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 April 14, 2026More 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 at high temperatures in deep-seated pegmatites and hydrothermal veins. Its pink color is typically caused by microscopic inclusions of fibrous dumortierite or similar minerals within the quartz.

Uses & applications

Used primarily in lapidary work for cabochons, beads, and carvings. Also popular in the gemstone and jewelry trade, and highly sought after by mineral collectors and practitioners of metaphysics.

Geological facts

Rose quartz rarely forms visible crystal faces; it almost always occurs as massive chunks. Large deposits are found in Brazil, South Africa, and Madagascar. The pink color can fade if exposed to prolonged intense sunlight.

Field identification & locations

Identify in the field by its distinctive pink color, 'greasy' or vitreous luster, and lack of cleavage. It is harder than glass (it will scratch glass) and lacks the geometric crystal habit of typical clear quartz.

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