
mineral
Tumbled blue chalcedony (likely agate or common opal)
Microcrystalline quartz, SiO₂; possibly hydrated silica opal, SiO₂·nH₂O
AI-generated identification · may be incorrectSmooth, rounded, pale blue-gray, translucent, and waxy to glassy; chalcedony has Mohs hardness 6.5–7, while opal is 5.5–6.5. Quartz varieties are trigonal cryptocrystalline and lack visible cleavage; opal is amorphous.
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Physical properties
Smooth, rounded, pale blue-gray, translucent, and waxy to glassy; chalcedony has Mohs hardness 6.5–7, while opal is 5.5–6.5. Quartz varieties are trigonal cryptocrystalline and lack visible cleavage; opal is amorphous.
Formation & geological history
Chalcedony forms when silica-rich groundwater fills cavities and fractures, often in volcanic rocks; opal forms from hydrated silica gels. Precise age and identity cannot be determined from the photograph.
Uses & applications
Used for inexpensive jewelry, cabochons, beads, carvings, and collectors’ specimens; industrial chalcedony is occasionally used as a silica source.
Geological facts
The uniform rounded shape and polished surface indicate human tumbling. Blue coloration may be natural, dyed, or enhanced, and color alone cannot reliably distinguish chalcedony from opal.
Field identification & locations
Common sources include Brazil, Uruguay, Madagascar, India, Mexico, and the western United States. A scratch test, specific-gravity test, and close inspection for banding or play-of-color can help; avoid scratching valuable pieces.
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