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

Milky Quartz Pebble

Silicon Dioxide (SiO2)

Hardness: 7 on Mohs scale. Color: Translucent white to pale yellowish-cream. Luster: Vitreous to greasy. Crystal structure: Hexagonal (trigonal). Cleavage: None (conchoidal fracture). Specific gravity: 2.65.

Hardness
7 on Mohs scale
Color
Translucent white to pale yellowish-cream
Luster
Vitreous to greasy
Identified More mineral
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Physical properties

Hardness: 7 on Mohs scale. Color: Translucent white to pale yellowish-cream. Luster: Vitreous to greasy. Crystal structure: Hexagonal (trigonal). Cleavage: None (conchoidal fracture). Specific gravity: 2.65.

Formation & geological history

Formed in pegmatites, hydrothermal veins, and metamorphic rocks. This water-worn, smooth river pebble was tumbled naturally over time through alluvial action.

Uses & applications

Used widely in jewelry (cabochons, beads), decorative stone collections, landscaping, and industrially for silica production.

Geological facts

Milky quartz gets its cloudy appearance from tiny inclusions of gas or liquid trapped during crystal growth millions of years ago.

Field identification & locations

Identified by its ability to scratch glass (Mohs 7), lack of cleavage, and smooth rounded pebble morphology. Commonly found in riverbeds, gravel pits, and beaches worldwide.