
mineral
Clear Quartz (Rock Crystal)
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: Colorless/Transparent; Luster: Vitreous; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Colorless/Transparent
- Luster
- Vitreous
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Physical properties
Hardness: 7 on Mohs scale; Color: Colorless/Transparent; Luster: Vitreous; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Forms in a wide range of geological environments, most commonly from the cooling of magma in igneous rocks like granite or from hydrothermal veins. It can be found in rocks of all ages.
Uses & applications
Extremely versatile; used in electronics (oscillators), optical instruments, glassmaking, abrasive blasting, and extensively in jewelry and gemstone carving.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. The name 'quartz' comes from the German word 'Quarz', while 'crystal' comes from the Greek word 'krystallos', meaning ice.
Field identification & locations
Identified by its transparency, its ability to scratch glass (hardness 7), and its lack of cleavage. Look for it in riverbeds, mountain veins, or within geodes. Collectors value specimens with high clarity or unique inclusions.
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mineral