
mineral
Quartz (Smoky/Milky variety)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Translucent grey to milky white; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Translucent grey to milky white
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale; Color: Translucent grey to milky white; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed through the crystallization of magma or from hydrothermal veins. It is found in all geological ages and environments, particularly in igneous rocks like granite and metamorphic rocks like quartzite.
Uses & applications
Used widely in glassmaking, electronics (piezoelectric properties), abrasives, and as a semi-precious gemstone in jewelry and decorative carvings.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Its name comes from the German 'Quarz' and Greek 'krustallos', meaning 'ice'. It is resistant to both chemical and physical weathering.
Field identification & locations
Identify in the field by its inability to be scratched by a steel knife (H=7) and its lack of cleavage. Found globally; major deposits in Brazil, USA (Arkansas), and the Alps. Collectors look for clarity and well-defined crystal faces.
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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