
mineral
Quartz (Milky/Clear variety)
Silicon Dioxide (SiO2)
Hardness: 7 (Mohs scale); Color: White to colorless/transparent; Luster: Vitreous (glassy); Crystal Structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 (Mohs scale)
- Color
- White to colorless/transparent
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 (Mohs scale); Color: White to colorless/transparent; Luster: Vitreous (glassy); Crystal Structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed through the cooling of molten rock (igneous) or through hydrothermal precipitation from hot, mineral-rich fluids in veins. It is found across all geological ages in igneous, metamorphic, and sedimentary environments.
Uses & applications
Used in electronics (oscillators), glassmaking, abrasives, construction (sand), and as a popular gemstone for jewelry and metaphysical collections.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Its name comes from the Greek word 'krustallos' meaning ice, as ancients believed it was permanently frozen ice.
Field identification & locations
Identify by its hardness (it can scratch glass), lack of cleavage, and glassy appearance. Commonly found along stream beds, in mountains, or inside geodes globally.
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