
mineral
Quartz (Milky Quartz)
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: Opaque white to translucent; Luster: Vitreous to greasy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Opaque white to translucent
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 on Mohs scale; Color: Opaque white to translucent; Luster: Vitreous to greasy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
Formation & geological history
Forms in wide variety of environments including igneous, metamorphic, and sedimentary. Commonly crystallizes from silica-rich hydrothermal veins or cooling magma. It is one of the most abundant minerals in the Earth's crust.
Uses & applications
Used in electronics (as a piezoelectric material), glass making, abrasive manufacturing, and as a raw material for silicon-based products. Also popular in jewelry and metaphysical collecting.
Geological facts
Quartz is highly resistant to both mechanical and chemical weathering. Because of its durability, it is the primary component of most beach sands worldwide.
Field identification & locations
Identify in the field by its hardness (cannot be scratched by steel), lack of cleavage, and white streak. Found globally in all rock types.
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