
mineral
Amazonite
Potassium Feldspar (Microcline), K(AlSi3O8)
AI-generated identification · may be incorrectHardness: 6–6.5 (Mohs scale); Color: green to bluish-green; Luster: vitreous; Crystal structure: triclinic; Cleavage: perfect in two directions; Specific gravity: 2.56–2.58
- Hardness
- 6–6
- Color
- green to bluish-green
- Luster
- vitreous
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Physical properties
Hardness: 6–6.5 (Mohs scale); Color: green to bluish-green; Luster: vitreous; Crystal structure: triclinic; Cleavage: perfect in two directions; Specific gravity: 2.56–2.58
Formation & geological history
Formed in plutonic rocks, primarily pegmatites and granites, through hydrothermal activity. Often found in pockets where lead impurities and water provide the signature teal color.
Uses & applications
Used primarily as a gemstone for jewelry, ornamental carvings, and a popular specimen for mineral collectors.
Geological facts
It is often called the 'Amazon stone,' though it is not actually found in the Amazon River itself; it was named after the region. Its green color was long thought to be due to copper, but recent research suggests it is caused by trace amounts of lead and water.
Field identification & locations
Identify in the field by its distinct teal/aqua color and white streaks (perthitic texture). Common locations include Brazil, Russia, Ethiopia, and the Pikes Peak region of Colorado, USA.
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