
mineral
Quartz (Milky/Common Quartz)
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: Milky white to translucent; Luster: Vitreous (glassy) to greasy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Milky white to translucent
- Luster
- Vitreous (glassy) to greasy
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Physical properties
Hardness: 7 on Mohs scale; Color: Milky white to translucent; Luster: Vitreous (glassy) to greasy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed through the cooling and crystallization of silica-rich magma or from hydrothermal veins. It is found in almost every geological environment and age, originating from igneous, metamorphic, and sedimentary processes.
Uses & applications
Used extensively in glassmaking, abrasives, quartz watches (piezoelectricity), semiconductors, construction aggregates, and as gemstones or decorative carvings.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Its name comes from the German word 'quarz', which stems from Slavic roots meaning 'hard'. Milky quartz gets its cloudy appearance from tiny fluid inclusions of gas or liquid trapped during crystal growth.
Field identification & locations
Identify in the field by its hardness (it will scratch glass/steel), lack of cleavage, and characteristic curved, glass-like (conchoidal) fractures. It is ubiquitous globally, commonly found in riverbeds, mountains, and beaches.
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