Rock Identifier
Turquoise Beads (CuAl6(PO4)4(OH)8·4H2O) — gemstone
gemstone

Turquoise Beads

CuAl6(PO4)4(OH)8·4H2O

Hardness: 5-6 on Mohs scale. Color: Robin's egg blue, greenish-blue, or green. Luster: Waxy to subvitreous. Crystal structure: Triclinic. Cleavage: Perfect in one direction, good in another (rarely seen as crystals are microcrystalline). Specific gravity: 2.60-2.86.

Hardness
5-6 on Mohs scale
Color
Robin's egg blue, greenish-blue, or green
Luster
Waxy to subvitreous
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Physical properties

Hardness: 5-6 on Mohs scale. Color: Robin's egg blue, greenish-blue, or green. Luster: Waxy to subvitreous. Crystal structure: Triclinic. Cleavage: Perfect in one direction, good in another (rarely seen as crystals are microcrystalline). Specific gravity: 2.60-2.86.

Formation & geological history

Formed by the chemical action of descending water rich in copper and aluminum percolating through crustal rocks in arid environments, typically in weathered volcanic or sedimentary rocks.

Uses & applications

Widely used in jewelry making, ornamental carvings, beads, and inlay work.

Geological facts

Turquoise is one of the world's most ancient gem materials, prized by the ancient Egyptians, Native Americans, and Persians as a sacred stone and a symbol of good fortune.

Field identification & locations

Identified by its distinctive blue-green color and typical dark web-like matrix veins. Found in arid regions worldwide including Iran, the southwestern United States, China, and Sinai.