
mineral
Milky Quartz
Quartz (Silicon Dioxide, SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale. Color: Translucent white to milky cloudy. Luster: Vitreous to greasy. Crystal structure: Trigonal/Hexagonal. Cleavage: None (conchoidal fracture). Specific gravity: ~2.65.
- Hardness
- 7 on Mohs scale
- Color
- Translucent white to milky cloudy
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 on Mohs scale. Color: Translucent white to milky cloudy. Luster: Vitreous to greasy. Crystal structure: Trigonal/Hexagonal. Cleavage: None (conchoidal fracture). Specific gravity: ~2.65.
Formation & geological history
Formed in various geological environments, including hydrothermal veins, pegmatites, igneous intrusive bodies, and sedimentary deposits, often rounded by water action into river or beach pebbles.
Uses & applications
Used in gemstone carvings, decorative landscaping, mineral collections, and historically as a silica source in glassmaking.
Geological facts
The milky or cloudy appearance of milky quartz is caused by tiny gas or fluid inclusions trapped inside the crystal lattice during its growth.
Field identification & locations
Can be identified by its ability to scratch glass (hardness 7), lack of cleavage, and translucent white color. Extensively found in riverbeds, gravel deposits, and pegmatite fields worldwide.
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