Milky Quartz
Silicon Dioxide (SiO2)
Rock Type: mineral

Physical Properties
Hardness: 7 (Mohs scale); Color: White, cloudy; Luster: Vitreous to greasy; Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65
Formation & Geological History
Formed through the cooling of magma or hydrothermal activity in veins. The cloudy appearance is caused by tiny inclusions of gas or liquid trapped during crystal growth. They are found across all geological eras.
Uses & Applications
Used in glassmaking, abrasives, and as a source of silicon for electronics. While cloudy specimens are less common in jewelry than clear quartz, they are widely used in landscaping and as decorative 'healing' crystals.
Geological Facts
Quartz is the second most abundant mineral in Earth's continental crust. Milky quartz specifically gets its white color from millions of microscopic fluid inclusions that scatter light.
Field Identification & Locations
Identified in the field by its hardness (will scratch glass), lack of cleavage, and white opaque color. It is ubiquitous in mountainous regions and riverbeds worldwide.
Identified on: 5/13/2026
Mode: Standard