
mineral
Amazonite
Microcline (Potassium Feldspar), KAlSi3O8
AI-generated identification · may be incorrectHardness of 6 on the Mohs scale, color ranges from bright turquoise-green to bluish-green and pale yellow with characteristic white or cream-colored mottled streaks (schiller effect), vitreous to pearly luster, triclinic crystal system, perfect cleavage in two directions at nearly right angles, specific gravity of 2.56…
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Physical properties
Hardness of 6 on the Mohs scale, color ranges from bright turquoise-green to bluish-green and pale yellow with characteristic white or cream-colored mottled streaks (schiller effect), vitreous to pearly luster, triclinic crystal system, perfect cleavage in two directions at nearly right angles, specific gravity of 2.56-2.58.
Formation & geological history
Forms in pegmatites, granitic rocks, and hydrothermal veins where potassium-rich solutions crystallize slowly under high temperatures, often millions of years old.
Uses & applications
Popularly used as a gemstone in beaded jewelry, cabochons, carvings, ornamental objects, and as a collector specimen.
Geological facts
The distinctive green color of amazonite was traditionally attributed to copper, but modern research shows it is caused by trace amounts of lead and water within the feldspar structure.
Field identification & locations
Identified by its characteristic green-to-blue-green color combined with a mottled white grid-like pattern (tartan twinning). Commonly found in the Amazon River region (though sources there are debated), USA, Russia, Madagascar, and Brazil.
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