
mineral
Milky Quartz
Silicon dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: White to cloudy translucent; Luster: Vitreous to greasy; Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- White to cloudy translucent
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 on Mohs scale; Color: White to cloudy translucent; Luster: Vitreous to greasy; Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed through the cooling of magma or precipitation from hydrothermal veins. The milky appearance is caused by tiny fluid or gas inclusions trapped during crystal growth.
Uses & applications
Used in glassmaking, jewelry (as semi-precious stones), gravel/construction, and as a source of silicon for electronics.
Geological facts
Milky quartz is the most common variety of crystalline quartz. While once ignored by many collectors, high-quality tumbled versions and those with unique inclusions are popular in metaphysical communities.
Field identification & locations
Identify by its hardness (will scratch glass), white cloudy appearance, and lack of cleavage. Commonly found in riverbeds, mountains, and as garden stones globally.
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Arenite (SiO2 based)
sedimentary
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Metamorphic
Epidote
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metamorphic
Gypsum (variety Selenite or Alabaster)
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Mineral
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Mineral/Rock
Granite
Granite (Phaneritic intrusive igneous rock)
igneous