
mineral
Turquoise
CuAl6(PO4)4(OH)8·4H2O (Hydrous phosphate of copper and aluminium)
Hardness: 5-6 Mohs; Color: Sky blue to apple green; Luster: Waxy to subvitreous; Crystal structure: Triclinic (usually cryptocrystalline); Cleavage: Perfect (rarely seen); Specific gravity: 2.6-2.9
- Hardness
- 5-6 Mohs
- Color
- Sky blue to apple green
- Luster
- Waxy to subvitreous
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Physical properties
Hardness: 5-6 Mohs; Color: Sky blue to apple green; Luster: Waxy to subvitreous; Crystal structure: Triclinic (usually cryptocrystalline); Cleavage: Perfect (rarely seen); Specific gravity: 2.6-2.9
Formation & geological history
Secondary mineral formed in the oxidation zones of copper deposits by the percolation of meteoric water through aluminous rock in arid environments.
Uses & applications
Primarily used in jewelry (cabochons, beads, and inlay) and as a highly prized collector specimen; historically used for amulets and decorative ornaments.
Geological facts
One of the first gemstones ever mined, turquoise was highly valued by the Egyptians as early as 3000 BCE and held deep spiritual significance for Native American tribes in the Southwest US.
Field identification & locations
Identify by its distinctive blue-green color and waxy luster; often contains dark matrix veins (limonite or manganese oxide). Commonly found in Iran, Southwestern USA, China, and Egypt.
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Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Schist
Schist
Metamorphic
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Nephrite Jade
Nephrite
Mineral/Rock
Banded Gneiss (River Rock/Pebble)
Gneiss (specifically a banded variety often found as a river rock)
Metamorphic Rock
Green Apatite on Albite
Fluorapatite [Ca5(PO4)3F] on Albite [Na(AlSi3O8)]
mineral