mineral

Rose Quartz

Silicon dioxide (SiO2) with trace amounts of titanium, iron, or manganese

AI-generated identification · may be incorrect

Hardness: 7 on the Mohs scale. Color: Pale pink to rose red. Luster: Vitreous to greasy. Crystal Structure: Hexagonal (trigonal) crystal system. Cleavage: Poor/indistinct. Specific gravity: 2.65.

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

Identified March 20, 2026More mineral →

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Physical properties

Hardness: 7 on the Mohs scale. Color: Pale pink to rose red. Luster: Vitreous to greasy. Crystal Structure: Hexagonal (trigonal) crystal system. Cleavage: Poor/indistinct. Specific gravity: 2.65.

Formation & geological history

Formed in pegmatites, usually in large hydrothermal veins. It crystallizes at high temperatures during the cooling of molten rock. Common in rocks dating from the Precambrian to Cenozoic eras.

Uses & applications

Commonly used in large quantities for ornamental carvings, semi-precious jewelry (beads and cabochons), and as a populat stone for mineral collectors and crystal healing enthusiasts.

Geological facts

Unlike clear quartz, rose quartz rarely forms large, well-defined single crystals; it is usually found in massive form. The pink color is often sensitive to light and can fade over time with excessive UV exposure.

Field identification & locations

Identify in the field by its distinct pink translucent color, its lack of clear crystalline faces, and its ability to scratch glass. Widely found in Brazil, South Africa, Madagascar, and the United States (South Dakota).