
mineral
Clear Quartz (Rock Crystal)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale. Color: Colorless and transparent to translucent. Luster: Vitreous (glass-like). Crystal structure: Hexagonal/Trigonal. Cleavage: Indistinct. Specific Gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Colorless and transparent to translucent
- Luster
- Vitreous (glass-like)
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Physical properties
Hardness: 7 on Mohs scale. Color: Colorless and transparent to translucent. Luster: Vitreous (glass-like). Crystal structure: Hexagonal/Trigonal. Cleavage: Indistinct. Specific Gravity: 2.65.
Formation & geological history
Forms through crystallization from magmatic pegmatites, hydrothermal veins, and metamorphic rocks across various geological ages.
Uses & applications
Used in jewelry, decorative carvings, optical instruments, electronics (piezoelectric oscillators), and highly sought after by mineral collectors.
Geological facts
Clear Quartz is one of the most abundant minerals on Earth's continental crust. Historically, ancient Greeks believed clear quartz was ice that had frozen so deeply it could never melt.
Field identification & locations
Identified by its hexagonal crystal habits, hardness 7 (scratches glass, cannot be scratched by a steel knife), and clear glassy appearance. Common in Brazil, Madagascar, the US (Arkansas, New York), and the Alps.
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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
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Granite
Granite (Phaneritic intrusive igneous rock)
igneous