
mineral
Rose Quartz
Quartz (Silicon Dioxide) - SiO2
AI-generated identification · may be incorrectHardness: 7 on the Mohs scale; Color: Pale pink to rose red; Luster: Vitreous (glass-like) to greasy; Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
- Hardness
- 7 on the Mohs scale
- Color
- Pale pink to rose red
- Luster
- Vitreous (glass-like) to greasy
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Physical properties
Hardness: 7 on the Mohs scale; Color: Pale pink to rose red; Luster: Vitreous (glass-like) to greasy; Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
Formation & geological history
Formed at high temperatures in pegmatites (igneous) or in hydrothermal veins. The pink color is usually attributed to microscopic inclusions of pink fibrous minerals like dumortierite. They can be found in rocks dating back hundreds of millions of years.
Uses & applications
Commonly used in jewelry (cabochons, beads), decorative carvings, and as a popular specimen for gemstone collectors and practitioners of crystal healing.
Geological facts
Unlike other varieties of quartz, rose quartz rarely forms well-defined external crystal faces; it is usually found in massive form. Large deposits are famously located in Brazil and Madagascar.
Field identification & locations
Identify in the field by its distinctive pink color, 7/10 hardness (it will scratch glass), and lack of cleavage. It is often found as rounded river pebbles or large chunky masses in granitic pegmatites. Collectors look for deep color and translucency.
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Granite
Granite (Phaneritic intrusive igneous rock)
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