
mineral
Cloudy Quartz (Milky Quartz)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: White to pale grey-blue, translucent; Luster: Vitreous to waxy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- White to pale grey-blue, translucent
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 7 on Mohs scale; Color: White to pale grey-blue, translucent; Luster: Vitreous to waxy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed through the cooling of magma or hydrothermal activity in veins. Milky quartz gets its appearance from tiny fluid inclusions of gas or liquid trapped during crystal growth.
Uses & applications
Used in glassmaking, jewelry (as cabochons), abrasives, and as a collectible metaphysical stone.
Geological facts
Milky quartz is the most common variety of crystalline quartz. While often overlooked for clearer varieties, it can contain traces of gold in hydrothermal vein deposits.
Field identification & locations
Identify in the field by its hardness (will scratch glass), lack of cleavage, and translucent 'milky' appearance. It is found globally in igneous and metamorphic environments.
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Other mineral specimens
Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Tumbled granite
Granite, a coarse-grained felsic intrusive igneous rock
igneous
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous