
mineral
Tumbled yellow quartz (likely citrine or iron-stained quartz)
Quartz, silicon dioxide (SiO₂), colored yellow by iron impurities; possibly heat-treated amethyst
AI-generated identification · may be incorrectMohs hardness 7; translucent honey-yellow color, vitreous luster, and conchoidal fracture. Quartz is trigonal and lacks cleavage; the rounded shape indicates tumbling or natural abrasion.
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Physical properties
Mohs hardness 7; translucent honey-yellow color, vitreous luster, and conchoidal fracture. Quartz is trigonal and lacks cleavage; the rounded shape indicates tumbling or natural abrasion.
Formation & geological history
Quartz crystallizes from silica-rich hydrothermal fluids and igneous rocks, commonly in cavities and veins; its age depends on the host rock. Yellow coloration commonly results from iron staining or irradiation/heat treatment.
Uses & applications
Used as a lapidary and jewelry stone, ornament, and inexpensive collector specimen; polished pieces are widely sold as citrine. It has modest value unless strongly colored, transparent, and natural.
Geological facts
True natural citrine is relatively uncommon; much commercial “citrine” is heat-treated purple amethyst. The photograph alone cannot reliably distinguish citrine from yellow glass, resin, or treated quartz.
Field identification & locations
Check for glassy luster, hardness, and irregular internal veils; quartz should scratch ordinary glass but not be scratched by a steel knife. Common sources include Brazil, Madagascar, Uruguay, and Spain.
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