
mineral
Rose Quartz
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: Pale pink to rose red; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (Trigonal); 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); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed through the crystallization of magma or from hydrothermal veins. The pink color is generally attributed to microscopic inclusions of a pink variety of the mineral dumortierite.
Uses & applications
Commonly used in jewelry (cabochons, beads), ornamental carvings, crystal healing practices, and as a decorative stone in landscaping or interior design.
Geological facts
Rose quartz rarely forms large crystals; it usually occurs in massive form. The pink color can fade if exposed to excessive heat or direct sunlight over a long period.
Field identification & locations
Identify in the field by its distinct pink hue, lack of cleavage, and ability to scratch glass. It is commonly found in pegmatites in Brazil, South Africa, India, and Madagascar.
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Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Sandstone with Mineral Veining or Crust
Sedimentary Sandstone (mostly SiO2 with Fe2O3 tinting)
sedimentary
Schist
Schist
Metamorphic
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Gypsum (variety Selenite or Alabaster)
Calcium sulfate dihydrate (CaSO4·2H2O)
Mineral
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Nephrite
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