
mineral
Clear Quartz
Silicon Dioxide (SiO2)
Hardness: 7 Mohs; Color: Colorless/Transparent; Luster: Vitreous; Crystal system: Trigonal/Hexagonal; Cleavage: None/Conchoidal fracture; Specific gravity: 2.65.
- Hardness
- 7 Mohs
- Color
- Colorless/Transparent
- Luster
- Vitreous
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Physical properties
Hardness: 7 Mohs; Color: Colorless/Transparent; Luster: Vitreous; Crystal system: Trigonal/Hexagonal; Cleavage: None/Conchoidal fracture; Specific gravity: 2.65.
Formation & geological history
Formed in almost all geological environments, primarily cooling from silica-rich magma or from hydrothermal veins. Often found in pegmatites and geodetic cavities.
Uses & applications
Used in electronics (oscillators), manufacturing of glass and ceramics, gemstone jewelry, and as a popular metaphysical or decorative stone.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. It is piezoelectric, meaning it generates an electric charge when mechanical pressure is applied.
Field identification & locations
Identified by its ability to scratch glass and lack of cleavage. This specific specimen appears to be 'Ema Egg' or a river-tumbled frosted quartz that has been window-polished on one side.
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sedimentary
Sandstone with Mineral Veining or Crust
Sedimentary Sandstone (mostly SiO2 with Fe2O3 tinting)
sedimentary
Schist
Schist
Metamorphic
Potassium Feldspar (Orthoclase)
Orthoclase (KAlSi3O8)
mineral
Gypsum (variety Selenite or Alabaster)
Calcium sulfate dihydrate (CaSO4·2H2O)
Mineral
Nephrite Jade
Nephrite
Mineral/Rock