Rock Identifier
Carnelian and turquoise beads (Carnelian: orange-red chalcedony (microcrystalline SiO₂); turquoise: hydrated copper aluminum phosphate, CuAl₆(PO₄)₄(OH)₈·4H₂O) — gemstone
gemstone

Carnelian and turquoise beads

Carnelian: orange-red chalcedony (microcrystalline SiO₂); turquoise: hydrated copper aluminum phosphate, CuAl₆(PO₄)₄(OH)₈·4H₂O

AI-generated identification · may be incorrect

The upper bead appears reddish-orange, translucent to opaque, with a waxy luster and Mohs hardness 6.5–7. The lower blue-green bead is opaque, waxy, commonly Mohs 5–6, with a cryptocrystalline aggregate structure; both are polished and shaped.

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Physical properties

The upper bead appears reddish-orange, translucent to opaque, with a waxy luster and Mohs hardness 6.5–7. The lower blue-green bead is opaque, waxy, commonly Mohs 5–6, with a cryptocrystalline aggregate structure; both are polished and shaped.

Formation & geological history

Carnelian forms when iron colors chalcedony in silica-rich volcanic cavities or sedimentary veins, commonly during the Cenozoic and older geologic periods. Turquoise forms as a secondary mineral in arid, oxidized copper deposits, generally over millions of years.

Uses & applications

Used for beads, cabochons, carvings, and jewelry; turquoise is also valued ornamentally and culturally. These small polished pieces are likely commercial jewelry components.

Geological facts

Carnelian’s color comes mainly from iron oxides. Natural turquoise often shows brown or black matrix veining, while vivid, uniformly colored material may be stabilized or dyed.

Field identification & locations

Identify carnelian by its glassy-to-waxy orange-red appearance and lack of cleavage; turquoise by its blue-green color, soft waxy surface, and copper-associated setting. Common sources include India, Brazil, Uruguay, Iran, Arizona, Nevada, and China.