Rock Identifier
Weathered basalt or andesite cobble (Fine-grained mafic to intermediate volcanic rock; commonly plagioclase ± pyroxene, amphibole, and iron oxides) — igneous
igneous

Weathered basalt or andesite cobble

Fine-grained mafic to intermediate volcanic rock; commonly plagioclase ± pyroxene, amphibole, and iron oxides

AI-generated identification · may be incorrect

Dark gray-green, dull to slightly waxy surface with rounded weathering; likely hardness 5–6, no obvious cleavage, fine-grained crystalline texture, and specific gravity about 2.7–3.0. The pale brown areas appear to be weathered rind or adhered sediment rather than a distinct mineral.

Identified More igneous
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Physical properties

Dark gray-green, dull to slightly waxy surface with rounded weathering; likely hardness 5–6, no obvious cleavage, fine-grained crystalline texture, and specific gravity about 2.7–3.0. The pale brown areas appear to be weathered rind or adhered sediment rather than a distinct mineral.

Formation & geological history

Formed when lava cooled relatively quickly at or near Earth’s surface, then became rounded by transport and weathering. Its precise age and identity cannot be determined from the photograph alone.

Uses & applications

Commonly used as aggregate, riprap, road stone, landscaping material, and occasionally carving stone; this ordinary cobble has little commercial or jewelry value.

Geological facts

Basalt is the most widespread volcanic rock on oceanic crust, while andesite is common in volcanic arcs. Weathering can produce brown iron-oxide coatings and soften the outer surface.

Field identification & locations

Test a fresh edge for a fine-grained texture, streakless dark gray interior, and lack of visible quartz; basalt is usually slightly magnetic, whereas andesite may be weakly magnetic. Common worldwide in volcanic regions and stream gravels.