
mineral
Clear Quartz
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Colorless/Transparent; Luster: Vitreous (glassy); Crystal Structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Colorless/Transparent
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale; Color: Colorless/Transparent; Luster: Vitreous (glassy); Crystal Structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Forms from the cooling of silica-rich magma or from hydrothermal veins. It is found in all types of geological environments (igneous, metamorphic, and sedimentary) and has been forming throughout Earth's history.
Uses & applications
Used in electronics for its piezoelectric properties, glassmaking, construction (as sandpaper or abrasives), and widely in jewelry and meditation/spiritual practices.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Pure quartz is known as 'rock crystal.' It was historically used to make lenses and crystal balls.
Field identification & locations
Identify by its ability to scratch glass, its six-sided crystal habit, and its lack of cleavage. Common in granite outcrops, riverbeds, and mountain ranges globally.
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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