
mineral
Milky Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs), Color: Milky white to cloudy, Luster: Vitreous to greasy, Crystal structure: Hexagonal (Trigonal), Cleavage: None/Conchoidal fracture, Specific gravity: 2.65
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Physical properties
Hardness: 7 (Mohs), Color: Milky white to cloudy, Luster: Vitreous to greasy, Crystal structure: Hexagonal (Trigonal), Cleavage: None/Conchoidal fracture, Specific gravity: 2.65
Formation & geological history
Forms in hydrothermal veins or as a major constituent in igneous and metamorphic rocks. The cloudy appearance is caused by tiny liquid or gas bubble inclusions trapped during crystal growth.
Uses & applications
Used in glass manufacturing, electronics (due to piezoelectric properties), construction aggregates, as a gemstone in tumbled form, and for decorative landscaping.
Geological facts
Milky quartz is one of the most common varieties of crystalline quartz on Earth. Its white color is specifically due to microscopic inclusions of water or gas being trapped inside the structure millions of years ago.
Field identification & locations
Identify in the field by its hardness (will scratch glass), lack of cleavage, and common occurrence as vein filler. It is ubiquitous in mountainous regions and riverbeds worldwide.
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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