
mineral
Milky Quartz
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: White to translucent with tan/brown iron staining; Luster: Vitreous to greasy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- White to translucent with tan/brown iron staining
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 on Mohs scale; Color: White to translucent with tan/brown iron staining; Luster: Vitreous to greasy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Forms from the cooling of silica-rich hydrothermal veins or within igneous pegmatites. It can be found in rocks from virtually all geological periods.
Uses & applications
Used in glass making, as an abrasive, in the electronics industry for its piezoelectric properties, and as a common landscape or decorative stone.
Geological facts
The cloudy white appearance is caused by tiny inclusions of gas or liquid trapped during the crystal's initial formation. Is the most common variety of crystalline quartz.
Field identification & locations
Identify by its hardness (scratches glass), waxy/glassy luster, and lack of cleavage. Very common in gravel pits, beaches, and mountain outcrops globally.
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Arenite (SiO2 based)
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Mineral/Rock
Banded Gneiss (River Rock/Pebble)
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