
mineral
Milky Quartz
Silicon Dioxide (SiO2)
Hardness: 7.0 on Mohs scale; Color: Milky white to opaque; Luster: Vitreous to greasy; Crystal Structure: Trigonal (often found as massive vein quartz); Cleavage: None (conchoidal fracture).
- Hardness
- 7
- Color
- Milky white to opaque
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7.0 on Mohs scale; Color: Milky white to opaque; Luster: Vitreous to greasy; Crystal Structure: Trigonal (often found as massive vein quartz); Cleavage: None (conchoidal fracture).
Formation & geological history
Forms through the crystallization of silica-rich hydrothermal fluids in veins or pegmatites. It is incredibly common and forms across nearly all geological ages in igneous, metamorphic, and sedimentary environments.
Uses & applications
Used in glass making, as an abrasive, in the production of silicon metal for electronics, and widely as garden landscaping or interior decorative stones.
Geological facts
The 'milky' appearance is caused by tiny inclusions of gas and/or liquid trapped during the crystal's growth. It is one of the most abundant minerals on Earth's surface.
Field identification & locations
Identify in the field by its hardness (it will scratch glass), its white translucent color, and its lack of cleavage. It is found globally in mountain ranges, riverbeds, and as vein outcroppings.
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Other mineral specimens
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Schist
Schist
Metamorphic
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Gypsum (variety Selenite or Alabaster)
Calcium sulfate dihydrate (CaSO4·2H2O)
Mineral
Nephrite Jade
Nephrite
Mineral/Rock
Granite
Granite (Phaneritic intrusive igneous rock)
igneous