
mineral
Rose Quartz
Silicon Dioxide (SiO2) with trace amounts of titanium, iron, or manganese
Hardness: 7 on the 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 the Mohs scale
- Color
- Pale pink to rose red
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 on the 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
Usually forms in massive form within pegmatites (igneous) through slow cooling of silica-rich magma. It is also found in hydrothermal veins. It can range in age from millions to billions of years depending on the host rock formation.
Uses & applications
Primary uses include ornamental carvings, jewelry (cabochons and beads), and as a popular decorative gemstone for collectors. It is also used in the 'metaphysical' industry.
Geological facts
Unlike regular clear quartz, rose quartz rarely forms well-defined crystals and usually occurs in large 'massive' lumps. Its color can fade if exposed to excessive sunlight over many years due to the nature of its trace mineral impurities.
Field identification & locations
Identify in the field by its distinctive pink hue, glass-like luster, and inability to be scratched by a steel knife. It is commonly found in Brazil, Madagascar, South Africa, and the United States (South Dakota).
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