Rock Identifier
Milky Quartz Pebble (Crystalline Silicon Dioxide (SiO2)) — mineral
mineral

Milky Quartz Pebble

Crystalline Silicon Dioxide (SiO2)

Hardness: 7 (Mohs scale), Color: Opaque white to translucent milky, Luster: Vitreous to waxy when water-worn, Crystal Structure: Hexagonal (trigonal), Cleavage: None (conchoidal fracture), Specific Gravity: 2.65

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Physical properties

Hardness: 7 (Mohs scale), Color: Opaque white to translucent milky, Luster: Vitreous to waxy when water-worn, Crystal Structure: Hexagonal (trigonal), Cleavage: None (conchoidal fracture), Specific Gravity: 2.65

Formation & geological history

Formed from hydrothermal solutions or cooling magma where gas bubbles and fluid inclusions create the characteristic white opacity. This specific specimen has been rounded by fluvial or marine erosion.

Uses & applications

Used in glass making, electronics (piezoelectric properties), landscaping, abrasives, and as decorative river stones.

Geological facts

The milky white color is caused by tiny inclusions of gas or liquid trapped during the crystal's growth. It is the most common variety of crystalline quartz found on Earth's crust.

Field identification & locations

Identify in the field by its hardness (will scratch glass), lack of cleavage, and white sugary appearance. Commonly found in riverbeds, beaches, and glacial till worldwide.