Rock Identifier
Tumbled dark stone, likely basalt (Basalt; chiefly plagioclase feldspar, pyroxene, and minor olivine or iron oxides) — igneous
igneous

Tumbled dark stone, likely basalt

Basalt; chiefly plagioclase feldspar, pyroxene, and minor olivine or iron oxides

AI-generated identification · may be incorrect

Fine-grained, dark gray to black, dull to faintly vitreous luster, typically massive with no visible cleavage; Mohs hardness about 6, specific gravity 2.8–3.0. The smooth shape indicates natural water wear or tumbling.

Identified More igneous
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Physical properties

Fine-grained, dark gray to black, dull to faintly vitreous luster, typically massive with no visible cleavage; Mohs hardness about 6, specific gravity 2.8–3.0. The smooth shape indicates natural water wear or tumbling.

Formation & geological history

Basalt forms when mafic lava rapidly cools at or near Earth’s surface, commonly in volcanic regions and oceanic crust. Individual formation ages vary from recent eruptions to billions of years old.

Uses & applications

Used as aggregate, road stone, riprap, paving, and sometimes decorative or metaphysical tumbled stone. Small pieces have modest collecting value.

Geological facts

Basalt is the most abundant volcanic rock on Earth and commonly forms extensive lava flows and ocean-floor crust.

Field identification & locations

Identify it by its uniformly dark, fine-grained appearance, heavy feel, and lack of large crystals; a streak, magnetism test, or close inspection may distinguish it from similar dark stones such as andesite or slate. Common worldwide, especially Hawaii, Iceland, India, and oceanic islands.