
mineral
Amazonite
K(AlSi3O8) (Microcline Feldspar)
AI-generated identification · may be incorrectHardness: 6-6.5 on Mohs scale; Color: bright blue-green to turquoise; Luster: vitreous to pearly; Crystal structure: triclinic; Cleavage: perfect in two directions; Specific gravity: 2.56-2.58.
- Hardness
- 6-6
- Color
- bright blue-green to turquoise
- Luster
- vitreous to pearly
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Physical properties
Hardness: 6-6.5 on Mohs scale; Color: bright blue-green to turquoise; Luster: vitreous to pearly; Crystal structure: triclinic; Cleavage: perfect in two directions; Specific gravity: 2.56-2.58.
Formation & geological history
Formed in igneous environments, specifically within granitic pegmatites. The green color arises from trace amounts of lead and water within the feldspar structure.
Uses & applications
Primarily used as a gemstone for jewelry, cabochons, and ornamental carvings. It is also a popular specimen for mineral collectors.
Geological facts
Named after the Amazon River, though it is not actually found there. It was historically called 'Amazon Stone'. The color was once thought to be caused by copper, but modern analysis confirmed lead impurities.
Field identification & locations
Look for the characteristic 'schiller' or white streaking within the blue-green matrix. Common locations include the Pikes Peak area of Colorado, USA, as well as Brazil, Russia, and Madagascar.
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