
mineral
Amazonite
Amazonite (Microcline Feldspar) K(AlSi3O8)
AI-generated identification · may be incorrectHardness: 6-6.5 on Mohs scale; Color: Blue-green to turquoise; Luster: Vitreous to pearly; Crystal Structure: Triclinic; Cleavage: Perfect in two directions at nearly 90 degrees; Specific Gravity: 2.56-2.58.
- Hardness
- 6-6
- Color
- Blue-green to turquoise
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 6-6.5 on Mohs scale; Color: Blue-green to turquoise; Luster: Vitreous to pearly; Crystal Structure: Triclinic; Cleavage: Perfect in two directions at nearly 90 degrees; Specific Gravity: 2.56-2.58.
Formation & geological history
Formed in plutonic rocks, primarily granitic pegmatites. The green color is caused by trace amounts of lead and water within the feldspar structure. Found in ancient metamorphic and igneous terrains.
Uses & applications
Commonly used as a gemstone for jewelry, beads, and cabochons. It is also a popular collector's specimen and is sometimes used in ornamental carvings.
Geological facts
Named after the Amazon River, though it is not actually found there; the name likely comes from confusion with other green stones. It was used in Ancient Egypt for jewelry andamulets, including being found in King Tutankhamun's tomb.
Field identification & locations
Identify in the field by its distinct 'schiller' or pearly sheen and cross-hatched twinning (Perthitic texture) visible on cleavage surfaces. Commonly found in Colorado (USA), Brazil, Russia, and Madagascar.
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Epidote
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Granite
Granite (Phaneritic intrusive igneous rock)
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