mineral

Rose Quartz

Quartz (Silicon Dioxide - SiO2)

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

Identified March 26, 2026More mineral →

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Physical properties

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

Formation & geological history

Formed in igneous pegmatites and hydrothermal veins. The pink color is generally attributed to microscopic inclusions of a fibrous pink mineral similar to dumortierite. They can be hundreds of millions of years old depending on the geological formation.

Uses & applications

Commonly used in jewelry (cabochons, beads), decorative carvings, spiritual/metaphysical practices, and as a popular ornamental stone for collectors.

Geological facts

Rose quartz rarely forms visible crystals; it is almost always found in massive form. The first record of its use dates back to 600 BC in modern-day Iraq (Assyria), where it was used as beads.

Field identification & locations

Identify by its translucent pink hue and ability to scratch glass. Found in Brazil, South Africa, Madagascar, and the US (South Dakota). Often found in riverbeds or near pegmatite outcrops.