mineral

Rose quartz

Quartz, silicon dioxide (SiO₂), pink massive variety

AI-generated identification · may be incorrect

Pale pink, translucent to nearly opaque, with a vitreous to slightly greasy luster and irregular fracture; Mohs hardness 7, no cleavage, trigonal crystal structure. The rough, blocky texture is consistent with massive quartz rather than well-formed crystals.

Identified September 14, 2026More mineral →

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Physical properties

Formation & geological history

Forms mainly in granitic pegmatites and hydrothermal quartz veins, with its pink color commonly linked to microscopic inclusions or trace elements. Quartz is geologically widespread and occurs from Precambrian rocks to modern hydrothermal systems.

Uses & applications

Used for carvings, ornamental stone, beads, cabochons, and inexpensive jewelry; massive pieces are also collected as mineral specimens.

Geological facts

Rose quartz commonly lacks visible crystal faces and is typically paler and cloudier than crystalline quartz varieties. Its pink color can fade with prolonged heat or strong sunlight.

Field identification & locations

Identify by its pink color, glassy luster, hardness, lack of cleavage, and ability to scratch ordinary glass; it should not fizz in dilute acid. Common sources include Brazil, Madagascar, India, South Africa, and the United States.