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 to greasy; 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 to greasy
Identified More mineral

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Physical properties

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

Formation & geological history

Formed in late-stage crystallization of pegmatites or in hydrothermal veins at relatively low temperatures. Most specimens are from the Phanerozoic eon, found in igneous rock formations.

Uses & applications

Used primarily in ornamental carvings, jewelry (cabochons and beads), and as a popular semi-precious stone for mineral collectors and metaphysical practitioners.

Geological facts

Rose quartz is famous for its unique pink hue which can fade in sunlight. While most quartz forms distinct crystals, rose quartz is rarely found in crystal form, usually appearing in massive or blocky habits.

Field identification & locations

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