
mineral
Milky Quartz
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale. Color: Milky white to translucent. Luster: Vitreous (glass-like) to greasy. Crystal System: Trigonal/Hexagonal. Cleavage: None (conchoidal fracture). Specific Gravity: ~2.65.
- Hardness
- 7 on Mohs scale
- Color
- Milky white to translucent
- Luster
- Vitreous (glass-like) to greasy
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Physical properties
Hardness: 7 on Mohs scale. Color: Milky white to translucent. Luster: Vitreous (glass-like) to greasy. Crystal System: Trigonal/Hexagonal. Cleavage: None (conchoidal fracture). Specific Gravity: ~2.65.
Formation & geological history
Forms during the late stages of magmatic crystallization in pegmatites, hydrothermal veins, and metamorphic environments. The white cloudy appearance is caused by tiny gas and liquid bubble inclusions trapped during crystal growth.
Uses & applications
Used extensively in glass manufacturing, electronics (piezoelectric properties), abrasives, landscaping, quartz countertops, and as ornamental/lapidary specimens.
Geological facts
Milky quartz is the most common variety of crystalline quartz on Earth. The milky appearance is due to millions of microscopic fluid inclusions of gas, liquid, or petroleum trapped during its formation.
Field identification & locations
Identified by its white milky color, vitreous luster, hardness of 7 (scratches glass), and absence of cleavage with typical conchoidal fracturing. Found worldwide in quartz veins, pegmatites, and gravel deposits.
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