mineral

Rose quartz

Quartz, SiO₂; pink coloration commonly associated with trace elements and microscopic inclusions

AI-generated identification · may be incorrect

Mohs hardness 7; pale pink, translucent to cloudy, vitreous luster, trigonal crystal structure, and no cleavage, with conchoidal fracture. The specimen appears to be a rough, massive piece.

Identified October 15, 2026More mineral →

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Physical properties

Mohs hardness 7; pale pink, translucent to cloudy, vitreous luster, trigonal crystal structure, and no cleavage, with conchoidal fracture. The specimen appears to be a rough, massive piece.

Formation & geological history

Forms in silica-rich pegmatites and hydrothermal veins as quartz crystallizes from cooling fluids; individual deposits span a wide range of geological ages.

Uses & applications

Used for beads, cabochons, carvings, and decorative objects; also collected as a mineral specimen.

Geological facts

Rose quartz is usually massive rather than forming distinct crystals; its color can fade with prolonged exposure to sunlight.

Field identification & locations

Recognize it by its pink color, glassy luster, hardness, and lack of cleavage. Common sources include Brazil, Madagascar, South Africa, and the United States.