
mineral
Milky Quartz
Silicon Dioxide (SiO2)
Hardness: 7 (Mohs scale); Color: translucent white to cloudy; Luster: vitreous (glassy) to greasy; Crystal structure: Trigonal (Hexagonal); Cleavage: Poor/None (conchoidal fracture); Specific gravity: 2.65.
- Hardness
- 7 (Mohs scale)
- Color
- translucent white to cloudy
- Luster
- vitreous (glassy) to greasy
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Physical properties
Hardness: 7 (Mohs scale); Color: translucent white to cloudy; Luster: vitreous (glassy) to greasy; Crystal structure: Trigonal (Hexagonal); Cleavage: Poor/None (conchoidal fracture); Specific gravity: 2.65.
Formation & geological history
Forms in hydrothermal veins, pegmatites, and as a primary constituent of igneous rocks like granite. The milky appearance is caused by tiny inclusions of gas or liquid trapped during crystal growth.
Uses & applications
Used in glass manufacturing, as an abrasive, and in electronics for its piezoelectric properties. In common forms, it is used for landscaping, construction aggregate, and as a gemstone for beads.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Milky quartz specifically is the most common variety of crystalline quartz.
Field identification & locations
Identify in the field by its hardness (scratches glass), lack of cleavage, and characteristic greasy luster on fracture surfaces. Found globally in almost all geological environments.
More like this
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
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