
mineral
Yellow chalcedony (likely lemon agate or yellow jasper)
Microcrystalline quartz, SiO₂; possibly iron-bearing jasper or chrysoprase-like chalcedony
AI-generated identification · may be incorrectPolished/tumbled, translucent to opaque yellow with a waxy-to-glassy luster and no visible cleavage; quartz hardness is about Mohs 6.5–7, with specific gravity near 2.6. The rounded shape and polish indicate a processed geological specimen.
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Physical properties
Polished/tumbled, translucent to opaque yellow with a waxy-to-glassy luster and no visible cleavage; quartz hardness is about Mohs 6.5–7, with specific gravity near 2.6. The rounded shape and polish indicate a processed geological specimen.
Formation & geological history
Forms when silica-rich groundwater fills cavities or fractures, depositing cryptocrystalline quartz; yellow coloration commonly comes from iron hydroxides or other impurities. Deposits occur in volcanic and sedimentary terrains, generally from relatively young to ancient silica-forming systems.
Uses & applications
Used for cabochons, beads, carvings, décor, and inexpensive lapidary specimens; durable enough for jewelry but less valuable than fine transparent gemstones.
Geological facts
Chalcedony is quartz made of microscopic intergrowths of quartz varieties. A stronger identification would require translucency, hardness, and possibly a streak or specific-gravity test.
Field identification & locations
Commonly found in Brazil, Madagascar, India, Mexico, Uruguay, and the western United States. Identify by its smooth waxy appearance, lack of cleavage, hardness, and resistance to scratching by steel; avoid confusing it with dyed glass or resin.
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