
mineral
Milky Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale. Color: White to opaque milky white. Luster: Vitreous to greasy. Crystal system: Trigonal. Cleavage: Indistinct/Conchoidal fracture. Specific Gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- White to opaque milky white
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 on Mohs scale. Color: White to opaque milky white. Luster: Vitreous to greasy. Crystal system: Trigonal. Cleavage: Indistinct/Conchoidal fracture. Specific Gravity: 2.65.
Formation & geological history
Forms in hydrothermal veins and pegmatites when silica-rich fluids cool. The milky appearance is caused by tiny inclusions of gas or liquid trapped during crystal growth. Can be found in rocks of all geological ages.
Uses & applications
Used as an abrasive, in glass making, as a source of silicon for electronics, and widely as a landscaping or decorative stone.
Geological facts
Milky quartz is the most common variety of crystalline quartz. While often overlooked for clearer varieties like rock crystal, it can contain microscopic gold inclusions in certain geological settings.
Field identification & locations
Identify in the field by its hardness (it will easily scratch glass), its white color, and its lack of true cleavage. It is ubiquitous in mountainous regions and streambeds.
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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