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 the 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 the Mohs scale
Color
Pale pink to rose red
Luster
Vitreous (glassy)
Identified More mineral
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Physical properties

Hardness: 7 on the 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

Forms in late-stage crystallization of granitic pegmatites. The pink color is often attributed to microscopic inclusions of a fibrous pink mineral similar to dumortierite within the quartz mass.

Uses & applications

Used extensively in jewelry (cabochons, beads), decorative carvings, spheres, and as a popular meditation or 'healing' stone in metaphysical communities.

Geological facts

Unlike clear quartz, rose quartz rarely forms well-defined crystal faces and usually occurs in massive form. Large deposits estimated to be hundreds of millions of years old are found in pegmatite cores.

Field identification & locations

Identify by its characteristic pink hue and translucency. In the field, look for quartz veins or pegmatite outcrops. It can be distinguished from pink calcite by its superior hardness (cannot be scratched by steel).