
mineral
Clear Quartz (Druzy/Crystal Cluster)
Silicon Dioxide (SiO2)
Hardness: 7 on the Mohs scale. Color: Colorless to white/transparent. Luster: Vitreous (glassy). Crystal Structure: Hexagonal (trigonal). Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.
- Hardness
- 7 on the Mohs scale
- Color
- Colorless to white/transparent
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on the Mohs scale. Color: Colorless to white/transparent. Luster: Vitreous (glassy). Crystal Structure: Hexagonal (trigonal). Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.
Formation & geological history
Formed from silica-rich hydrothermal solutions cooling in rock cavities (geodes or veins) or as late-stage crystallizations in igneous pegmatites. It can be found in rocks from nearly any geological age.
Uses & applications
Extensively used in electronics (oscillators), glassmaking, abrasives, and as a gemstone for jewelry, carvings, and metaphysical/collecting purposes.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. It is piezoelectric, meaning it generates an electric charge in response to applied mechanical stress, which is why it is used in watches.
Field identification & locations
Identify in the field by its hardness (will scratch glass and steel), lack of cleavage, and characteristic six-sided crystals. Common worldwide; notable deposits include Brazil, Arkansas (USA), and Madagascar.
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