
mineral
Pink quartz pebble (likely rose quartz)
Rose quartz, pink quartz; silicon dioxide (SiO₂)
AI-generated identification · may be incorrectMohs hardness 7; pale pink, translucent to opaque, with a vitreous to waxy luster. Quartz has a trigonal crystal structure and no cleavage, though this rounded specimen is tumbled and shows conchoidal fracture surfaces.
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Physical properties
Mohs hardness 7; pale pink, translucent to opaque, with a vitreous to waxy luster. Quartz has a trigonal crystal structure and no cleavage, though this rounded specimen is tumbled and shows conchoidal fracture surfaces.
Formation & geological history
Rose quartz forms mainly in granitic pegmatites and hydrothermal quartz veins, with its color commonly related to microscopic inclusions of minerals such as dumortierite. The specimen’s exact geological age and locality cannot be determined from the image.
Uses & applications
Used as an ornamental stone, beads, carvings, polished pebbles, and inexpensive jewelry; it has little industrial value compared with ordinary quartz.
Geological facts
Rose quartz is usually massive rather than well-crystallized; transparent pink quartz crystals are rarer and may be classified separately as pink quartz.
Field identification & locations
Identify it by its pink color, glassy/waxy surface, lack of obvious cleavage, and hardness sufficient to scratch glass. Common sources include Brazil, Madagascar, India, South Africa, and the United States.
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