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 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 More 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

Primarily forms at high temperatures in late-stage silicic igneous rocks like pegmatites and hydrothermal veins. Its pink color is due to microscopic inclusions of pink borosilicate fibers.

Uses & applications

Extensively used in jewelry (beads, cabochons), ornamental carvings, decorative stones, and holistic/spiritual practices. Limited industrial use compared to clear quartz.

Geological facts

Unlike other varieties of quartz, rose quartz rarely forms distinct, well-defined crystals and is mostly found in massive form. The color can fade over time if exposed to prolonged intense sunlight.

Field identification & locations

Identified by its distinctive pale pink color and hardness (it can scratch glass). Commonly found in Brazil, Madagascar, South Africa, and the United States (South Dakota).