mineral

Rose quartz (probable)

Quartz, SiO₂; pink coloration typically from trace inclusions or irradiation-related defects

AI-generated identification · may be incorrect

Pale to salmon-pink, translucent, and glassy with irregular fracture; visible grains suggest massive rather than well-formed crystals. Hardness 7 Mohs, no cleavage, specific gravity about 2.65; identification is uncertain from imagery alone because the surface appears weathered or coated.

Identified August 12, 2026More mineral →

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Physical properties

Formation & geological history

Forms mainly in silica-rich pegmatites and hydrothermal veins, commonly during late stages of granitic activity. Its age depends on locality, often Precambrian to younger; the specimen’s provenance is unknown.

Uses & applications

Used as an ornamental and lapidary stone, in carvings, beads, cabochons, and inexpensive jewelry; attractive translucent material has modest collector value.

Geological facts

Rose quartz commonly occurs as massive aggregates rather than clear crystal points. Pink color can fade somewhat with prolonged heating or strong light in some specimens.

Field identification & locations

Check for glassy luster, hardness sufficient to scratch ordinary glass, absence of cleavage, and white streak; quartz should not fizz in dilute acid. Common sources include Brazil, Madagascar, India, South Africa, and the United States.