Rock Identifier
Likely tumbled basalt (Basalt, a fine-grained mafic volcanic rock; commonly composed of plagioclase, pyroxene, and minor olivine) — igneous
igneous

Likely tumbled basalt

Basalt, a fine-grained mafic volcanic rock; commonly composed of plagioclase, pyroxene, and minor olivine

AI-generated identification · may be incorrect

Dark gray to black, fine-grained, with a wet vitreous-to-dull luster; typically massive and non-cleaved. Mohs hardness is about 5–6, and specific gravity is approximately 2.8–3.0; the image’s rounded, polished shape suggests tumbling or water wear.

Identified More igneous
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Physical properties

Dark gray to black, fine-grained, with a wet vitreous-to-dull luster; typically massive and non-cleaved. Mohs hardness is about 5–6, and specific gravity is approximately 2.8–3.0; the image’s rounded, polished shape suggests tumbling or water wear.

Formation & geological history

Basalt forms when iron- and magnesium-rich lava rapidly cools at or near Earth’s surface, commonly in oceanic crust, volcanic islands, and continental lava flows. Specimen age cannot be determined from the image and may range from recent to billions of years.

Uses & applications

Used as crushed aggregate, road stone, building stone, and basalt fiber; attractive polished pieces are used for décor and inexpensive lapidary items.

Geological facts

Often weakly magnetic if it contains magnetite. Vesicles, tiny pale plagioclase crystals, or green olivine may occur, though none are clearly visible here.

Field identification & locations

Identify by its uniformly dark fine texture, high density, and lack of obvious layering or large crystals; distinguish it from slate by its massive texture and from glass by its granular surface. Common worldwide, especially volcanic regions and river gravels.