
mineral
Milky Quartz
Crystalline Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Cloudy white to grayish; Luster: Vitreous (glassy) to greasy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Cloudy white to grayish
- Luster
- Vitreous (glassy) to greasy
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Physical properties
Hardness: 7 on Mohs scale; Color: Cloudy white to grayish; Luster: Vitreous (glassy) to greasy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Forms in hydrothermal veins and pegmatites when silica-rich fluids cool and crystallize. The milky appearance is caused by tiny inclusions of gas or liquid trapped during crystal growth. Can be found in geological formations across all ages.
Uses & applications
Used in glass manufacturing, electronics (due to piezoelectric properties), construction aggregates, as an abrasive, and in landscaping or decorative home decor.
Geological facts
Milky Quartz is the most common variety of crystalline quartz. It can sometimes contain trace amounts of gold within its veins in certain geological regions.
Field identification & locations
Identify by its hardness (will scratch glass), lack of cleavage, and translucent white color. It is commonly found in riverbeds, mountain ranges, and near granite outcrops globally. collectors should look for distinct crystal faces.
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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