
mineral
Quartz
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: Colorless to white/translucent; Luster: Vitreous (glassy); Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Colorless to white/translucent
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale; Color: Colorless to white/translucent; Luster: Vitreous (glassy); Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
Formation & geological history
Forms in a wide variety of environments, including igneous crystallization (from magma), hydrothermal veins, and by precipitation from hot aqueous solutions. It is found in all geological ages.
Uses & applications
Used extensively in glassmaking, electronics (piezoelectric crystals), abrasives, construction (as sand/aggregate), and as a gemstone or ornamental stone.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. It is extremely resistant to chemical and physical weathering, which is why it often dominates beach sands.
Field identification & locations
Identify in the field by its hardness (will scratch glass), lack of cleavage, and glassy appearance. It is found globally in almost every geological setting.
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Other mineral specimens
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Schist
Schist
Metamorphic
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Gypsum (variety Selenite or Alabaster)
Calcium sulfate dihydrate (CaSO4·2H2O)
Mineral
Nephrite Jade
Nephrite
Mineral/Rock
Granite
Granite (Phaneritic intrusive igneous rock)
igneous