
mineral
Milky Quartz
Quartz (Silicon Dioxide, SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs), Color: Opaque white to translucent cream, Luster: Vitreous to greasy, Crystal System: Trigonal (Hexagonal), Cleavage: Indistinct/Conchoidal fracture, Specific Gravity: 2.65
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Physical properties
Hardness: 7 (Mohs), Color: Opaque white to translucent cream, Luster: Vitreous to greasy, Crystal System: Trigonal (Hexagonal), Cleavage: Indistinct/Conchoidal fracture, Specific Gravity: 2.65
Formation & geological history
Formed through the crystallization of silica-rich hydrothermal solutions or within pegmatites. The milky color is caused by microscopic inclusions of fluids or gas trapped during crystal growth.
Uses & applications
Used as a gemstone in tumbled form, for ornamental carvings, in the manufacturing of glass and ceramics, and as a source of silicon for electronics.
Geological facts
Milky quartz is one of the most common varieties of crystalline quartz. It is sometimes called 'Snow Quartz' in metaphysical circles and was used by ancient civilizations for tools and talismans.
Field identification & locations
Identified by its white color, inability to be scratched by steel, and lack of visible cleavage. Commonly found in veins within granite and metamorphic rocks across the globe.
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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