
mineral
Milky Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs scale); Color: Opaque white to cream/tan; Luster: Vitreous to greasy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 (Mohs scale)
- Color
- Opaque white to cream/tan
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 (Mohs scale); Color: Opaque white to cream/tan; Luster: Vitreous to greasy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Forms in hydrothermal veins or as a primary constituent in igneous rocks like granite. It is extremely common and found in geological formations across all ages due to its chemical stability.
Uses & applications
Used as a gemstone in jewelry (cabochons), as an abrasive, in the production of glass and silicon, and as a popular specimen for collectors.
Geological facts
Milky quartz is the most common variety of crystalline quartz. Its cloudy appearance is caused by tiny fluid or gas inclusions trapped during crystal growth.
Field identification & locations
Identify in the field by its hardness (scratches glass), waxy/greasy luster on broken surfaces, and lack of cleavage. Commonly found in riverbeds and mountainous terrain.
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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