mineral

Rose Quartz

Silicon Dioxide (SiO2)

Hardness: 7 on Mohs scale; Color: Pale pink to rose red; Luster: Vitreous; 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

Identified June 17, 2026More mineral →

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Physical properties

Hardness: 7 on Mohs scale; Color: Pale pink to rose red; Luster: Vitreous; Crystal Structure: Hexagonal (Trigonal); Cleavage: None/Conchoidal fracture; Specific Gravity: 2.65

Formation & geological history

Formed through the cooling and crystallization of silica-rich magma in pegmatites, or occasionally in hydrothermal veins. The pink color is caused by trace amounts of titanium, iron, or manganese.

Uses & applications

Used primarily in jewelry (cabochons, beads), decorative carvings, high-end interior ornaments, and as a popular specimen for gemstone collectors and metaphysical practitioners.

Geological facts

Rose quartz is rarely found as individual crystals; it usually occurs in massive form. The pink color is sensitive to light and can fade if exposed to prolonged UV sunlight.

Field identification & locations

Identify by its characteristic hazy translucent pink color and ability to scratch glass. It is commonly found in Brazil, Madagascar, South Africa, and the United States (South Dakota).