
mineral
Milky Quartz
Quartz (Silicon Dioxide, SiO2)
Hardness: 7 on the Mohs scale. Color: White to milky white, often with minor inclusions. Luster: Vitreous to greasy. Crystal Structure: Trigonal. Cleavage: None, exhibits conchoidal fracture. Specific Gravity: 2.65.
- Hardness
- 7 on the Mohs scale
- Color
- White to milky white, often with minor inclusions
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 on the Mohs scale. Color: White to milky white, often with minor inclusions. Luster: Vitreous to greasy. Crystal Structure: Trigonal. Cleavage: None, exhibits conchoidal fracture. Specific Gravity: 2.65.
Formation & geological history
Forms in hydrothermal veins, pegmatites, and igneous, metamorphic, and sedimentary rocks as water-rich fluids cool and precipitate silica over millions of years.
Uses & applications
Used in gemstone collection, decorative items, lapidary work, and sometimes as a minor source of silicon for industrial applications.
Geological facts
Milky quartz is the most common variety of crystalline quartz found on Earth. Its cloudy appearance is caused by microscopic fluid or gas inclusions trapped during crystal growth.
Field identification & locations
Easily identified by its high hardness (scratches glass), white color, conchoidal fracture, and lack of cleavage. Found worldwide in almost all geological environments.
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