
mineral
Quartz (Smoky or Citrine variety)
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: yellowish-brown to tan; Luster: Vitreous/glassy; Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- yellowish-brown to tan
- Luster
- Vitreous/glassy
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Physical properties
Hardness: 7 on Mohs scale; Color: yellowish-brown to tan; Luster: Vitreous/glassy; Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed through hydrothermal processes or in pegmatites. It crystallizes from molten silica-rich fluids as they cool in Earth's crust. Most specimens are millions of years old.
Uses & applications
Used in jewelry as gemstones, in manufacturing glass, and in electronics for its piezoelectric properties. Highly sought after by mineral collectors.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Its name comes from the German word 'Quarz', which has Slavic origins meaning 'hard'.
Field identification & locations
Identify in the field by its hardness (will scratch glass) and lack of cleavage. Found globally in deserts, mountains, and riverbeds. Look for glassy luster and hexagonal crystal faces.
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