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) 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 (glassy) to greasy
Identified More mineral

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Physical properties

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

Formation & geological history

Formed in late-stage igneous pegmatites or hydrothermal veins. The pink color is generally attributed to microscopic inclusions of a pink variety of the borosilicate mineral dumortierite.

Uses & applications

Extensively used for ornamental carvings, faceted gemstones, beads for jewelry, and as a popular specimen for mineral collectors and metaphysical practitioners.

Geological facts

Rose quartz rarely forms well-defined crystal faces and usually occurs in massive aggregate forms. Ancient Egyptians, Greeks, and Romans used rose quartz as talismans and in facial masks to clear complexions.

Field identification & locations

Identify by its characteristic pink hue, high hardness (will scratch glass), and lack of cleavage. Common locations include Brazil, Madagascar, South Africa, and the United States (South Dakota).