
mineral
Tumbled rose quartz
Quartz (silicon dioxide, SiO₂), pink variety known as rose quartz
AI-generated identification · may be incorrectMohs hardness 7; pale pink, translucent to cloudy, with a vitreous luster before tumbling and a smooth polish afterward. Trigonal crystal structure; no prominent cleavage, with conchoidal fracture. The specimen appears to be a rounded, polished pebble.
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Physical properties
Mohs hardness 7; pale pink, translucent to cloudy, with a vitreous luster before tumbling and a smooth polish afterward. Trigonal crystal structure; no prominent cleavage, with conchoidal fracture. The specimen appears to be a rounded, polished pebble.
Formation & geological history
Rose quartz forms in silica-rich pegmatites and hydrothermal veins, with its color commonly linked to trace elements or microscopic inclusions. It occurs in Precambrian rocks, though the age of this particular piece cannot be determined from the image.
Uses & applications
Used for beads, ornaments, carvings, and inexpensive jewelry; quartz also has industrial uses in glassmaking and electronics.
Geological facts
Quartz is one of Earth’s most abundant minerals; rose quartz is commonly tumbled to produce smooth, rounded stones.
Field identification & locations
Identify by its pink color, glassy polish, hardness, and lack of obvious cleavage; major sources include Brazil, Madagascar, and South Dakota, USA. The image shows a small tumbled specimen.
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