
mineral
Quartz (Clear/Smoky Geode fragment)
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: Colorless to greyish-lilac; Luster: Vitreous (glassy); Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Colorless to greyish-lilac
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale; Color: Colorless to greyish-lilac; Luster: Vitreous (glassy); Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed via hydrothermal activity where silica-rich fluids precipitate in rock cavities (vugs) or gas bubbles in volcanic rock. These specimens can range from thousands to millions of years old based on the host rock formation.
Uses & applications
Used extensively in industry for glassmaking, abrasives, and electronics (due to piezoelectric properties). Highly valued in jewelry as semi-precious stones and popular in metaphysical and crystal collections.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Pure quartz is known as rock crystal, while impurities create variants like amethyst or citrine.
Field identification & locations
Identify by its inability to be scratched by steel, its glassy luster, and the presence of hexagonal pyramidal crystal terminations. Found globally in all types of geological environments.
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