
mineral
Clear Quartz
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: Clear to translucent; Luster: Vitreous; Crystal system: Trigonal/Hexagonal; Cleavage: None/Conchoidal fracture; Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Clear to translucent
- Luster
- Vitreous
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Physical properties
Hardness: 7 on Mohs scale; Color: Clear to translucent; Luster: Vitreous; Crystal system: Trigonal/Hexagonal; Cleavage: None/Conchoidal fracture; Specific Gravity: 2.65
Formation & geological history
Quartz forms in a wide variety of geological environments, most notably from the cooling of magma or precipitation from hydrothermal veins. It is a major constituent of igneous rocks like granite and metamorphic rocks like quartzite.
Uses & applications
Extensively used in electronics for its piezoelectric properties, glass manufacturing, abrasives, timekeeping (quartz watches), and as a gemstone for jewelry and metaphysical collecting.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. It is highly resistant to both mechanical and chemical weathering.
Field identification & locations
Identify by its 7 hardness (scratches glass and steel), hexagonal crystal shape (if present), and conchoidal (shell-like) fracture patterns. It is found globally in almost all rock-forming environments.
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