mineral

Rose Quartz

Silicon dioxide with traces of titanium, iron, or manganese (SiO2)

AI-generated identification · may be incorrect

Hardness: 7 (Mohs scale); Color: Pale pink to rose red; Luster: Vitreous 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 to greasy

Identified April 15, 2026More mineral →

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Physical properties

Hardness: 7 (Mohs scale); Color: Pale pink to rose red; Luster: Vitreous to greasy; Crystal Structure: Hexagonal (Trigonal); Cleavage: Indistinct/Conchoidal fracture; Specific Gravity: 2.65

Formation & geological history

Formed in high-temperature silica-rich environments, specifically within hydrothermal veins and igneous pegmatites. Coloration is a result of microscopic inclusions of dumortierite or similar minerals containing titanium and manganese.

Uses & applications

Extensively used in lapidary work for cabochons, beads, and carvings. Also popular in jewelry, as raw decorative specimens, and increasingly within the metaphysical/spiritual community.

Geological facts

Unlike other varieties of quartz, rose quartz rarely forms well-defined crystal faces and is typically found in massive (clumpy) form. It can exhibit asterism (a star-like light effect) when cut correctly as a cabochon.

Field identification & locations

Identify in the field by its distinct pink hue, lack of cleavage, and ability to scratch glass. It is commonly found in Brazil, Madagascar, South Africa, and the United States (South Dakota).