
mineral
Rose Quartz
Silicon dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: Pink, ranging from very pale to deep rose; Luster: Vitreous (glass-like); Crystal structure: Hexagonal/Trigonal; Cleavage: None/Conchoidal fracture; Specific gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Pink, ranging from very pale to deep rose
- Luster
- Vitreous (glass-like)
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Physical properties
Hardness: 7 on Mohs scale; Color: Pink, ranging from very pale to deep rose; Luster: Vitreous (glass-like); Crystal structure: Hexagonal/Trigonal; Cleavage: None/Conchoidal fracture; Specific gravity: 2.65
Formation & geological history
Forms primarily in igneous pegmatites through the crystallization of silica-rich magma. The pink color is caused by trace amounts of titanium, iron, or manganese, or microscopic inclusions of aluminum-containing borosilicate. It is often millions of years old.
Uses & applications
Commonly used in jewelry (beads, cabochons), ornamental carvings, decorative stones, and modern spiritual practices as a 'love stone'.
Geological facts
Unlike clear quartz, rose quartz rarely forms large well-defined crystal faces. It is the state mineral of South Dakota. The world's largest Rose Quartz sphere is over 12,000 lbs.
Field identification & locations
Identify by its characteristic pink hue and translucency. It will scratch glass but cannot be scratched by a steel knife. Major deposits are found in Brazil, Madagascar, and South Dakota, USA.
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mineral