Rock Identifier
Blue chalcedony cabochon (likely) (Chalcedony, microcrystalline SiO₂; possibly blue agate or common opal, which cannot be distinguished confidently from the image) — mineral
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 incorrect

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.

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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.