Rock Identifier
Tumbled blue-green stone, likely turquoise or chrysocolla (Turquoise: CuAl₆(PO₄)₄(OH)₈·4H₂O; chrysocolla: hydrated copper silicate) — mineral
mineral

Tumbled blue-green stone, likely turquoise or chrysocolla

Turquoise: CuAl₆(PO₄)₄(OH)₈·4H₂O; chrysocolla: hydrated copper silicate

AI-generated identification · may be incorrect

Opaque blue-green, waxy to subvitreous luster, smooth tumbled surface; typical hardness is Mohs 2–6, depending on species and treatment. The photograph is insufficient to distinguish turquoise from chrysocolla or dyed material.

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Physical properties

Opaque blue-green, waxy to subvitreous luster, smooth tumbled surface; typical hardness is Mohs 2–6, depending on species and treatment. The photograph is insufficient to distinguish turquoise from chrysocolla or dyed material.

Formation & geological history

Copper-bearing minerals formed in arid, oxidized zones above copper deposits, commonly during weathering over millions of years. Major sources include Arizona, Nevada, Iran, China, Chile, and Peru.

Uses & applications

Cut and polished for cabochons, beads, carvings, and inexpensive jewelry; turquoise also has longstanding ornamental and cultural significance.

Geological facts

Turquoise commonly shows brown or black limonite matrix, while chrysocolla is generally softer and may have glassy blue-green color zoning. Color enhancement, stabilization, or dyeing is common in commercial specimens.

Field identification & locations

Check hardness cautiously, avoid scratching the specimen, and use magnification for matrix and polish clues; copper staining and a waxy surface support turquoise-group minerals. Reliable identification requires specific-gravity, hardness, spectroscopy, or chemical testing.