
mineral
Rose Quartz
Silicon Dioxide (SiO2) with trace amounts of titanium, iron, or manganese
Hardness: 7 (Mohs scale); Color: Pale pink to rose red; Luster: Vitreous (glassy) to greasy; Crystal structure: Hexagonal (Trigonal); Cleavage: Indistinct/Conchoidal fracture; Specific gravity: 2.65
- Hardness
- 7 (Mohs scale)
- Color
- Pale pink to rose red
- Luster
- Vitreous (glassy) to greasy
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Physical properties
Hardness: 7 (Mohs scale); Color: Pale pink to rose red; Luster: Vitreous (glassy) to greasy; Crystal structure: Hexagonal (Trigonal); Cleavage: Indistinct/Conchoidal fracture; Specific gravity: 2.65
Formation & geological history
Formed through the crystallization of magma (igneous) in pegmatites or in hydrothermal veins. Specimens can range from hundreds of millions to billions of years old depending on the geological deposit.
Uses & applications
Primarily used in jewelry (cabochons, beads), decorative carvings, and as 'pocket stones' for crystal healing practices. It is also used as a gemstone for collectors and in ornamental home decor.
Geological facts
Unlike clear quartz, rose quartz rarely forms large, well-defined individual crystal prisms. The color is thought to be caused by microscopic inclusions of a fibrous pink mineral (similar to dumortierite) within the quartz matrix.
Field identification & locations
Identify in the field by its characteristic pink hue, high hardness (will scratch glass), and lack of cleavage planes. Common locations include Brazil (Minas Gerais), South Africa, Madagascar, and the United States (South Dakota).
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