Rock Identifier
Turquoise-colored bead necklace, likely dyed howlite or magnesite (Possibly dyed CaCO₃ (howlite) or MgCO₃ (magnesite); turquoise is CuAl₆(PO₄)₄(OH)₈·4H₂O) — mineral
mineral

Turquoise-colored bead necklace, likely dyed howlite or magnesite

Possibly dyed CaCO₃ (howlite) or MgCO₃ (magnesite); turquoise is CuAl₆(PO₄)₄(OH)₈·4H₂O

AI-generated identification · may be incorrect

Opaque, polished blue-green beads with a glossy luster; hardness and crystal structure cannot be identified from the image. The uniform color and lack of visible matrix make imitation or dyed material plausible.

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Physical properties

Opaque, polished blue-green beads with a glossy luster; hardness and crystal structure cannot be identified from the image. The uniform color and lack of visible matrix make imitation or dyed material plausible.

Formation & geological history

If genuine turquoise, it forms as a secondary copper phosphate in arid-zone weathering deposits, commonly in old, geologically variable deposits. The beads are cut and polished; their material cannot be confirmed visually.

Uses & applications

Jewelry and ornamental use; genuine turquoise is also collected and sometimes used in decorative inlay.

Geological facts

Turquoise is a hydrated copper-aluminum phosphate; its color ranges from sky blue to green and may include brown or black matrix veining.

Field identification & locations

The photograph does not establish whether these are turquoise or dyed substitutes. Look for natural matrix and variation, and use gemological testing or seller documentation; common sources of genuine turquoise include the southwestern United States, Iran, and China.