
mineral
Amazonite
KAlSi3O8 (Potassium Aluminum Silicate)
Hardness: 6-6.5 (Mohs scale); Color: green to blue-green (due to trace lead content); Luster: vitreous (pearly on cleavage planes); Crystal Structure: Triclinic; Cleavage: perfect in two directions at nearly 90 degrees; Specific Gravity: 2.56-2.58
- Hardness
- 6-6
- Color
- green to blue-green (due to trace lead content)
- Luster
- vitreous (pearly on cleavage planes)
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Physical properties
Hardness: 6-6.5 (Mohs scale); Color: green to blue-green (due to trace lead content); Luster: vitreous (pearly on cleavage planes); Crystal Structure: Triclinic; Cleavage: perfect in two directions at nearly 90 degrees; Specific Gravity: 2.56-2.58
Formation & geological history
Found in granitic pegmatites and metamorphic rocks that have undergone hydrothermal alteration. It often forms through slow cooling of potassium-rich magma, allowing for the development of characteristic white streaking (perthite).
Uses & applications
Primarily used as a gemstone in necklaces, bracelets, and rings. Also used for ornamental carvings, interior decoration, and as a popular specimen for mineral collectors.
Geological facts
Amazonite is named after the Amazon River, although no deposits are actually found there. It is the green variety of Microcline feldspar. Its color was long believed to be caused by copper, but modern research indicates trace amounts of lead and water are the true cause.
Field identification & locations
Identify by its unique blue-green hue and white grid-like streaks (perthitic textures). Common locations include the Pikes Peak area in Colorado (USA), Madagascar, Russia, and Brazil. Collectors look for intense color and sharp crystal faces.
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Mineral/Rock
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mineral