GARNET

The name garnet is applied to a group of six closely related silicate

minerals that are alike in crystal structure but that differ mainly in

the substitution of certain metallic elements in their composition.

These minerals are:

_Pyrope_, magnesium aluminum garnet

_Almandine_, iron aluminum garnet

_Spessartine_, manganese aluminum garnet

_Uvarovite_, calcium chromium garnet

_Grossular_, calcium aluminum garnet

_Andradite_, calcium iron garnet

Most natural garnets have compositions intermediate between members of

the basic group of six. For example, there are garnets having

compositions anywhere between pyrope and almandine, depending on the

amount of difference in the magnesium or iron content. These same

garnets may even have varying amounts of manganese, and thus be

partially spessartine.

The six garnets in the basic group are found in considerable quantity in

many areas, but seldom are they of sufficiently high quality to be

considered gemstone material. Even when stones of gem quality are found,

their colors—particularly the reds—tend to be so intense that they seem

to be opaque.

[Illustration: Garnets occur in several colors, although most people

think of them as red. Shown here are a 54-carat spessartine from

Brazil (top right), a 6-carat rhodolite from North Carolina (at

left), a magnificent 10-carat green demantoid from Russia, a 9-carat

grossular from Ceylon (bottom), and a 26-carat spessartine from

Virginia. (Seven-eighths actual size.)]

Garnet has a hardness (about 7) suitable for gemstone material and a

fairly high refractive index (1.74 and above).

Ruby red pyrope is the most popular variety of garnet. It is found in

Bohemia, in Czechoslovakia, where it occurs as small, poorly shaped

crystals. Red pyrope also is found in Africa, where it is called Cape

ruby, and in Arizona, where it is sold as Arizona ruby. Another kind of

pyrope called _rhodolite_ is noted for its soft, rosy purple color.

Actually, rhodolite is one of the intermixed garnets with a composition

somewhere between pyrope and almandine. Most of the fine rhodolite gems

have come from North Carolina.

Almandine is popular in its deep red, transparent form, but since the

red is so dark and intense that it appears black, the stones usually are

cut as cabochons with the back hollowed out. This makes them thinner,

and thus lightens their color. Garnets cut in this manner are all known

as carbuncles. Brazil, India, Ceylon, Australia, and parts of the United

States are important sources of almandine.

Although spessartine has a rich orange color, it is not often used as a

gemstone because of the relative rarity of gem-quality cutting material.

This mineral gets its name from the town of Spessart, Germany, where it

was first found. Excellent spessartine with colors ranging from orange

to brown has been found at Amelia Court House, Va., and quality gems

have been cut from such material. Ceylon, Burma, Madagascar, and Brazil

also have furnished some gem spessartine.

The chromium garnet, uvarovite, generally is too poor in quality for

cutting. Uvarovite crystals, which are emerald green in color, occur in

only small sizes. They are found mostly in Russia, Finland, and

California.

Grossular varies in color. It occurs chiefly in some shade of red,

green, yellow, or brown, depending on the impurities present. When pure,

grossular is colorless. A kind of grossular called _hessonite_ has an

attractive cinnamon color, and it is found mainly in Ceylon. Because of

its color it can easily be confused with spessartine, which it closely

resembles.

Andradite, a very common garnet, usually is found in shades of red,

black, brown, yellow, or green. Some types of gem andradite have special

names for different colors: _topazolite_, yellow; _demantoid_, green;

and _melanite_, sparkling black. The very valuable demantoid is found in

Russia and Italy.

VARIETIES:

Grossular: Colorless, green, amber, brownish yellow, rose

Hessonite: Cinnamon colored

Pyrope: Deep red

Rhodolite: Rose red and purple

Almandine: Deep red

Spessartine: Brownish red to orange

Andradite: Yellow, greenish yellow, emerald green, brownish red,

brownish yellow, brown, black

Topazolite: Yellow to greenish

Demantoid: Grass green to emerald green

Melanite: Black

Uvarovite: Green

Gems in the Smithsonian Institution · 第 18 / 22 题