![Decorated turquoise-like bead or mineral pendant (Likely turquoise [CuAl₆(PO₄)₄(OH)₈·4H₂O], possibly dyed composite or blue-green jasper) — mineral](https://media.rock.id/decorated-turquoise-like-bead-or-mineral-661926a6-4a55-4e2f-8883-e37cff87c97f-compressed.jpg)
mineral
Decorated turquoise-like bead or mineral pendant
Likely turquoise [CuAl₆(PO₄)₄(OH)₈·4H₂O], possibly dyed composite or blue-green jasper
AI-generated identification · may be incorrectA small polished, cylindrical blue-green specimen with brown/black matrix and a glossy surface; apparent gold-colored metal fittings are human-made. Turquoise has Mohs hardness 5–6, waxy to subvitreous luster, cryptocrystalline structure, and no visible cleavage.
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Physical properties
A small polished, cylindrical blue-green specimen with brown/black matrix and a glossy surface; apparent gold-colored metal fittings are human-made. Turquoise has Mohs hardness 5–6, waxy to subvitreous luster, cryptocrystalline structure, and no visible cleavage.
Formation & geological history
Natural turquoise forms as a secondary copper-aluminum phosphate in arid, oxidized zones of copper deposits, commonly millions of years old; the pictured item appears shaped and assembled as jewelry. Exact identification and age cannot be established from the photograph.
Uses & applications
Used for beads, cabochons, carvings, and jewelry; lower-grade material is often stabilized, dyed, or reconstructed.
Geological facts
Blue-green color with dark matrix is characteristic of turquoise, but similar appearances occur in dyed howlite, chrysocolla, variscite, and composite materials.
Field identification & locations
Check for natural irregular matrix, moderate softness, and a warm waxy luster; avoid destructive tests because coatings and treatments are common. Major sources include Iran, the southwestern United States, Mexico, and China.