
Mineral
Amazonite
Potassium Feldspar (Microcline) - K(AlSi3O8)
Hardness: 6-6.5 on Mohs scale; Color: Turquoise, green, or blue-green; Luster: Vitreous to pearly; Crystal structure: Triclinic; Cleavage: Perfect in two directions; Specific Gravity: 2.56-2.58
- Hardness
- 6-6
- Color
- Turquoise, green, or blue-green
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 6-6.5 on Mohs scale; Color: Turquoise, green, or blue-green; Luster: Vitreous to pearly; Crystal structure: Triclinic; Cleavage: Perfect in two directions; Specific Gravity: 2.56-2.58
Formation & geological history
Formed in plutonic rocks, primarily granitic pegmatities. Its color is attributed to small amounts of lead and water within the feldspar structure. These minerals can be hundreds of millions of years old, often dating to the Precambrian or Paleozoic eras.
Uses & applications
Predominantly used as a gemstone for jewelry (cabochons, beads, carvings) and collected as ornamental mineral specimens. It is also used occasionally in decorative tiles or mosaics.
Geological facts
Named after the Amazon River, though it is not actually found there. The green color was long thought to be due to copper, but modern research suggests it is caused by lead and water impurities acting on the feldspar during irradiation from nearby radioactive minerals.
Field identification & locations
Identify in the field by its distinct teal/green color and 'schiller' effect (shimmering sheen). It is commonly found in the Ilmen Mountains (Russia), Colorado and Virginia (USA), Madagascar, and Brazil. Collectors look for high color saturation and distinct white streaks (exsolution lamellae).
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