
mineral
Milky Quartz
Quartz (Silicon Dioxide - SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale. Color: White to cloudy. Luster: Vitreous (glassy) to greasy. Crystal structure: Hexagonal/Trigonal. Cleavage: Indistinct/None. Specific gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- White to cloudy
- Luster
- Vitreous (glassy) to greasy
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Physical properties
Hardness: 7 on Mohs scale. Color: White to cloudy. Luster: Vitreous (glassy) to greasy. Crystal structure: Hexagonal/Trigonal. Cleavage: Indistinct/None. Specific gravity: 2.65.
Formation & geological history
Formed from the crystallization of silica-rich magma or hydrothermal fluids. The milky appearance is caused by tiny inclusion of gas, liquids, or both, trapped during crystal growth.
Uses & applications
Used as an abrasive, in glassmaking, and in electronics (piezoelectric properties). Often used as a landscaping decorative stone or for metaphysical/collecting purposes.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Milky quartz is the most common variety of crystalline quartz found in nature.
Field identification & locations
Identify by its ability to scratch glass, its white cloudy color, and its lack of cleavage (conchoidal fracture). It is found worldwide in igneous and metamorphic terrains.
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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