
mineral
Quartz Crystal
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale. Color: Clear, white, gray, yellowish, or smoky. Luster: Vitreous (glassy). Crystal Structure: Trigonal. Cleavage: None. Specific Gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Clear, white, gray, yellowish, or smoky
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale. Color: Clear, white, gray, yellowish, or smoky. Luster: Vitreous (glassy). Crystal Structure: Trigonal. Cleavage: None. Specific Gravity: 2.65.
Formation & geological history
Formed in a wide variety of geological environments, commonly in hydrothermal veins, pegmatites, and as a primary constituent of igneous, metamorphic, and sedimentary rocks.
Uses & applications
Used in electronics, oscillators, watches, glassware, gemstones, and abrasive materials.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust, surpassed only by feldspar. It exhibits piezoelectric properties, meaning it can generate an electrical charge in response to applied mechanical stress.
Field identification & locations
Identified by its conchoidal fracture, lack of cleavage, high hardness (scratches glass), and distinct vitreous luster. Found globally in almost every geological setting.
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