
mineral
Quartz (Clear or Cloudy Quartz)
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: Colorless to white/cloudy; Luster: Vitreous (glassy); Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Colorless to white/cloudy
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale; Color: Colorless to white/cloudy; Luster: Vitreous (glassy); Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65
Formation & geological history
Formed primarily in igneous rocks like granite or in hydrothermal veins. It crystallizes from silica-rich magma or precipitates from hot watery solutions in rock crevices. It is found in all geological ages.
Uses & applications
Extensively used in glass manufacturing, electronics (due to piezoelectric properties), construction as aggregate, and in its pure forms for jewelry (gemstones) and crystal healing collections.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. It is highly resistant to both chemical and physical weathering, which is why it often ends up as the primary component of river and beach sand.
Field identification & locations
Identify in the field by its hardness (it can scratch glass), its glassy luster, and its characteristic curved (conchoidal) fracture surface. It is found worldwide, especially in mountainous regions and riverbeds.
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mineral