
mineral
Honey-yellow chalcedony (likely common opal or silicified material)
Microcrystalline quartz, SiO₂; possibly hydrated silica opal, SiO₂·nH₂O
AI-generated identification · may be incorrectOpaque honey-orange, waxy to dull luster, irregular fracture, and no visible cleavage; chalcedony has Mohs hardness 6.5–7, while opal is 5.5–6.5. The rounded shape and surface texture suggest a naturally water-worn or roughly polished specimen.
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Physical properties
Opaque honey-orange, waxy to dull luster, irregular fracture, and no visible cleavage; chalcedony has Mohs hardness 6.5–7, while opal is 5.5–6.5. The rounded shape and surface texture suggest a naturally water-worn or roughly polished specimen.
Formation & geological history
Silica-rich groundwater deposited chalcedony or opal in cavities, fractures, or sedimentary settings; such deposits range from Cenozoic to much older. Exact age and identification require hardness, specific-gravity, and microscopic tests.
Uses & applications
Used as a lapidary material, ornamental stone, cabochons, carvings, and collectible specimens; translucent, patterned varieties may have modest jewelry value.
Geological facts
Orange coloration commonly comes from iron oxides or hydroxides. Chalcedony and opal can look similar, but opal is generally softer and less crystalline.
Field identification & locations
Commonly found in volcanic cavities, silica-rich sediments, and alluvial gravels worldwide, including Australia, Mexico, Brazil, and the western United States. A steel-file scratch test, specific gravity, and absence or presence of play-of-color help distinguish it from opal, jasper, and resin.
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