
mineral
Rose Quartz
Silicon Dioxide (SiO2) with trace amounts of titanium, iron, or manganese
Hardness: 7 on Mohs scale; Color: Pale pink to rose red; Luster: Vitreous (glassy) to greasy; Crystal Structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Pale pink to rose red
- Luster
- Vitreous (glassy) to greasy
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Physical properties
Hardness: 7 on Mohs scale; Color: Pale pink to rose red; Luster: Vitreous (glassy) to greasy; Crystal Structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed in late-stage igneous pegmatites or hydrothermal veins. The pink color is generally attributed to microscopic inclusions of a pink variety of the borosilicate mineral dumortierite.
Uses & applications
Extensively used for ornamental carvings, faceted gemstones, beads for jewelry, and as a popular specimen for mineral collectors and metaphysical practitioners.
Geological facts
Rose quartz rarely forms well-defined crystal faces and usually occurs in massive aggregate forms. Ancient Egyptians, Greeks, and Romans used rose quartz as talismans and in facial masks to clear complexions.
Field identification & locations
Identify by its characteristic pink hue, high hardness (will scratch glass), and lack of cleavage. Common locations include Brazil, Madagascar, South Africa, and the United States (South Dakota).
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