
mineral
Milky Quartz
Quartz (Silicon Dioxide, SiO2)
Hardness: 7 on Mohs scale; Color: Cloudy white to opaque; Luster: Vitreous to greasy; Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Cloudy white to opaque
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 on Mohs scale; Color: Cloudy white to opaque; Luster: Vitreous to greasy; Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed from the cooling of silica-rich hydrothermal fluids or magma. Often found in igneous pegmatites or metamorphic vein deposits. Many specimens are hundreds of millions of years old.
Uses & applications
Used as an abrasive, in the manufacture of glass, ceramics, and electronics (as oscillators). Also popular as a decorative stone and for landscaping.
Geological facts
Milky quartz gets its cloudy appearance from minute fluid inclusions of gas and/or liquid trapped during crystal growth. It is the most common variety of crystalline quartz.
Field identification & locations
Identify by its hardness (it will scratch glass) and lack of cleavage planes. Found globally in riverbeds, mountains, and near mining sites.
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