
mineral
Pink Quartz / Rose Quartz
Silicon Dioxide (SiO2)
Hardness: 7 (Mohs scale); Color: Pale pink to reddish blossom; Luster: Vitreous to greasy; Crystal structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific gravity: 2.65
- Hardness
- 7 (Mohs scale)
- Color
- Pale pink to reddish blossom
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 (Mohs scale); Color: Pale pink to reddish blossom; Luster: Vitreous to greasy; Crystal structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific gravity: 2.65
Formation & geological history
Usually forms in magmatic pegmatites through the cooling of silica-rich hydrothermal fluids or as part of the core concentration in granite pegmatites.
Uses & applications
Primary use in jewelry (beads, cabochons), ornamental carvings, crystal healing/metaphysical practices, and as a decorative landscaping stone.
Geological facts
The pink color was traditionally thought to be caused by titanium, manganese, or iron, but modern studies suggest microscopic inclusions of a fibrous pink borosilicate mineral related to dumortierite cause the hue.
Field identification & locations
Identify by its characteristic pink hue, hardness (it will scratch glass), and lack of cleavage. It is commonly found in riverbeds or within quartz veins near granitic bodies.
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