


Abstract: Procedures for identifying growth planes, growth zones and twin planes in optical biaxial gemstones are described and the most commonly observed interfacial angles are tabulated, using chrysoberyl as an example. The strong pleochroism of the chromium-bearing chrysoberyl variety alexandrite was found to be a useful indicator for locating the positions of the crystallographic axes, and the optic axes are determined using interference fi gures
under crossed polarizers. Examples of the typical features of growth zoning in natural alexandrites from Russia, Sri Lanka and Brazil are shown. Twinned chrysoberyls from Madagascar are described in detail.
All the Journal articles placed online in 2011 will also be published in hard copy as a single Journal issue and sent to all paid-up Gem-A members early in 2012 as part of their 2011 subscription. Gem-A members may login to the membership area to view the full articles.