
mineral
Milky Quartz
Quartz (Silicon Dioxide, SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Milky white to opaque; Luster: Vitreous (glassy) to greasy; Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Milky white to opaque
- Luster
- Vitreous (glassy) to greasy
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Physical properties
Hardness: 7 on Mohs scale; Color: Milky white to opaque; Luster: Vitreous (glassy) to greasy; Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65
Formation & geological history
Formed through the crystallization of silica-rich hydrothermal solutions or cooling magma in veins. The white 'milky' color is caused by microscopic inclusions of fluids or gas trapped during crystal growth.
Uses & applications
Used in glass manufacturing, as an abrasive, in electronics (due to piezoelectric properties), construction material, and as a semi-precious gemstone in jewelry and decor.
Geological facts
Milky quartz is the most common variety of crystalline quartz. It can often be found associated with precious metals like gold in hydrothermal vein deposits.
Field identification & locations
Identify by its ability to scratch glass, its lack of cleavage, and its distinctive white, cloudy appearance. It is found globally in almost all geological environments.
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