mineral

Rose Quartz

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

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)

Identified March 24, 2026More mineral →

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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 in late-stage crystallization of igneous pegmatites and hydrothermal veins. It occurs in massive forms rather than distinct crystals. Can be found in Precambrian to Cenozoic formations.

Uses & applications

Primary use is in decorative carvings (like the elephant shown), beads, jewelry, and for spiritual/metaphysical collections.

Geological facts

Rose quartz is unique among quartz varieties because it does not form well-defined crystal faces. The pink color can fade if exposed to excessive sunlight over many years.

Field identification & locations

Identify by its characteristic hazy pink translucency and inability to be scratched by steel. Commonly found in Brazil, Madagascar, South Africa, and the Black Hills of South Dakota.

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