
mineral
Tumbled yellow chalcedony (likely yellow jasper or citrine-colored quartz)
Microcrystalline quartz, SiO₂; coloration may come from iron oxides or fine inclusions
AI-generated identification · may be incorrectSmooth, opaque-to-translucent yellow oval with a waxy-to-dull luster; quartz hardness is about 7 Mohs, lacks visible cleavage, and has a microcrystalline structure. The image cannot reliably distinguish chalcedony, jasper, dyed material, or glass.
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Physical properties
Smooth, opaque-to-translucent yellow oval with a waxy-to-dull luster; quartz hardness is about 7 Mohs, lacks visible cleavage, and has a microcrystalline structure. The image cannot reliably distinguish chalcedony, jasper, dyed material, or glass.
Formation & geological history
Chalcedony forms when silica-rich groundwater fills cavities and fractures, commonly in volcanic rocks; iron staining produces yellow tones. Formation ages vary widely, from relatively young cavities to ancient Paleozoic and older deposits.
Uses & applications
Used as a lapidary and decorative stone, cabochon, bead, and inexpensive collector specimen; polished pieces have modest jewelry value.
Geological facts
Chalcedony is cryptocrystalline quartz composed of intergrown quartz varieties. A scratch test, specific-gravity test, and close inspection for bubbles or dye concentration are needed for confident identification.
Field identification & locations
Common sources include Brazil, Uruguay, India, Madagascar, Mexico, and the western United States. It should resist scratching by a steel knife; glass-like bubbles or perfectly uniform color may indicate an imitation.
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