mineral

Rose Quartz

Silicon dioxide (SiO2)

Hardness: 7 Mohs; Color: Pale pink to rosy red; Luster: Vitreous to greasy; Crystal Structure: Trigonal (hexagonal system); Cleavage: None/Conchoidal fracture; Specific Gravity: 2.65

Hardness: 7 Mohs
Color: Pale pink to rosy red
Luster: Vitreous to greasy

Identified May 20, 2026More mineral →

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Physical properties

Hardness: 7 Mohs; Color: Pale pink to rosy red; Luster: Vitreous to greasy; Crystal Structure: Trigonal (hexagonal system); Cleavage: None/Conchoidal fracture; Specific Gravity: 2.65

Formation & geological history

Formed in igneous pegmatites at high temperatures; the pink color is caused by trace amounts of titanium, iron, or manganese, and microscopic inclusions of dumortierite.

Uses & applications

Used primarily in lapidary work, jewelry, stone carvings, ornamental decorations, and is highly popular in the metaphysical and gemstone collecting community.

Geological facts

Rose quartz rarely forms visible crystal faces and usually occurs in massive form. The color can fade over time when exposed to direct sunlight for long periods.

Field identification & locations

Identify by its translucent pink color and hardness (can scratch glass). Commonly found in Brazil, Madagascar, South Africa, and the United States (South Dakota).