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Painite
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Painite is a very rare . It was first found in Myanmar (Burma) by British and gem dealer Arthur C.D. Pain who misidentified it as , until it was discovered as a new gemstone in the 1950s. When it was confirmed as a new mineral species, the mineral was named after him.

The chemical makeup of painite contains , , , , and (CaZrAl9O15(BO3)). The mineral also contains trace amounts of and , which are responsible for Painite's typically orange-red to brownish-red color, Painite history at Caltech. Minerals.gps.caltech.edu. Retrieved on 2012-05-28. similar to . The mineral's rarity is due to zirconium and boron rarely interacting with each other in nature. The crystals are naturally hexagonal, but may also be euhedral or orthorhombic. They also may have no crystalline structure, but usually are accompanied by a crystalline structure. Until late 2004, only two had been cut into faceted gemstones. Ten gemstones that are rarer than diamond. io9.com


Discovery and occurrence
Extensive exploration in the area surrounding , which comprises a large part of the extremely small region the mineral is known to exist in, has identified several new painite occurrences that have been vigorously explored resulting in several thousand new available painite specimens. Painite history at Caltech. Minerals.gps.caltech.edu. Retrieved on 2012-05-28.

File:Painite-266170.jpg|Striated, euhedral painite crystal (size: 0.9×0.8×0.7 cm) File:Painite-255206.jpg| var. on a large painite crystal, , Burma. (size: 3.7×3.1×2.3 cm)


See also
  • List of minerals


External links
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