
mineral
Quartz (River Pebble)
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: Milky white to yellowish-tan; Luster: Vitreous to waxy; Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Milky white to yellowish-tan
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 7 on Mohs scale; Color: Milky white to yellowish-tan; Luster: Vitreous to waxy; Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
Formation & geological history
Formed from silica-rich hydrothermal solutions or cooling magma. This specific specimen has been chemically weathered and physically rounded by river transport over thousands of years.
Uses & applications
Used in glass manufacturing, electronics (piezoelectric properties), abrasives, and as decorative landscaping gravel. High-quality crystals are used in jewelry.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Its name comes from the German word 'Quarz', which means 'hard'.
Field identification & locations
Identify in the field by its hardness (it will scratch glass) and lack of cleavage (it breaks into irregular, shell-like curves). Commonly found in riverbeds and beaches globally.
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