
mineral
Rose Quartz
Silicon Dioxide (SiO2) with trace Titanium, Manganese, or Iron
Hardness: 7 on Mohs scale; Color: Pale pink to rose red; Luster: Vitreous 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 to greasy
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Physical properties
Hardness: 7 on Mohs scale; Color: Pale pink to rose red; Luster: Vitreous to greasy; Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed in late-stage crystallization of pegmatites and hydrothermal veins. The pink color is attributed to microscopic inclusions of fibrous dumortierite-related minerals or charge-transfers between metal ions.
Uses & applications
Extensively used in lapidary work for beads, cabochons, and carvings. Also used as a decorative stone in architecture and popular in the metaphysical community.
Geological facts
Rose quartz rarely forms visible crystals; it usually occurs as massive aggregates. It is often called the 'Heart Stone' and has been used in jewelry since at least 700 BC in Mesopotamia.
Field identification & locations
Identify by its characteristic pink hue and quartz hardness (will scratch glass). Commonly found in Brazil, Madagascar, South Africa, and the United States (South Dakota).
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Mineral/Rock
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Metamorphic Rock
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mineral