Rock Identifier
Tumbled basalt pebble (Basalt (fine-grained mafic volcanic rock; commonly plagioclase, pyroxene, and iron-titanium oxides)) — igneous
igneous

Tumbled basalt pebble

Basalt (fine-grained mafic volcanic rock; commonly plagioclase, pyroxene, and iron-titanium oxides)

AI-generated identification · may be incorrect

Dark gray-black with rusty yellow-brown weathering or iron-oxide staining; fine-grained, massive texture, dull to faintly vitreous luster, and no visible cleavage. Hardness is roughly 5–6 Mohs; specific gravity about 2.8–3.0.

Identified More igneous
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Physical properties

Dark gray-black with rusty yellow-brown weathering or iron-oxide staining; fine-grained, massive texture, dull to faintly vitreous luster, and no visible cleavage. Hardness is roughly 5–6 Mohs; specific gravity about 2.8–3.0.

Formation & geological history

Basalt forms when mafic lava rapidly cools at or near Earth’s surface, ranging from ancient Precambrian flows to modern volcanic eruptions. Its rounded shape indicates abrasion in a stream, beach, or tumbling process.

Uses & applications

Used as crushed aggregate, road stone, riprap, railway ballast, and landscaping material; attractive polished pieces are inexpensive collectibles.

Geological facts

The ochre patches likely represent oxidation of iron-bearing minerals during weathering, not necessarily a separate mineral species.

Field identification & locations

Identify it by its heavy feel, dark fine-grained appearance, lack of large crystals, and inability to scratch glass consistently; common worldwide in volcanic terrains and river gravels.