
mineral
Milky Quartz
Quartz (Silicon Dioxide, SiO2)
Hardness: 7 (Mohs scale); Color: White to cloudy translucent; Luster: Vitreous to greasy; Crystal Structure: Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 (Mohs scale)
- Color
- White to cloudy translucent
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 (Mohs scale); Color: White to cloudy translucent; Luster: Vitreous to greasy; Crystal Structure: Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Forms through the cooling of magma or hydrothermal activity in veins. The milky appearance is caused by tiny fluid or gas inclusions trapped during crystal growth.
Uses & applications
Used in jewelry (cabochons), as an abrasive, in glassmaking, and in metaphysical practices as a healing stone.
Geological facts
Milky Quartz is the most common variety of crystalline quartz. The white color is often referred to as 'snow quartz' and is caused by microscopic bubbles of liquid or gas.
Field identification & locations
Identified in the field by its hardness (scratches glass), lack of cleavage, and white cloudy appearance. Extremely common in pegmatites and gold-bearing hydrothermal veins.
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