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Gemstones
Gemstones are minerals that are treasured for their beauty and durability.
A large number of minerals have been used as gems. Their value generally
depends on four elements: the beauty of the stone itself; its rarity;
its hardness and toughness; and the skill with which it has been cut and
polished. Stones such as diamonds, rubies, and emeralds represent one
of the greatest concentrations of money value. During times of war or
economic disturbance many people convert their wealth into precious stones,
which are transportable and more easily sold.
Optical
Properties
The beauty of gems depends to a large extent on their optical properties.
The most important optical properties are the degree of refraction and
color. Other properties include fire, the display of prismatic colors;
dichroism, the ability of some gemstones to present two different colors
when viewed in different directions; and transparency. Diamond is highly
prized because of its fire and brilliancy, ruby and emerald because of
the intensity and beauty of their colors, and star sapphire and star ruby
because of the star effect, known as asterism, as well as for their color.
In certain gemstones, notably opals, brilliant areas of color can be seen
within the stone; these areas change in hue and size as the stone is moved.
This phenomenon, known as play of color, differs from fire and is caused
by interference and reflection of the light by tiny irregularities and
cracks inside the stone. Opals also exhibit milky or smoky reflections
from within the gem. Gems that are fibrous in structure show irregular
interior reflections similar to those seen on watered or moiré silk. This
optical property, which is called chatoyancy, is exhibited by several
gems, notably the tigereye and cat's-eye. The appearance of a gem as seen
by reflected light is another optical property of gemstones and is called
luster. The luster of gems is characterized by the terms metallic, adamantine
(like the luster of the diamond), vitreous (like the luster of glass),
resinous, greasy, silky, pearly, or dull. Luster is particularly important
in the identification of gemstones in their uncut state.
Identification
of Gems
A gem cannot always be identified by sight alone. It is therefore necessary
to rely on measurement of the optical properties that can be determined
without harming the stone in any way. The gemologist uses an instrument
called a refractometer to measure the characteristic property of the stone,
known as refractive index, which is its relative ability to refract light.
In addition, an instrument called the polariscope is employed to determine
whether a gem is doubly or singly refracting (see Crystal). Emeralds,
rubies, sapphires, amethysts, and synthetic rubies and sapphires are all
doubly refracting, whereas diamonds, spinels, synthetic spinels, garnets,
and glass are singly refracting. A special dark-field illuminator with
a binocular microscope is employed for examining the interior of a gemstone
to determine whether it is of natural or artificial origin, and to search
for inclusions characteristic of a given gemstone. These tests usually
are sufficient to identify the rather limited number of materials used
as gemstones; occasionally, however, other instruments are required, including
a dichroscope, which measures the property called dichroism, or a spectroscope
to determine the characteristic absorption spectra (see Spectroscopy;
Spectrum). Hardness, the test ordinarily associated with gem testing,
is never used on cut stones by the gemologist. Another physical test that
can be given to an unknown stone is the determination of its specific
gravity (see Density). For exact determinations various weighing devices
are used, but rough approximations of the specific gravity of lighter
stones can be made by means of a series of liquids of known specific gravity.
If the stone will float in a liquid having a specific gravity of 4 and
sink in a liquid with a specific gravity of 3, the specific gravity of
the stone must lie between these limits and be approximately 3.5.
Gem
Materials
The accompanying table lists precious and semiprecious gem minerals with
the names commonly applied to them. See separate articles on many of the
gems mentioned. V. Artificial Gems The term artificial gem is used to
describe either an imitation of a natural gemstone or a synthetic gem
that is chemically identical to naturally occurring gems. A. Imitation
Gem Such a gem may be made of flint glass, often silvered on the back
to increase the brilliance. Since World War II, colored plastics have
replaced glass, especially in costume jewelry. Plastics are cheaper, more
easily molded, and lighter in weight. During the 19th century, artificial
pearls were made by blowing hollow beads of glass and pouring into them
a mixture of liquid ammonia and the white matter from the scales of fish
such as the bleak, roach, or dace. A much better type of artificial pearl,
the indestructible bead, was introduced shortly after 1900. The bead is
made of solid glass with only a narrow hole for the thread. Pearl essence,
consisting of the crushed scales of certain herring, is applied to the
outside of the glass and covered with a transparent, colorless lacquer.
