
mineral
Rose Quartz
Silicon Dioxide (SiO2) with trace elements of Titanium, Iron, or Manganese
AI-generated identification · may be incorrectHardness: 7 on the Mohs scale. Color: Pale pink to rose red. Luster: Vitreous (glassy). Crystal structure: Trigonal/Hexagonal (usually found in massive form). Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.
- Hardness
- 7 on the Mohs scale
- Color
- Pale pink to rose red
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on the Mohs scale. Color: Pale pink to rose red. Luster: Vitreous (glassy). Crystal structure: Trigonal/Hexagonal (usually found in massive form). Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.
Formation & geological history
Formed at high temperatures in deep-seated pegmatites and hydrothermal veins. It crystallizes from magma as it cools, often occurring in large masses rather than individual crystals. Geological ages vary by location, ranging from millions to billions of years old.
Uses & applications
Primarily used in jewelry (cabochons, beads), decorative carvings, and as a popular specimen for mineral collectors. In industry, high-purity quartz is used in glassmaking and electronics, though rose quartz specifically is mostly ornamental.
Geological facts
Unlike clear quartz which forms distinct crystals, rose quartz usually occurs in large, shapeless lumps called 'massive' quartz. A rare variety called 'Star Rose Quartz' displays asterism (a star-like reflection) due to microscopic rutile inclusions.
Field identification & locations
Identify by its translucent pink hue and lack of visible crystal faces. It can be found globally with major deposits in Brazil, South Africa, Madagascar, and the United States (South Dakota). For collectors, look for uniform color and clarity.
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Epidote
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Granite (Phaneritic intrusive igneous rock)
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