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: Pale pink to rose red; Luster: Vitreous to greasy; Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65

Hardness
7 (Mohs scale)
Color
Pale pink to rose red
Luster
Vitreous to greasy
Identified More mineral

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Physical properties

Hardness: 7 (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 (igneous) or hydrothermal veins. Its color is derived from microscopic mineral inclusions. Common in Precambrian and Palaeozoic formations.

Uses & applications

Used primarily in jewelry, cabochons, ornamental carvings, and home decor. It is also highly popular in metaphysical and mineral collecting communities.

Geological facts

Unlike other varieties of quartz, rose quartz does not usually form well-defined crystal faces. The pink color is light-sensitive and can fade over long exposure to direct sunlight.

Field identification & locations

Identify by its characteristic pink hue, high hardness (scratches glass), andLack of cleavage. Found globally, with major deposits in Brazil, Madagascar, and South Dakota, USA.