The most successful imitation of a diamond is strontium titanate, made
by a flame-fusion technique. Its index of refraction is almost identical
to that of a diamond, and it has a higher dispersion. Thus, it has the
brilliance and greater fire than the diamond. It scratches easily, however.
A harder material simulating the diamond is rutile, or titanium oxide.
B. Synthetic Gems The term is limited by the U.S. Federal Trade Commission
to manufactured materials that duplicate a natural gemstone chemically,
physically, and optically. Synthetic gems can be distinguished under a
microscope because they are more perfect than natural gemstones and contain
no irregularities. Synthetic diamonds were first made by the General Electric
Company in the U.S. in 1955. In their process, carbonaceous compounds
are subjected to pressures of 56 metric tons per sq cm (360 metric tons
per sq in) at temperatures of 2760° C (5000° F). The diamonds thus produced
are suitable only for industrial use. In the late 1960s a method was developed
for "growing" diamonds by heating a diamond particle to a high temperature
and subjecting it to methane gas. The gas decomposes into carbon atoms,
which adhere to the diamond crystal. The crystal structure of the enlarged
diamond is identical to that of a natural diamond. Diamonds of about 1
carat (200 mg or 0.007 oz) have been produced by this method, but their
cost is still considerably higher than that of naturally occurring diamonds.
Sapphires are made in an apparatus resembling an oxyhydrogen torch. The
flame is directed into a fireclay support inside an insulated chamber.
The oxygen gas carries finely powdered pure aluminum oxide into the flame,
and the powder fuses into droplets, forming a cylindrical boule, or matrix,
on the support. The size of the resulting sapphire is controlled by varying
the gas flow, temperature, and amount of powder. Boules weighing up to
200 carats (40 g or 1.41 oz) can be produced by this technique. Perfect
rubies and sapphires up to 50 carats (10 g or 0.353 oz) have been cut
from such a boule. Rubies are made by the same process by adding 5 to
6 percent chromium oxide to the aluminum oxide. Colors other than red
are produced by adding different metallic oxides. Stars can be added to
synthetic rubies or sapphires by adding an excess of titanium oxide to
the aluminum oxide powder and heating to temperatures greater than 1000°
C (greater than 1832° F). In gems made with this technique, synthetic
stars appear sharper than naturally occurring stars. Emeralds, some of
which are of gem quality, are synthesized by still-secret methods. They
can be distinguished from natural emeralds by their red glow under ultraviolet
light.
Gem
Cutting
The shaping and polishing of gem materials to enhance their beauty and,
in some cases, to remove imperfections is performed by expert workers
known as lapidaries. Their trade, although highly skilled, is not as exacting
as that of the diamond cutter.
- Materials and Equipment
Gems are shaped
entirely by being ground on abrasive wheels or revolving abrasive
disks. For minerals that are no harder than quartz, natural sandstone
wheels are sometimes used, but for the harder stones, such as rubies
and sapphires, synthetic grinding wheels of cemented Carborundum (silicon
carbide) must be employed. The first step in the cutting of a gem
is to saw it roughly to shape. Thin abrasive disks or metal disks
charged with powdered diamond or other abrasives are employed in this
process. Wheels (called laps) made of Carborundum or of abrasive-charged
cast iron are used to shape the stone. The stone to be shaped is cemented
to the end of a wooden stick called a dop and is held against the
revolving wheel or lap with the aid of a supporting block placed adjacent
to the wheel. This supporting block contains a number of holes in
which the end of the dop can be rested. By changing the dop from one
hole to another the lapidary is able to control the angle of the facet,
or face, being ground. When the stone has been ground to the required
shape, it is brought to a high polish on wooden or cloth wheels charged
with a fine abrasive such as rouge or tripoli powder.
- Gem Cuts The
oldest and simplest of the many standardized shapes or cuts given
to gemstones is the cabochon cut, in which the stone is smoothly rounded.
The cabochon cut is essential if a star or cat's-eye is to be visible,
and is the most satisfactory cut for opal, moonstone, and colorful
opaque gems. Cabochon-cut stones usually are rounded on the back;
this is sometimes advantageous in improving appearance, but often
is done in order to give the stone extra weight. Various forms of
faceted cuts, in which the gem is given a number of symmetrical plane
surfaces, or facets, are universally employed in the cutting of diamonds
and are used extensively for other stones as well. The most common
cut is the brilliant. In this cut the top of the stone is ground to
a flat so-called table from which the sides of the stone slope outward
to the broadest portion of the stone, which is known as the girdle.
