mineral

Rose Quartz

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

Identified March 25, 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

Usually forms in magmatic pegmatites through the crystallization of silica-rich magma. The pink color is generally attributed to microscopic inclusions of pink borosilicate mineral fibers (dumortierite).

Uses & applications

Primarily used for ornamental purposes, including carvings, beads, and cabochons in jewelry. It is also highly popular in the metaphysical/collecting community as a 'stone of love'.

Geological facts

Unlike other varieties of quartz, rose quartz rarely forms well-defined external crystal faces; it usually occurs in massive form. The first specimens were found in the 1800s in Maine, USA, and Brazil.

Field identification & locations

Identify by its translucent pink hue and lack of visible crystal faces. It can scratch glass easily due to its hardness. Common locations include Brazil, Madagascar, South Africa, and the United States (South Dakota and Maine).