
mineral
Quartz (Milky/Rose variety)
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: translucent white to faint pink; Luster: vitreous (glassy); Crystal structure: Trigonal/Hexagonal; Cleavage: none (conchoidal fracture); Specific gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- translucent white to faint pink
- Luster
- vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale; Color: translucent white to faint pink; Luster: vitreous (glassy); Crystal structure: Trigonal/Hexagonal; Cleavage: none (conchoidal fracture); Specific gravity: 2.65.
Formation & geological history
Formed from silicon-rich hydrothermal solutions or cooling magma in igneous rocks like granite. Common in veins and pegmatites across most geological eras.
Uses & applications
Used in glassmaking, electronics (piezoelectric properties), abrasives, and as a popular gemstone for lapidary work and jewelry.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. It is highly resistant to chemical and physical weathering, which is why it's a primary component of beach sand.
Field identification & locations
Identify by its ability to scratch glass, its lack of cleavage planes, and its characteristic waxy to glassy appearance. Commonly found in gravel, stream beds, and mountainous regions worldwide.
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