defined
in a strong light, while its boundaries are sharpest in small stones.
The effect of the chatoyancy is in great part due to the judicious work
of the lapidary, and usually the greatest possible effect is produced
by the greatest curvature of the surface. Chatoyancy appears only in
the cloudy chrysoberyl, and the cloudiness is due to thousands of
microscopically small cavities within the stone. The influence of the
whims and preferences of royalty on the popularity of gems was
remarkably illustrated by the sudden favour with which chrysoberyl
cat's-eye was invested, when His Royal Highness, the Duke of Connaught,
gave his fiancee a ring set with this stone, which vastly increased the demand for it and caused a corresponding rise in price.
The
Minas Novas district in the northern part of the state of Minas Geraes,
Brazil, is the most prolific producer of chrysoberyl of the finest
colours; most of the specimens are chatoyant. The mineral in this
locality occurs associated with rock crystal, amethyst, red quartz,
green tourmaline, yellowish-red (vinegar) spinel, garnet, euclase and
white and blue topaz. Chrysoberyl is erroneously inden-tified with, and
termed, chrysolite by the Brazil-