Rock Identifier
Rose Quartz (Silicon Dioxide (SiO2) with trace amounts of titanium, iron, or manganese) — mineral
mineral

Rose Quartz

Silicon Dioxide (SiO2) with trace amounts of titanium, iron, or manganese

Hardness: 7.0 on the 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
Color
Pale pink to rose red
Luster
Vitreous (glassy)
Identified More mineral

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Physical properties

Hardness: 7.0 on the 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

Typically forms at high temperatures in late-stage crystallization of igneous pegmatites or in hydrothermal veins. It is found in deposits dating back millions of years.

Uses & applications

Widely used for ornamental carvings, jewelry (beads and cabochons), metaphysical products, and as a decorative stone in landscaping and interior design.

Geological facts

Unlike other varieties of quartz, rose quartz rarely forms visible crystal faces and usually occurs in massive form. The pink color is widely attributed to microscopic inclusions of a fibrous pink mineral similar to dumortierite.

Field identification & locations

Identified by its signature pink hue and lack of cleavage planes. Found abundantly in Brazil, Madagascar, South Africa, and the United States (South Dakota). Can be identified in the field by its hardness (ability to scratch glass) and glassy luster.