mineral

Honey-colored quartz (likely citrine or iron-stained quartz)

Quartz, SiO₂; the yellow coloration may come from iron impurities

AI-generated identification · may be incorrect

Small translucent yellow-to-amber fragment with a vitreous luster and irregular fracture; quartz has Mohs hardness 7 and a trigonal crystal structure, with no cleavage. The image is too small to confirm whether it is citrine or another stained quartz variety.

Identified October 16, 2026More mineral →

Explore Honey-colored quartz (likely citrine or iron-stained quartz) in the encyclopedia →

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Physical properties

Formation & geological history

Quartz crystallizes from silica-rich fluids in veins and cavities, or forms in igneous and metamorphic rocks. Its age depends on its host deposit; iron staining may develop later through weathering.

Uses & applications

Quartz is widely used in glass, electronics, abrasives, and construction; attractive transparent pieces may be cut as gemstones. This fragment appears too small for typical commercial use.

Geological facts

Natural citrine is relatively uncommon; much commercial citrine is heat-treated amethyst. Yellow color alone cannot distinguish citrine from iron-stained quartz or other minerals.

Field identification & locations

Check for glassy luster, hardness near 7, and lack of cleavage; a scratch test or closer inspection of crystal faces can help distinguish quartz from softer amber-colored minerals. Quartz occurs worldwide, especially in veins and pegmatites.