Rock Identifier
Rose Quartz (Rose Quartz (SiO₂)) — Mineral
Mineral

Rose Quartz

Rose Quartz (SiO₂)

Hardness: 7 (Mohs scale); Color: Pink to rose-red, sometimes varying in intensity; Luster: Vitreous to sub-vitreous; Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65

Hardness
7 (Mohs scale)
Color
Pink to rose-red, sometimes varying in intensity
Luster
Vitreous to sub-vitreous
Identified More mineral

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Physical properties

Hardness: 7 (Mohs scale); Color: Pink to rose-red, sometimes varying in intensity; Luster: Vitreous to sub-vitreous; Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65

Formation & geological history

Rose quartz is a variety of quartz that forms in pegmatites and hydrothermal veins, primarily at elevated temperatures. Its characteristic pink color is believed to be due to microscopic inclusions of dumortierite, or traces of titanium, iron, or manganese, or irradiation-induced color centers. It typically forms large anhedral masses rather than distinct crystals. Geological Age: Varies, often found in ancient granitic pegmatites and hydrothermal deposits worldwide, ranging from hundreds of millions to billions of years old.

Uses & applications

Rose quartz is widely used in jewelry (beads, cabochons, carvings), ornamental objects, and as a decorative stone. It is also a popular specimen for mineral collectors. In holistic practices, it's known as the 'love stone' and used for emotional healing and promoting self-love.

Geological facts

Many of the world's finest rose quartz specimens come from Brazil. Large deposits are also found in the United States (South Dakota), India, South Africa, and Madagascar. Massive rose quartz can be found in sizes ranging from small pebbles to large boulders. The color can fade over time with prolonged exposure to sunlight.

Field identification & locations

In the field, rose quartz is identified by its distinctive pink color, glassy luster, and hardness (it can scratch glass). It typically occurs in massive, anhedral forms within pegmatites or hydrothermal veins. It is commonly found in areas with past volcanic activity and granite intrusions. To distinguish it from other pink minerals, checking its hardness with a streak plate or steel file can be helpful. Its lack of cleavage produces conchoidal (shell-like) fractures when broken. Its translucent to opaque nature and milky turbidity are also key identifiers. The specimen shown, likely a bead bracelet, is typical of faceted and polished rose quartz used in jewelry.