Rock Identifier
Tumbled brown-and-black stone, likely basalt or andesite (Fine-grained mafic to intermediate volcanic rock; commonly plagioclase, pyroxene, and possibly olivine or iron oxides) — igneous
igneous

Tumbled brown-and-black stone, likely basalt or andesite

Fine-grained mafic to intermediate volcanic rock; commonly plagioclase, pyroxene, and possibly olivine or iron oxides

AI-generated identification · may be incorrect

Dark gray-brown, mottled, and weakly lustrous with a fine-grained texture; estimated Mohs hardness 5–6.5, no visible cleavage, and likely specific gravity about 2.7–3.1.

Identified More igneous
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Physical properties

Dark gray-brown, mottled, and weakly lustrous with a fine-grained texture; estimated Mohs hardness 5–6.5, no visible cleavage, and likely specific gravity about 2.7–3.1.

Formation & geological history

Likely formed from cooling lava, probably in the Cenozoic or older; subsequent weathering and tumbling produced the smooth rounded shape. Exact identification requires a fresh surface, streak, and mineralogical testing.

Uses & applications

Used as aggregate, road stone, landscaping material, and occasionally as a decorative tumbled stone; usually has little jewelry value.

Geological facts

The rusty brown areas likely reflect oxidation of iron-bearing minerals. Basalt and andesite can look similar in hand-sized, polished specimens.

Field identification & locations

Common in volcanic regions worldwide, including oceanic islands, western North America, Iceland, India, and Japan. A magnetism test, close inspection of grain size, and specific-gravity measurement can help distinguish basalt from andesite.