
mineral
Clear Quartz (Rock Crystal)
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: Colorless/Transparent; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: Indistinct; Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Colorless/Transparent
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale; Color: Colorless/Transparent; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: Indistinct; Specific Gravity: 2.65
Formation & geological history
Forms in igneous, metamorphic, and sedimentary environments. Typically crystallizes from cooling magma or hydrothermal veins. It is found in many geological ages from Precambrian to recent.
Uses & applications
Used in electronics for its piezoelectric properties, glass manufacturing, jewelry, and as decorative tumbled stones for collectors.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Historically, the Greeks believed clear quartz was ice that had frozen so hard it could never melt.
Field identification & locations
Identify by its hardness (scratches glass), lack of cleavage, and transparent appearance. Commonly found in mountain ranges, riverbeds, and as geodes in volcanic areas.
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