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: 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
Pink to rose-red
Luster
Vitreous (glassy)
Identified More mineral
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Physical properties

Hardness: 7 on Mohs scale; Color: Pink to rose-red; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: None/Conchoidal fracture; Specific Gravity: 2.65

Formation & geological history

Primarily formed in pegmatites through the slow cooling of silica-rich magma, often occurring in large hydrothermal veins and massive deposits.

Uses & applications

Extensively used in jewelry making, ornamental carvings, beads, and as a popular collector's specimen for decorative or metaphysical purposes.

Geological facts

The distinctive pink color is caused by microscopic inclusions of fibrous dumortierite-like minerals. Unlike amethyst, it rarely forms distinct crystal faces and is usually found in massive chunks.

Field identification & locations

Identified by its signature pink hue, lack of cleavage, and inability to be scratched by a steel blade. Common locations include Brazil, Madagascar, South Africa, and the United States (South Dakota).