Rock Identifier
Milky quartz pebble (Quartz (SiO₂)) — mineral
mineral

Milky quartz pebble

Quartz (SiO₂)

AI-generated identification · may be incorrect

Mohs hardness 7; white to translucent with a vitreous-to-waxy luster and irregular fracture. Quartz has a trigonal crystal structure and no cleavage; this small specimen appears naturally rounded, possibly water-worn.

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Physical properties

Mohs hardness 7; white to translucent with a vitreous-to-waxy luster and irregular fracture. Quartz has a trigonal crystal structure and no cleavage; this small specimen appears naturally rounded, possibly water-worn.

Formation & geological history

Quartz commonly forms when silica-rich fluids crystallize in veins or cavities and is highly resistant to weathering, so fragments accumulate in streambeds and soils. Its age cannot be determined from the image; quartz occurs in rocks of nearly all geological ages.

Uses & applications

Quartz is used in glassmaking, electronics, abrasives, and decorative objects; this small pebble is mainly suitable for collecting or crafts.

Geological facts

Quartz is one of Earth’s most abundant minerals and ranks 7 on the Mohs scale.

Field identification & locations

Look for its glassy appearance, lack of cleavage, and ability to scratch ordinary glass; common worldwide in veins, beaches, and river gravels. The pictured piece is too small and visually nonspecific for a precise locality identification.