mineral

Rose quartz

Quartz (SiO₂), pink variety

AI-generated identification · may be incorrect

Usually pale pink to rose, translucent, and vitreous; Mohs hardness 7, conchoidal fracture, no cleavage, and trigonal crystal structure. The specimen appears rough and granular, though its small size and lighting limit certainty.

Identified September 3, 2026More mineral →

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Physical properties

Formation & geological history

Forms mainly in silica-rich igneous and hydrothermal environments, with pink color commonly caused by microscopic inclusions of dumortierite or related minerals. Rose quartz deposits occur in Precambrian pegmatites and massive quartz bodies.

Uses & applications

Used for beads, carvings, cabochons, ornamental objects, and inexpensive crystal collecting; transparent faceted material is uncommon. This small rough piece has minimal commercial value.

Geological facts

Rose quartz is generally massive rather than forming obvious points, unlike many clear quartz crystals. Its pink color can fade with prolonged strong sunlight or heating.

Field identification & locations

Identify it by pink color, glassy luster, hardness sufficient to scratch ordinary glass, and lack of cleavage; test cautiously because scratching damages specimens. Common sources include Brazil, Madagascar, South Africa, India, and the United States.