
mineral
Milky Quartz
Silicon Dioxide (SiO2)
Hardness: 7; Color: White to translucent milky gray; Luster: Vitreous to greasy; Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65
- Hardness
- 7
- Color
- White to translucent milky gray
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7; Color: White to translucent milky gray; Luster: Vitreous to greasy; Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65
Formation & geological history
Forms in hydrothermal veins, pegmatites, and as a primary constituent in igneous rocks like granite. The milky appearance is caused by tiny inclusions of gas or liquid trapped during crystal growth.
Uses & applications
Used in glass manufacturing, electronics (due to piezoelectric properties), construction aggregates, and low-cost jewelry or landscaping.
Geological facts
Milky quartz is the most common variety of crystalline quartz. It can sometimes contain small amounts of gold in hydrothermal vein systems.
Field identification & locations
Identify by its ability to scratch glass, its lack of cleavage, and its waxy/greasy luster on broken surfaces. It is ubiquitous globally especially in mountain ranges and gravel pits.
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Other mineral specimens
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Schist
Schist
Metamorphic
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Nephrite Jade
Nephrite
Mineral/Rock
Banded Gneiss (River Rock/Pebble)
Gneiss (specifically a banded variety often found as a river rock)
Metamorphic Rock
Green Apatite on Albite
Fluorapatite [Ca5(PO4)3F] on Albite [Na(AlSi3O8)]
mineral