Rock Identifier
Yellow chalcedony (likely citrine-colored quartz) (Microcrystalline quartz, SiO₂ (chalcedony); yellow color likely from iron impurities) — mineral
mineral

Yellow chalcedony (likely citrine-colored quartz)

Microcrystalline quartz, SiO₂ (chalcedony); yellow color likely from iron impurities

AI-generated identification · may be incorrect

Mohs hardness 6.5–7; translucent yellow to honey-yellow, waxy to slightly vitreous luster, cryptocrystalline structure, no visible cleavage, conchoidal fracture; specific gravity about 2.60–2.65.

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Physical properties

Mohs hardness 6.5–7; translucent yellow to honey-yellow, waxy to slightly vitreous luster, cryptocrystalline structure, no visible cleavage, conchoidal fracture; specific gravity about 2.60–2.65.

Formation & geological history

Forms when silica-rich groundwater deposits quartz in cavities, fractures, and volcanic rocks; commonly Cenozoic to younger, though chalcedony occurs in rocks of nearly all ages.

Uses & applications

Used as a lapidary material for cabochons, carvings, beads, and decorative objects; attractive translucent pieces may be sold as yellow chalcedony or “honey quartz.”

Geological facts

The specimen appears naturally rough or lightly worn rather than highly polished. Similar-looking yellow materials include lemon quartz, jasper, calcite, and dyed chalcedony.

Field identification & locations

Field clues include waxy luster, translucent edges, hardness sufficient to scratch glass, and conchoidal fracture; it is commonly found in volcanic cavities and silica-rich gravels worldwide, including Brazil, Uruguay, India, Madagascar, and the western United States.