
Mineral
Clear Quartz
Silicon Dioxide (SiO2)
Hardness: 7 (Mohs scale); Color: Colorless/Transparent; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 (Mohs scale)
- Color
- Colorless/Transparent
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 (Mohs scale); Color: Colorless/Transparent; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed through the cooling and crystallization of silica-rich magma or from hydrothermal veins. It can occur in all geological ages and is found in igneous, metamorphic, and sedimentary environments.
Uses & applications
Used in electronics for its piezoelectric properties, glass manufacturing, abrasives, jewelry (gemstones), and decorative carvings.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Ancient civilizations believed it was permanent ice formed by the gods. It is the defining mineral for hardness 7 on the Mohs scale.
Field identification & locations
Identify by its ability to scratch glass and steel, lack of cleavage, and common six-sided prism shape. It is found worldwide, notably in Brazil, Arkansas (USA), and Madagascar.
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