
mineral
Quartz / Vein Quartz
Quartz (Silicon Dioxide, SiO2)
Hardness: 7 on Mohs scale; Color: Milky white to translucent grayish; 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 grayish
- Luster
- Vitreous (glassy) to greasy
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Physical properties
Hardness: 7 on Mohs scale; Color: Milky white to translucent grayish; Luster: Vitreous (glassy) to greasy; Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
Formation & geological history
Formed through hydrothermal processes where silicon-rich fluids fill fractures in surrounding rock. It can also be found in igneous rocks like granite or as a primary component in metamorphic rocks. Occurs across all geological eras.
Uses & applications
Used widely in glass making, electronics (piezoelectric properties), abrasives, as a construction aggregate, and in jewelry (as semiprecious stones like amethyst or citrine).
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 is the primary component of most beach sand.
Field identification & locations
Identify in the field by its inability to be scratched by a steel knife (7 hardness) and its lack of cleavage. It often has a 'sugary' or glassy appearance and is common in riverbeds and mountainous terrain.
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