mineral

Rose Quartz

Silicon Dioxide with trace inclusions (SiO2)

AI-generated identification · may be incorrect

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 29, 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

Forms in late-stage igneous pegmatites through hydrothermal processes. The pink hue is caused by microscopic inclusions of fibrous dumortierite-like minerals or traces of titanium and manganese.

Uses & applications

Predominantly used for ornamental purposes, cabochons for jewelry, decorative sculptures, and metaphysical 'healing' crystals.

Geological facts

Unlike other varieties of quartz, rose quartz rarely forms well-defined crystal faces and is almost always found in massive form. Some rare specimens exhibit asterism (a star-like reflection).

Field identification & locations

Identify in the field by its distinct pink color, lack of cleavage, and the ability to easily scratch glass. Commonly found in Brazil, Madagascar, South Africa, and the United States (South Dakota).