mineral

Rose Quartz

Silicon Dioxide (SiO2)

Hardness: 7 on Mohs scale; Color: pale pink to rose red; Luster: vitreous to greasy; 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 to greasy

Identified March 8, 2026More mineral →

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Physical properties

Hardness: 7 on Mohs scale; Color: pale pink to rose red; Luster: vitreous to greasy; Crystal Structure: Hexagonal (Trigonal); Cleavage: none (conchoidal fracture); Specific Gravity: 2.65

Formation & geological history

Formed in high-temperature silica-rich environments, typically in pegmatites or hydrothermal veins. The pink hue is caused by trace amounts of titanium, iron, or manganese, or microscopic inclusions of didumortierite.

Uses & applications

Commonly used in jewelry (cabochons, beads), decorative carvings, and as a popular specimen for rock collectors or spiritual healing practitioners.

Geological facts

Rose quartz rarely forms visible crystals; it is almost always found in massive form. Historically, it has been used in facial masks and cosmetics since Ancient Egyptian times for its supposed anti-aging properties.

Field identification & locations

Identify by its translucent pink color, lack of cleavage, and ability to scratch glass. Widely found in Brazil, Madagascar, India, and South Dakota (USA). Collectors look for deep color saturation and translucency.