Rock Identifier
Likely tumbled basalt or dark volcanic rock (Basalt; chiefly plagioclase feldspar, pyroxene, and commonly olivine or iron oxides) — igneous
igneous

Likely tumbled basalt or dark volcanic rock

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

AI-generated identification · may be incorrect

Dark gray-black, fine-grained, subvitreous to dull luster, rounded by tumbling or water; hardness about 5–6 Mohs, no visible cleavage, and typically dense (specific gravity ~2.8–3.0). The image is too small to confirm mineral grains or texture.

Identified More igneous
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Physical properties

Dark gray-black, fine-grained, subvitreous to dull luster, rounded by tumbling or water; hardness about 5–6 Mohs, no visible cleavage, and typically dense (specific gravity ~2.8–3.0). The image is too small to confirm mineral grains or texture.

Formation & geological history

Basalt forms when low-silica basaltic lava rapidly cools at or near Earth’s surface, commonly in volcanic regions and oceanic crust; specimens may range from recent eruptions to billions of years old. Its rounded shape suggests natural abrasion or human tumbling.

Uses & applications

Used as crushed aggregate, road stone, railway ballast, dimension stone, and occasionally in landscaping or jewelry as an inexpensive polished stone. Collector value is generally low.

Geological facts

Basalt is the most abundant volcanic rock and makes up much of the ocean floor. Vesicles, magnetic response, or tiny pale feldspar crystals can help distinguish it from other dark stones.

Field identification & locations

Common worldwide, especially Hawaii, Iceland, the Deccan Traps, and oceanic volcanic terrains; test for a weak magnet, dense feel, and fine texture. Estimated value: $1–$10 for a small common tumbled piece; unusual textures or provenance may reach $20–$50.