
mineral
White Quartz (Milky Quartz)
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: Milky white to translucent; 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 translucent
- Luster
- Vitreous (glassy) to greasy
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Physical properties
Hardness: 7 on Mohs scale; Color: Milky white to translucent; Luster: Vitreous (glassy) to greasy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Forms in igneous, metamorphic, and sedimentary environments through hydrothermal activity and the cooling of silica-rich magma or hot fluids in veins and geodes. It can be found across all geological ages.
Uses & applications
Used in glassmaking, as an abrasive in sandblasting, in the manufacturing of semiconductors, jewelry (cabochons and beads), and widely as a decorative stone in landscaping and home decor.
Geological facts
Milky quartz gets its cloudy appearance from minute fluid inclusions of gas or liquid trapped during the crystal's growth. It is the most common variety of crystalline quartz found on Earth.
Field identification & locations
Identify in the field by its hardness (it will scratch glass), lack of cleavage, and characteristic milky white opacity. It is commonly found in gravel pits, riverbeds, and as veins in mountain ranges worldwide.
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