
mineral
Quartz (specifically Clear Quartz or Rock Crystal)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on the Mohs scale. Color: Clear to translucent/white. Luster: Vitreous (glass-like). Crystal structure: Trigonal/Hexagonal. Cleavage: Indistinct (conchoidal fracture). Specific gravity: 2.65.
- Hardness
- 7 on the Mohs scale
- Color
- Clear to translucent/white
- Luster
- Vitreous (glass-like)
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Physical properties
Hardness: 7 on the Mohs scale. Color: Clear to translucent/white. Luster: Vitreous (glass-like). Crystal structure: Trigonal/Hexagonal. Cleavage: Indistinct (conchoidal fracture). Specific gravity: 2.65.
Formation & geological history
Formed through the cooling of silica-rich magma or from hydrothermal veins. It is found in all three types of rock (igneous, metamorphic, and sedimentary) across billions of years of Earth's history.
Uses & applications
Extensively used in electronics (oscillators), manufacturing of glass, abrasives, and as gemstones in jewelry. Also popular in metaphysical and crystal collecting communities.
Geological facts
Quartz is one of the most abundant minerals in Earth's crust. It is piezoelectric, meaning it generates an electric charge when mechanically stressed, which is why it is used in watches and clocks.
Field identification & locations
Identify in the field by its hardness (will scratch glass and steel), lack of cleavage (breaks like shards of glass), and hexagonal crystal habits if not weathered. Found globally in almost every geological environment.
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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