Rock Identifier
White quartz pebble (Quartz (silicon dioxide, SiO₂), likely milky quartz or quartz-rich vein material) — mineral
mineral

White quartz pebble

Quartz (silicon dioxide, SiO₂), likely milky quartz or quartz-rich vein material

AI-generated identification · may be incorrect

Hardness 7 Mohs; white to cream, translucent to opaque, with a vitreous-to-waxy luster and no obvious cleavage. The smooth rounded shape indicates water or abrasion wear; specific gravity is about 2.65.

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Physical properties

Hardness 7 Mohs; white to cream, translucent to opaque, with a vitreous-to-waxy luster and no obvious cleavage. The smooth rounded shape indicates water or abrasion wear; specific gravity is about 2.65.

Formation & geological history

Formed when silica-rich fluids crystallized in veins or igneous rocks, commonly during Precambrian to younger geological events, then weathered and rounded in sediment or beach environments.

Uses & applications

Common quartz is used in glass, ceramics, abrasives, electronics, and engineered stone; this small rounded piece has little jewelry or industrial value.

Geological facts

Milky color results from microscopic fluid inclusions, fractures, or impurities that scatter light. Quartz is one of Earth’s most abundant and durable minerals.

Field identification & locations

Identify by its glassy appearance, lack of cleavage, and inability to be scratched by a steel knife; it should scratch ordinary glass. Common worldwide in riverbeds, beaches, and quartz veins.