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

Quartz Pebble (Milky Quartz)

Silicon Dioxide (SiO2)

Hardness: 7 (Mohs scale), Color: Translucent white to milky white with minor iron staining, Luster: Vitreous to waxy (when water-worn), Crystal Structure: Trigonal/Hexagonal, Cleavage: None (conchoidal fracture), Specific Gravity: 2.65

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Physical properties

Hardness: 7 (Mohs scale), Color: Translucent white to milky white with minor iron staining, Luster: Vitreous to waxy (when water-worn), Crystal Structure: Trigonal/Hexagonal, Cleavage: None (conchoidal fracture), Specific Gravity: 2.65

Formation & geological history

Formed from silica-rich hydrothermal fluids cooling in veins/fissures within igneous or metamorphic rock. This specific specimen has been weathered and rounded through coastal erosion and wave action (beach pebble).

Uses & applications

Used in glass manufacturing, as an abrasive, in landscaping/decor, as a tumbled gemstone, and historically in flint-knapping.

Geological facts

Milky quartz gets its cloudy appearance from tiny inclusions of gas or liquid trapped during crystal growth. It is the most common variety of crystalline quartz found on Earth's surface.

Field identification & locations

Identify in the field by its hardness (will scratch glass), translucent appearance, and lack of cleavage planes. Found globally on tectonic beaches and riverbeds.