Below the girdle, the sides slope inward at a slightly broader angle
to a tiny flat surface, the culet, parallel to the table at the bottom
of the stone. The ordinary brilliant-cut stone has 32 facets besides
the table in the top portion of the stone (called the crown or bezel)
above the girdle, and 24 facets besides the culet on the bottom portion
of the stone (called the pavilion or base) below the girdle. In rare
cases the number of facets is increased by some multiple of 8. Scientific
studies have worked out proportions of the size and inclination of
the facets that give the maximum brilliance to a given gem. In addition
to the round brilliant, stones are cut in a variety of square, triangular,
diamond-shaped, and trapezoidal faceted cuts. The use of such cuts
is largely determined by the original shape of the stone. Large rubies,
sapphires, and emeralds are often cut square or rectangular with a
large table facet surrounded by a relatively small number of supplementary
facets. The emerald cut, which is frequently also used for diamonds,
resembles the brilliant, but has a large square or rectangular facet
at the top and a total of 58 facets in all, although more or less
facets may be used, again added or subtracted in multiples of 8.
Gem
Engraving
Designs are cut in precious or semiprecious stones either as cameos, in
which the design is raised in relief above the surface, or as intaglios,
in which the design is incised into the surface. Intaglios were formerly
often used as seals for making impressions on wax or damp clay. The technique
of gem engraving requires, on all hard stones, the use of a rotating metal
tool. The stone is fastened to a wooden handle and moved against the tool,
which does not itself perform the cutting of the design but merely rubs
abrasive powder on the stone. The ancients probably used emery powder
for this purpose, but since Roman times the abrasive has been a mixture
of diamond dust with oil. A. Ancient Engraving Intaglio cutting probably
started during the 4th millennium BC, in Mesopotamia, during the Elamite
and Sumerian civilizations. The first seals, made of stone, were usually
cylindrical and were suspended on a cord. The art reached its peak about
2800 BC, in elaborate cuttings on cylindrical rock crystal; these commonly
dealt with the adventures of the mythical king Gilgamesh. By the 1st millennium
BC the art had spread throughout Asia Minor and Egypt. Although the cylindrical
form was still common, domed and conical seals with flat surfaces for
the intaglios became popular. The Egyptians initially adopted the cylinder
but later produced seals of various shapes, including that of the scarab
beetle, often cut in one of the colored quartzes, such as amethyst, carnelian,
or jasper. Unlike the people of Asia Minor, they engraved symbols rather
than pictorial scenes. Although the Egyptians made use of the quartzes
for their engravings, the most popular material for the making of seals
was glazed earthenware. The earliest Cretan gems were carved in soft steatite,
but by about 1700 BC harder stones such as chalcedony were employed. The
engraving of seals for the bezels of rings was first practiced about 1100
BC. The carvings on the gems of Greece and Rome provide a complete miniature
history of the art of every period during which they were made. The Greek
gems of the 6th century BC were cut in agate, carnelian, and chalcedony;
by the 4th century BC the last had become the most popular material, although
lapis lazuli, agate, jasper, and rock crystal were also employed. Gems
of the Hellenistic period, dating from about 330 BC, were cut in a large
variety of stones, including garnet, beryl, topaz, sard, agate, and amethyst.
The use of glass as a substitute for more precious stones was introduced
about this time. The cameo, usually made of one of the layered quartzes
(such as sardonyx) or in colored glass, made its first appearance in Hellenic
Greece and was brought to a high artistic level by the Roman craftsmen.
The cameo was commonly employed in articles of personal adornment, such
as brooches or clasps. The intaglio gems of Rome were usually used as
the bezels of rings. B. Revival in Europe By the 2nd century AD gem engraving
had declined in Asia Minor, the best examples being talismans produced
by the adherents of the Gnostic heresy. They are frequently connected
with the symbolism attached to the worship of Mithras. In Europe a limited
number of gems were engraved, usually for bishops' rings, until the 7th
century, but the art then declined until the end of the 14th century,
when Florentine and German engravings made their appearance. In Italy
the art received impetus from the ardor with which the Medici family collected
gems. Although the artists of the Renaissance based their designs on those
of the Greek and Roman artists, they employed a freedom of interpretation
that made their work individual. On the other hand, the revival of gem
engraving that took place in the 18th and 19th centuries produced works
that so closely resembled the classical originals that it is difficult
to tell them apart.
Contributed by: Gemological
Institute of America
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