mineral

Pink quartz crystal (likely rose quartz)

Quartz, silicon dioxide (SiO₂), possibly rose quartz

AI-generated identification · may be incorrect

Pale pink, translucent, vitreous luster, and irregular crystal faces; quartz has Mohs hardness 7, hexagonal crystal structure, no cleavage, and specific gravity about 2.65. The rounded, frosted appearance may reflect abrasion or minor surface coating/weathering.

Identified August 17, 2026More mineral →

Explore Pink quartz crystal (likely rose quartz) in the encyclopedia →

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Physical properties

Formation & geological history

Rose quartz forms mainly in silica-rich pegmatites and hydrothermal veins, crystallizing as granite-related material during Precambrian to younger geological episodes. The image alone cannot establish an exact locality or age.

Uses & applications

Used for carvings, beads, decorative stone, and inexpensive jewelry; transparent, well-formed pink quartz crystals are collected but are less common than massive rose quartz.

Geological facts

The pink color commonly results from microscopic inclusions or lattice defects rather than a simple impurity. Natural rose quartz usually occurs massive, while distinct crystals are more characteristic of pink quartz varieties.

Field identification & locations

Test hardness against glass or a steel file cautiously; quartz should scratch glass and show no cleavage. Common sources include Brazil, Madagascar, India, South Africa, and the United States; confirm identity with a loupe and locality information.