Rock Identifier
Blue-green turquoise (probable) (Turquoise — hydrated copper aluminum phosphate, CuAl₆(PO₄)₄(OH)₈·4H₂O) — mineral
mineral

Blue-green turquoise (probable)

Turquoise — hydrated copper aluminum phosphate, CuAl₆(PO₄)₄(OH)₈·4H₂O

AI-generated identification · may be incorrect

Opaque blue-green, typically waxy to dull luster with a cryptocrystalline aggregate structure; Mohs hardness 5–6, no obvious cleavage, and specific gravity about 2.6–2.9. The specimen may also contain matrix or resemble chrysocolla, so visual identification is provisional.

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Physical properties

Opaque blue-green, typically waxy to dull luster with a cryptocrystalline aggregate structure; Mohs hardness 5–6, no obvious cleavage, and specific gravity about 2.6–2.9. The specimen may also contain matrix or resemble chrysocolla, so visual identification is provisional.

Formation & geological history

Forms as a secondary mineral in arid, oxidized copper deposits when phosphate-bearing groundwater alters aluminum-rich rock. Most turquoise is Cenozoic to relatively young geologically, commonly associated with copper mineralization.

Uses & applications

Used as a gemstone, ornamental material, cabochons, beads, and carvings; lesser-grade material is used for specimens and stabilized jewelry. It has substantial cultural importance in Southwestern Native American jewelry.

Geological facts

Common localities include Iran, the southwestern United States, China, Egypt, Chile, and Mexico. Natural turquoise is porous and is often stabilized with resin; dyeing and synthetic imitations are also common.

Field identification & locations

Look for an opaque blue-to-green color, low glassy reflectivity, soft surface, and brown or black host-rock matrix; a streak, hardness, or laboratory test is safer than appearance alone. Avoid prolonged water, chemicals, and oils.