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

Formed in high-temperature silica-rich igneous environments such as pegmatites. The pink color is attributed to microscopic inclusions of fibrous dumortierite or similar minerals. Most deposits are millions of years old.

Uses & applications

Extensively used in jewelry (cabochons, beads), decorative carvings, and as a popular specimen for rock collectors and metaphysical use.

Geological facts

Unlike clear quartz, rose quartz rarely forms well-defined external crystal faces; it is almost always found as a massive, translucent chunk. Its color can fade if exposed to excessive sunlight.

Field identification & locations

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