
mineral
Clear Quartz Crystal
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: Colorless to transparent; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: Indistinct/None; Specific Gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Colorless to transparent
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale; Color: Colorless to transparent; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: Indistinct/None; Specific Gravity: 2.65.
Formation & geological history
Formed through the cooling and crystallization of silica-rich hydrothermal fluids in veins or cavities within igneous, metamorphic, and sedimentary rocks. They grow over millions of years.
Uses & applications
Used in electronics for its piezoelectric properties (oscillators, watches), glass-making, jewelry, optics, and as decorative collector specimens.
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
Identify by its transparent appearance, hexagonal prism shape with pyramidal ends, and the ability to scratch glass. Found worldwide, with major deposits in Brazil and Arkansas, USA.
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Mineral/Rock
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mineral