
mineral
Milky Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Opaque white to off-white; Luster: Vitreous to greasy; Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Opaque white to off-white
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 on Mohs scale; Color: Opaque white to off-white; Luster: Vitreous to greasy; Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65
Formation & geological history
Forms in hydrothermal veins, pegmatites, igneous intrusive environments, and metamorphic rocks. The white cloudy appearance is caused by tiny gas or liquid bubbles trapped during crystal growth.
Uses & applications
Used in electronics (piezoelectric applications), silicon metal production, glassmaking, construction aggregates, and popular for decorative carving and rock collecting.
Geological facts
Milky Quartz is the most common variety of crystalline quartz found on Earth's surface. Its white appearance is often due to microscopic fluid inclusions dating back billions of years.
Field identification & locations
Identified by its white milky color, inability to be scratched by steel (hardness 7), and glass-like to greasy luster. Widely available worldwide in river beds, gravel pits, and mountain veins.
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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
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
Septarian Pebble
Septarian nodule / Concretion
sedimentary