
mineral
Milky Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Opaque white to milky white; Luster: Vitreous to greasy; Crystal Structure: Hexagonal (trigonal); Cleavage: None/Conchoidal fracture; Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Opaque white to milky white
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 on Mohs scale; Color: Opaque white to milky white; Luster: Vitreous to greasy; Crystal Structure: Hexagonal (trigonal); Cleavage: None/Conchoidal fracture; Specific Gravity: 2.65
Formation & geological history
Formed from hydrothermal solutions or within pegmatites and igneous rocks. The cloudy appearance is caused by tiny inclusions of gas or liquid trapped during crystal growth. They can be found in rocks from many geological ages.
Uses & applications
Used in glassmaking, construction as aggregate, electronics (piezoelectric properties), and as inexpensive gemstones or decorative landscaping stones.
Geological facts
Milky quartz is the most common variety of crystalline quartz. It is often found as the 'vein' material that miners follow to find gold, as they frequently occur together.
Field identification & locations
Identified by its white, opaque appearance, hardness (it can scratch glass), and lack of cleavage. It is commonly found in riverbeds, mountains, and as garden stones worldwide.
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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