Rock Identifier
Rose Quartz (Silicon Dioxide (SiO2) with trace amounts of titanium, iron, or manganese) — mineral
mineral

Rose Quartz

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

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

Hardness
7 (Mohs scale)
Color
Pink to rose red
Luster
Vitreous/glassy
Identified More mineral
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Physical properties

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

Formation & geological history

Typically found in pegmatite veins formed through the slow cooling of magma. The pink hue is caused by microscopic inclusions of dumortierite or other related minerals within the quartz matrix.

Uses & applications

Extensively used in jewelry (beads, cabochons), ornamental carvings, decorative figurines, and as a popular specimen for crystal healing and mineral collectors.

Geological facts

Unlike other varieties of quartz, rose quartz rarely forms well-defined crystals and typically occurs as massive aggregates. It can exhibit asterism (a star effect) when inclusions are properly oriented.

Field identification & locations

Identified by its distinctive pink color, glassy luster, and lack of cleavage. Common in Brazil, Madagascar, South Africa, and the United States (South Dakota). Look for its characteristic conchoidal fracture.