
mineral
Blue chalcedony cabochon (likely)
Chalcedony, microcrystalline SiO₂; possibly blue agate or common opal, which cannot be distinguished confidently from the image
AI-generated identification · may be incorrectPale blue-white, translucent to opaque, waxy/glassy luster, with dark inclusions. If chalcedony: Mohs 6.5–7, trigonal microcrystalline quartz, no cleavage; the polished cabochon is mounted in a dark setting.
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Physical properties
Pale blue-white, translucent to opaque, waxy/glassy luster, with dark inclusions. If chalcedony: Mohs 6.5–7, trigonal microcrystalline quartz, no cleavage; the polished cabochon is mounted in a dark setting.
Formation & geological history
Chalcedony forms as silica-rich fluids fill cavities and fractures, commonly in volcanic rocks; deposits range from ancient to recent. The image does not establish the specimen’s geological age or locality.
Uses & applications
Cabochons are used in jewelry and decorative objects; chalcedony is also collected as a lapidary material.
Geological facts
Chalcedony is made of microscopic quartz crystals, so it lacks the visible crystal faces of ordinary quartz.
Field identification & locations
Look for hardness near 7, a smooth waxy surface, and conchoidal fracture on an unpolished piece. The mounted stone’s identity and locality cannot be confirmed visually.
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