
mineral
Turquoise-bearing rock (likely turquoise in matrix)
Turquoise, CuAl₆(PO₄)₄(OH)₈·4H₂O; commonly intergrown with limonite, iron oxides, or host rock
AI-generated identification · may be incorrectOpaque blue-green to turquoise material with earthy to waxy luster; Mohs hardness 5–6, triclinic crystal system, usually massive rather than visibly crystalline. The specimen appears porous and matrix-rich, so color and hardness may vary substantially.
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Physical properties
Opaque blue-green to turquoise material with earthy to waxy luster; Mohs hardness 5–6, triclinic crystal system, usually massive rather than visibly crystalline. The specimen appears porous and matrix-rich, so color and hardness may vary substantially.
Formation & geological history
Forms as a secondary mineral in arid, oxidized copper deposits when phosphate-bearing groundwater alters aluminum-rich rock. Most deposits are Cenozoic to relatively young, though turquoise occurrences span broad geological ages.
Uses & applications
Used as a cabochon, beads, carvings, and ornamental stone; historically important in jewelry and amulets. Matrix turquoise is often valued for natural patterns and is also used in collectible mineral specimens.
Geological facts
Common localities include Iran, the southwestern United States, Mexico, China, Chile, and Egypt. Natural turquoise is frequently stabilized with resin, so untreated material is generally more valuable.
Field identification & locations
Identify by its blue-green color, opaque appearance, moderate hardness, low density, and association with brown or gray matrix; avoid confusing dyed howlite or plastic. A laboratory test is needed to confirm composition and treatments.
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