
mineral
Clear Quartz (Rock Crystal)
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale. Color: Colorless and transparent. Luster: Vitreous (glassy). Crystal structure: Trigonal/Hexagonal. Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Colorless and transparent
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale. Color: Colorless and transparent. Luster: Vitreous (glassy). Crystal structure: Trigonal/Hexagonal. Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.
Formation & geological history
Forms in a wide variety of geological environments, most commonly from cooling magma in igneous rocks like granite or from hydrothermal veins. It can form at various temperatures and pressures throughout geological history.
Uses & applications
Used in jewelry, carvings, and as a decorative gemstone. Due to its piezoelectric properties, it is also used in electronics (oscillators and clocks) and glassmaking.
Geological facts
Clear quartz, also known as Rock Crystal, comes from the Greek word 'krystallos' meaning ice. It was once believed to be ice that had frozen so hard it would never melt. It is the second most abundant mineral in Earth's continental crust.
Field identification & locations
Identify by its transparency, 7.0 hardness (will scratch glass but not topaz), and lack of cleavage. It is found globally, with major deposits in Brazil, Madagascar, and the United States (Arkansas). Collectors look for clarity and well-defined crystal faces.
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Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Sandstone with Mineral Veining or Crust
Sedimentary Sandstone (mostly SiO2 with Fe2O3 tinting)
sedimentary
Schist
Schist
Metamorphic
Gypsum (variety Selenite or Alabaster)
Calcium sulfate dihydrate (CaSO4·2H2O)
Mineral
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Nephrite Jade
Nephrite
Mineral/Rock