Rock Identifier
Polished turquoise (Turquoise (hydrated copper–aluminum phosphate; CuAl₆(PO₄)₄(OH)₈·4H₂O), likely with brown limonite matrix) — gemstone
gemstone

Polished turquoise

Turquoise (hydrated copper–aluminum phosphate; CuAl₆(PO₄)₄(OH)₈·4H₂O), likely with brown limonite matrix

AI-generated identification · may be incorrect

Opaque, blue-green to green with dark brown/black matrix veining; waxy to dull luster and typically cryptocrystalline structure. Mohs hardness is 5–6; no prominent cleavage; specific gravity about 2.6–2.9. The rounded, glossy surface indicates tumbling or polishing.

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Physical properties

Opaque, blue-green to green with dark brown/black matrix veining; waxy to dull luster and typically cryptocrystalline structure. Mohs hardness is 5–6; no prominent cleavage; specific gravity about 2.6–2.9. The rounded, glossy surface indicates tumbling or polishing.

Formation & geological history

Forms as a secondary phosphate mineral in arid, oxidized zones of copper deposits, commonly replacing aluminum-rich rock. Most deposits are Cenozoic to older, with major sources in Iran, the southwestern United States, China, Chile, and Mexico.

Uses & applications

Used for cabochons, beads, carvings, and ornamental objects; historically important in jewelry and ceremonial art. It has limited industrial use.

Geological facts

Color depends on copper, iron, and water content: iron commonly shifts turquoise toward green. Brown matrix is usually iron oxide minerals such as limonite, though host-rock patterns can vary.

Field identification & locations

Identify by its opaque blue-green color, low-to-moderate hardness, waxy polish, and copper response; a streak, hardness, or chemical test should be done inconspicuously because dyed imitations and stabilized turquoise are common. Similar-looking chrysocolla, variscite, and dyed howlite are alternatives.