
mineral
Quartz (Milky/Clear variety)
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: Translucent to milky white; Luster: Vitreous (glassy); Crystal Structure: Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Translucent to milky white
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale; Color: Translucent to milky white; Luster: Vitreous (glassy); Crystal Structure: Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed from the cooling of magma or by hydrothermal precipitation in veins. Quartz is common throughout all geological periods and is found in igneous, metamorphic, and sedimentary environments.
Uses & applications
Used in electronics (as piezoelectric crystals), glass manufacturing, abrasives, jewelry, and as a popular specimen for collectors.
Geological facts
Quartz is one of the most abundant minerals in Earth's crust. It is highly resistant to both chemical and physical weathering, which is why it often remains as river pebbles or sand.
Field identification & locations
Identify by its ability to scratch glass or steel, its glassy luster, and the lack of cleavage (it breaks in curved surfaces). Common in granite outcroppings and river beds worldwide.
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