mineral

Rose Quartz

Quartz (Silicon Dioxide - SiO2)

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

Identified April 25, 2026More mineral →

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Physical properties

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

Formation & geological history

Formed in high-temperature silica-rich environments such as pegmatites, hydrothermal veins, and occasionally as a primary mineral in igneous rocks. The pink color is generally attributed to trace amounts of titanium, iron, or manganese.

Uses & applications

Commonly used in jewelry (beads, cabochons), ornamental carvings, meditation/crystal healing practices, and as a raw collector specimen.

Geological facts

Rose quartz rarely forms visible crystals; it is almost always found in massive, chunky aggregates. It has been used in talismans and jewelry for thousands of years, with archaeological evidence spanning back to 7000 BC in Mesopotamia.

Field identification & locations

Identify in the field by its distinct pink hue, hardness (it will scratch glass), and lack of cleavage (it breaks in smooth, curved 'conchoidal' patterns). Commonly found in Brazil, Madagascar, South Africa, and the Black Hills of South Dakota.