basalt identification. Common worldwide in volcanic terrains.