Rock Identifier
Tumbled turquoise-colored agate or chalcedony (Cryptocrystalline quartz (SiO₂), possibly dyed chalcedony; exact identification requires testing) — gemstone
gemstone

Tumbled turquoise-colored agate or chalcedony

Cryptocrystalline quartz (SiO₂), possibly dyed chalcedony; exact identification requires testing

AI-generated identification · may be incorrect

Translucent blue-green body with cloudy beige inclusions and a waxy-to-glassy luster, typical of polished chalcedony. Quartz hardness is about 6.5–7 Mohs, with no visible cleavage and a microcrystalline structure; the strong color may be artificial.

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Physical properties

Translucent blue-green body with cloudy beige inclusions and a waxy-to-glassy luster, typical of polished chalcedony. Quartz hardness is about 6.5–7 Mohs, with no visible cleavage and a microcrystalline structure; the strong color may be artificial.

Formation & geological history

Chalcedony forms when silica-rich groundwater fills cavities and fractures, commonly in volcanic rocks; deposits range from Paleozoic to Cenozoic in age. The specimen has been cut and tumbled, and its blue-green color may result from dye treatment rather than natural formation.

Uses & applications

Used for beads, cabochons, carvings, and decorative objects; attractive tumbled pieces have modest jewelry and collector value.

Geological facts

The rounded shape and polish are human-produced. Dye commonly concentrates in pores, fractures, and surface pits, producing uneven turquoise-blue coloration.

Field identification & locations

Check hardness, translucency, conchoidal fracture, and dye concentration; a streak test, magnification, and refractive-index or spectroscopy testing can distinguish chalcedony from glass or resin. Common sources include Brazil, Uruguay, Madagascar, India, and the United States.