
mineral
Milky Quartz
Silicon Dioxide (SiO2)
Hardness: 7 (Mohs scale); Color: White, milky, or gray; Luster: Vitreous to greasy; Crystal structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific gravity: 2.65
- Hardness
- 7 (Mohs scale)
- Color
- White, milky, or gray
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 (Mohs scale); Color: White, milky, or gray; Luster: Vitreous to greasy; Crystal structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific gravity: 2.65
Formation & geological history
Forms in hydrothermal veins or pegmatites where silica-rich fluids cool slowly; often found in all types of environments including igneous, metamorphic, and sedimentary rocks.
Uses & applications
Used as a landscape stone, in glass making, as a source of silicon for electronics, and occasionally for carving or low-value jewelry.
Geological facts
Milky quartz gets its white color from tiny bubbles of gas or liquid trapped during its formation. It is the most common variety of crystalline quartz.
Field identification & locations
Identify in the field by its hardness (it will scratch glass), lack of cleavage, and white opaque color. It is commonly found in mountainous regions or as pebbles in riverbeds.
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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
Gypsum (variety Selenite or Alabaster)
Calcium sulfate dihydrate (CaSO4·2H2O)
Mineral
Nephrite Jade
Nephrite
Mineral/Rock
Granite
Granite (Phaneritic intrusive igneous rock)
igneous