mineral
Milky Quartz
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: Milky white to translucent; Luster: Vitreous to greasy; Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Milky white to translucent
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 on Mohs scale; Color: Milky white to translucent; Luster: Vitreous to greasy; Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Forms during the cooling of hydrothermal veins and pegmatites. It is the most common variety of crystalline quartz and is found in almost all geological environments worldwide.
Uses & applications
Used as a source of silica for glass manufacturing, as an abrasive, in electronics (piezoelectric properties), and widely as an ornamental stone or decorative gravel.
Geological facts
The milky appearance is caused by tiny inclusions of gas or liquid trapped during crystal growth. It is the most common mineral in Earth's continental crust.
Field identification & locations
Identify by its hardness (it will easily scratch glass), its white color, and its lack of cleavage. Look for it in quartz veins, gravel pits, and mountain ranges.
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Other mineral specimens
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Sandstone with Mineral Veining or Crust
Sedimentary Sandstone (mostly SiO2 with Fe2O3 tinting)
sedimentary
Schist
Schist
Metamorphic
Gypsum (variety Selenite or Alabaster)
Calcium sulfate dihydrate (CaSO4·2H2O)
Mineral
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Nephrite Jade
Nephrite
Mineral/Rock