Gems in the Smithsonian InstitutionDesautels, Paul E.
History
Gems in the Smithsonian Institution
Desautels, Paul E.
Gems; Precious stones; Smithsonian Institution
With color ranging from shades of yellow and brown through blue-green to
olive, and with a hardness of 8½, chrysoberyl has most of the
characteristics necessary for a fine gem. Rare stones of high-quality
chrysoberyl demand fairly high prices, and they are sought eagerly by
the connoisseur of gemstones.
Chrysoberyl is beryllium aluminate, and thus is closely related to the
gemstone spinel, which is magnesium aluminate. When pure, chrysoberyl is
colorless and relatively uninteresting as a gemstone because of its lack
of color dispersion and its moderate refractive index of 1.75. However,
few pure samples are known, as chrysoberyl normally contains some iron
or chromium in place of aluminum and some iron in place of beryllium. As
a result of such impurities, the color of chrysoberyl my be yellowish,
greenish, or brownish.
Chrysoberyl and beryl are the only important gemstones containing the
element beryllium. The minerals beryllonite, euclase, hambergite, and
phenakite also contain this element, but they are rare and seldom are
seen as cut gems.
[Illustration: One of the finest chrysoberyl cat’s-eyes in existence
is the 58-carat Maharani from Ceylon. (Actual size.)]
The _alexandrite_ variety of chrysoberyl has two colors in delicate
balance, and it changes from a columbine red to an emerald green when
viewed under different light. When viewed in daylight, which is richer
in green, the color balance shifts toward green, and that hue is seen by
the observer. Under artificial light, normally richer in red, the color
balance shifts toward red, and the stone seems to have changed to that
color. This extremely rare stone, named after Czar Alexander II of
Russia, is found only occasionally, in Russia and Ceylon. The Russian
stones, found with emerald in mica schist, tend to be smaller than the
Ceylon stones and have a color change going from emerald green to
violet-red. The Ceylon stones, found as pebbles in gem gravels, have a
color change going from a less-emerald green to a browner red. The
66-carat, record-size alexandrite in the National Collection shows the
color change typical of Ceylon stones. A synthetic stone is commonly
marketed as synthetic alexandrite, but this substitute not only is
man-made but is actually synthetic corundum instead of synthetic
chrysoberyl.
[Illustration: In addition to its fine cat’s-eyes and its
color-changing alexandrite varieties, chrysoberyl occurs in handsome
stones that vary in depth of color. Shown here with an uncut twinned
crystal of gem quality from Brazil are a 46-carat stone from Brazil
(left) and a 121-carat stone from Ceylon. The uncut crystal is a
gift of Bernard T. Rocca, Sr. (Two-thirds actual size.)]
_Cat’s-eye_ chrysoberyl contains myriads of tiny fiberlike channels
arranged in parallel position. When the stone is cut as a cabochon, a
band of light is reflected from the curved top of the stone, producing
an effect that resembles the slit pupil of a cat’s eye.
Public-domain text, read in full here on John Shaqi.
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