
mineral
Clear Quartz Point
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale. Color: Colorless to transparent. Luster: Vitreous (glass-like). Crystal structure: Hexagonal/Trigonal prism terminated with pyramids. Cleavage: None (conchoidal fracture). Specific gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Colorless to transparent
- Luster
- Vitreous (glass-like)
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Physical properties
Hardness: 7 on Mohs scale. Color: Colorless to transparent. Luster: Vitreous (glass-like). Crystal structure: Hexagonal/Trigonal prism terminated with pyramids. Cleavage: None (conchoidal fracture). Specific gravity: 2.65.
Formation & geological history
Forms primarily in pegmatites, hydrothermal veins, and igneous rocks through the crystallization of silica-rich fluids over millions of years.
Uses & applications
Widely used in electronics (piezoelectric oscillators), optics, lapidary art, jewelry, and crystal healing/metaphysical practices.
Geological facts
Clear quartz, also known as rock crystal, was believed by ancient Greeks to be ice frozen so hard that it could never melt. It exhibits piezoelectric properties, generating electricity when mechanical stress is applied.
Field identification & locations
Identified by its hexagonal crystal form, transparent appearance, high hardness (scratches glass easily), and lack of cleavage. Commonly found globally, with major deposits in Brazil, Madagascar, and the USA (Arkansas).
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