
mineral
Rose Quartz
Rose Quartz (SiO2 with traces of Ti, Fe, or Mn)
Hardness: 7 on Mohs scale; Color: Pale pink to rose red; Luster: Vitreous/Glassy; Crystal Structure: Trigonal (often occurs in massive form); 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: Trigonal (often occurs in massive form); Cleavage: None/Conchoidal fracture; Specific Gravity: 2.65
Formation & geological history
Formed in late-stage crystallization of pegmatites (igneous) through hydrothermal veins. Its pink color is typically attributed to microscopic inclusions of a fibrous pink mineral similar to dumortierite.
Uses & applications
Extensively used in jewelry (beads, cabochons), carving, ornamental decor, and as healing stones in metaphysical practices. High-quality transparent pieces are rare and used for faceted gems.
Geological facts
Unlike other quartz varieties, Rose Quartz rarely forms distinct crystal points and is usually found in large 'massive' chunks. Large deposits are found in Brazil, South Africa, and Madagascar.
Field identification & locations
Identify by its characteristic pink hue and translucency. In the field, look for glassy luster and lack of cleavage. Common in pegmatite-rich areas like the Black Hills of South Dakota.
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