
mineral
Milky Quartz
Crystalline Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: Milky white to translucent; Luster: Vitreous to greasy; Crystal Structure: Hexagonal (trigonal); Cleavage: Conchoidal fracture; Specific gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Milky white to translucent
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 on Mohs scale; Color: Milky white to translucent; Luster: Vitreous to greasy; Crystal Structure: Hexagonal (trigonal); Cleavage: Conchoidal fracture; Specific gravity: 2.65
Formation & geological history
Formed in hydrothermal veins and pegmatites through the cooling and crystallization of silica-rich solutions in the Earth's crust over millions of years.
Uses & applications
Used in glassmaking, abrasives, electronics (piezoelectric properties), and as decorative landscaping stone or pocket stones.
Geological facts
Milky quartz gets its white color from tiny fluid inclusions of gas or liquid trapped during crystal growth. It is the most common variety of crystalline quartz found on Earth.
Field identification & locations
Identified by its white color, inability to be scratched by a steel knife, and lack of cleavage. It is found globally in mountainous regions and riverbeds.
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Sandstone with Mineral Veining or Crust
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Potassium Feldspar (Orthoclase)
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