Rock Identifier
Dark river-worn stone, likely basalt (Basalt; fine-grained mafic volcanic rock, chiefly plagioclase and pyroxene) — igneous
igneous

Dark river-worn stone, likely basalt

Basalt; fine-grained mafic volcanic rock, chiefly plagioclase and pyroxene

AI-generated identification · may be incorrect

Gray-green to charcoal, dull to weakly subvitreous luster, massive and fine-grained with no visible crystals; Mohs hardness about 5–6 and typically no cleavage. The rounded shape indicates water abrasion.

Identified More igneous
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Physical properties

Gray-green to charcoal, dull to weakly subvitreous luster, massive and fine-grained with no visible crystals; Mohs hardness about 5–6 and typically no cleavage. The rounded shape indicates water abrasion.

Formation & geological history

Basalt forms when mafic lava rapidly cools at or near Earth’s surface, commonly in oceanic crust, flood-basalt provinces, and volcanic islands; its age may range from recent to billions of years. The image alone cannot establish its exact age or locality.

Uses & applications

Used as crushed aggregate, road stone, riprap, paving, and occasionally decorative stone; ordinary pieces have little jewelry value.

Geological facts

Basalt is the most abundant volcanic rock and commonly contains iron- and magnesium-rich minerals, giving it a dark color. Some varieties develop vesicles or green alteration minerals, but none are clearly visible here.

Field identification & locations

Confirm with a fresh surface, strong streak-free hardness, and lack of reaction to dilute acid; a magnet may show weak attraction. Commonly found in volcanic terrains and streambeds; exact identification could also include andesite or altered basalt.