
mineral
Rose Quartz
Silicon dioxide (SiO2)
Hardness: 7 on Mohs scale. Color: Pale pink to rose red. Luster: Vitreous (glassy). Crystal Structure: Hexagonal (trigonal), though rarely found as distinct crystals. Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Pale pink to rose red
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale. Color: Pale pink to rose red. Luster: Vitreous (glassy). Crystal Structure: Hexagonal (trigonal), though rarely found as distinct crystals. Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.
Formation & geological history
Forms in PEGMATITES (igneous rock) and hydrothermal veins. The pink color is usually attributed to trace amounts of titanium, iron, or manganese, or microscopic mineral inclusions of a pinkish fibrous silicate.
Uses & applications
Widely used as an ornamental stone, in jewelry (beads, cabochons), and for decorative carvings. It is also highly popular in the metaphysical and gemstone collecting communities.
Geological facts
Unlike other varieties of quartz, rose quartz rarely forms well-defined crystals. It is the state mineral of South Dakota. The name is derived from its unique rose-pink hue.
Field identification & locations
Identify by its translucent pink color and inability to be scratched by a steel blade. It is commonly found in Brazil, Madagascar, South Africa, and the United States (South Dakota).
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Sedimentary Sandstone (mostly SiO2 with Fe2O3 tinting)
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Schist
Schist
Metamorphic
Potassium Feldspar (Orthoclase)
Orthoclase (KAlSi3O8)
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Gypsum (variety Selenite or Alabaster)
Calcium sulfate dihydrate (CaSO4·2H2O)
Mineral
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
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