Amazonite is a mineral of limited occurrence. Formerly it was obtained almost exclusively from the area of Miass in the Ilmen mountains, 50 miles southwest of Chelyabinsk, Russia, where it occurs in granitic rocks. More recently, high-quality crystals have been obtained from Pike's Peak, Colorado, where it is found associated with smoky quartz, orthoclase, and albite in a coarse granite or pegmatite. Crystals of amazonite can also be found in Crystal Park, El Paso County, Colorado. Other localities in the United States which yield amazonite include the Morefield Mine in Amelia, Virginia. It is also found in pegmatite in Madagascar and in Brazil.
For many years, the source of amazonite's color was a mystery. Naturally, many people assumed the color was due to copper because copper compounds often have blue and green colors. More recent studies suggest that the blue-green color results from small quantities of lead and water in the feldspar.
Gallery of Amazonite specimens
Amazonite from the well-known locality on Pikes Peak, Colorado. Size: 5.5 x 3.1 x 2.5 cm.
Large Amazonite crystal from Konso special woreda, Ethiopia. Size: 16.4 x 11.9 x 8.0 cm.
- Amazonite, Mindat.org
- D. Allen Penick, Jr. and Palmer C. Sweet, Mineral Collecting Sites in Virginia, Virginia Minerals, May 1992, V. 38, No. 2, p. 10 - 11
- Hoffmeister and Rossman (1985). "A spectroscopic study of irradiation coloring of amazonite; structurally hydrous, Pb-bearing feldspar". American Mineralogist 70: 794–804.
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