mineral

Rose Quartz

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

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

Identified March 13, 2026More mineral →

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Physical properties

Hardness: 7 on the 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

Typically forms in large, coarse-grained igneous rocks called pegmatites at high temperatures. It is often found in massive form rather than distinct crystal shapes. Geological age varies greatly from millions to billions of years depending on the host pegmatite formation.

Uses & applications

Extensively used for ornamental carvings, spheres, beads for jewelry, and lapidary work. It is also a very popular specimen for crystal healing practitioners and mineral collectors.

Geological facts

Unlike other varieties of quartz, rose quartz rarely forms well-defined crystals; it usually appears as massive clumps. The pink color is often sensitive to light and can fade over long exposure to direct sunlight.

Field identification & locations

Identify in the field by its characteristic cloudy pink translucency and hardness (it will scratch glass). Common locations include Brazil, Madagascar, South Africa, and the Custer District of South Dakota (USA).

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