
mineral
Milky Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale. Color: White, grayish-white, to opaque milky appearance. Luster: Vitreous to greasy. Crystal System: Trigonal. Cleavage: None (conchoidal fracture).
- Hardness
- 7 on Mohs scale
- Color
- White, grayish-white, to opaque milky appearance
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 on Mohs scale. Color: White, grayish-white, to opaque milky appearance. Luster: Vitreous to greasy. Crystal System: Trigonal. Cleavage: None (conchoidal fracture).
Formation & geological history
Forms in igneous, metamorphic, and sedimentary environments, frequently occurring in hydrothermal veins and pegmatites where fluid inclusions (gas or liquid bubbles trapped during crystallization) cause the distinctive milky opacity.
Uses & applications
Used in glassmaking, ceramics, electronics (as a source of silicon), abrasives, landscaping, and gemstone carving or lapidary collection.
Geological facts
Milky quartz is one of the most common quartz varieties on Earth. Its cloudy white appearance is due to millions of microscopic fluid inclusions trapped during the mineral's growth.
Field identification & locations
Identify by its hardness (scratches glass, cannot be scratched by steel), glassy to waxy luster, lack of cleavage, and translucent to opaque white color. Found globally in stream beds, gravel pits, veins, and rocky outcrops.
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