Rock Identifier
Polished basalt pebble (Basalt; primarily plagioclase feldspar, pyroxene, and commonly olivine or iron oxides) — igneous
igneous

Polished basalt pebble

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

AI-generated identification · may be incorrect

Hardness about 6–7 Mohs; dark brown to black, fine-grained, and commonly dull to glassy when polished. It has an interlocking microscopic crystal structure, no visible cleavage, and specific gravity roughly 2.8–3.1.

Identified More igneous
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Physical properties

Hardness about 6–7 Mohs; dark brown to black, fine-grained, and commonly dull to glassy when polished. It has an interlocking microscopic crystal structure, no visible cleavage, and specific gravity roughly 2.8–3.1.

Formation & geological history

Basalt is an extrusive igneous rock formed when low-viscosity mafic lava cools rapidly at or near Earth’s surface, commonly during volcanic eruptions; its age depends on locality and may range from recent to billions of years.

Uses & applications

Used as aggregate, road stone, paving, building stone, and occasionally as a polished ornamental or worry stone; this shaped specimen is primarily decorative or collectible.

Geological facts

The rounded form and glossy surface indicate natural water abrasion followed by polishing or tumbling. Small pale or metallic-looking patches may represent altered minerals, vesicle fillings, or weathering products.

Field identification & locations

Identify it by its heavy feel, dark fine-grained appearance, lack of obvious large crystals, and resistance to scratching by steel; basalt commonly occurs in volcanic regions, river gravels, and oceanic crust.