
mineral
Turquoise
Hydrated phosphate of copper and aluminium: CuAl6(PO4)4(OH)8·4H2O
Hardness: 5-6 (Mohs scale), Color: Sky-blue to apple-green, Luster: Waxy to subvitreous, Crystal Structure: Triclinic (usually cryptocrystalline massive), Specific Gravity: 2.6-2.9
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Physical properties
Hardness: 5-6 (Mohs scale), Color: Sky-blue to apple-green, Luster: Waxy to subvitreous, Crystal Structure: Triclinic (usually cryptocrystalline massive), Specific Gravity: 2.6-2.9
Formation & geological history
Secondary mineral formed in the oxidation zones of copper deposits. It results from the percolation of acidic aqueous solutions through aluminous and phosphatic minerals in arid regions.
Uses & applications
Primarily used as an ornamental stone, in jewelry (beads, cabochons), and as a cultural gemstone for various indigenous peoples.
Geological facts
Turquoise is one of the oldest gemstones in history; it was used by Ancient Egyptians as early as 3000 BCE. Its name comes from the French 'pierre turquoise', meaning 'Turkish stone', as it entered Europe via Turkish trade routes.
Field identification & locations
Identify by its unique blue-green color and waxy luster. In the field, look for thin veins or nodules in weathered volcanic or sedimentary rock. Common locations include Iran, Southwestern USA, China, and Egypt.
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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