
mineral
Milky Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Milky white to cloudy; Luster: Vitreous to greasy; Crystal Structure: Hexagonal (trigonal); Cleavage: Indistinct/conchoidal fracture; Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Milky white to cloudy
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 on Mohs scale; Color: Milky white to cloudy; Luster: Vitreous to greasy; Crystal Structure: Hexagonal (trigonal); Cleavage: Indistinct/conchoidal fracture; Specific Gravity: 2.65
Formation & geological history
Formed in hydrothermal veins and pegmatites through the slow cooling of silica-rich hot fluids deep within the Earth's crust. It is a major constituent of igneous rocks like granite.
Uses & applications
Used in glassmaking, abrasives, electronics (piezoelectric properties), jewelry (cabochons), and as a landscape decorative stone.
Geological facts
The milky appearance is caused by tiny inclusions of gas or liquid trapped during crystal growth. It is the most common variety of crystalline quartz found on Earth.
Field identification & locations
Identify by its white cloudy color, inability to be scratched by a steel knife, and glass-like luster on fresh breaks. Found globally in mountainous regions and riverbeds.
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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