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 February 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 pegmatites or in hydrothermal veins, typically at high temperatures. Occurs in large massive formations rather than individual crystals.

Uses & applications

Used widely in the jewelry industry for beads, cabochons, and carvings. Also used as a decorative stone in interior design, landscaping, and by metaphysical collectors.

Geological facts

Unlike other varieties of quartz, rose quartz rarely forms well-defined crystal faces; it is almost always found in 'massive' form. The color is believed to be caused by microscopic inclusions of didumortierite.

Field identification & locations

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

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