known, having furnished a
host of small stones which have usually been rose cut for cluster work
or made into beads. The Bohemian garnets are of the pyrope or fire-red
type. Relatively few large stones of sufficient transparency for cutting
are produced in the Bohemian mines. The so-called "Cape rubies" of the
diamond mines of South Africa are pyrope garnets and some large and fine
ones are found. The "Arizona rubies" are pyrope garnets, and while
seldom of notable size, some are of very fine color, approaching deep
rubies, and the color remains attractive by artificial light.
Almandite garnet, the "almandine" of the jeweler is less abundant than
pyrope, when of gem quality. Ceylon furnishes some and India furnishes
perhaps more. Brazil, from its prolific gem gravels at Minas Novas,
supplies good almandite, and smaller quantities are found in many
different localities.
Hessonite garnet, the cinnamon stone or "hyacinth" (incorrect) of the
trade, comes mainly from Ceylon.
Andradite garnet, of the variety known as demantoid, from its
diamond-like properties, and which is usually sold under the misleading
name "olivine" in the trade, comes from the western slopes of the Ural
Mountains.
TOURMALINE. Gem tourmaline comes from Ceylon, from Madagascar, from the
Ural Mountains, from Brazil, from Maine, from Connecticut, and from
California.
The Ceylon tourmalines are mostly yellow or yellowish green, sometimes
fine olive-green. Those from the Urals may be pink, blue or green.
Brazilian tourmalines are usually green, but sometimes red. In fact in
many localities several colors of tourmaline are usually found together
and it may be that a single crystal will be green in most of its length
but red or pink tipped. Some crystals have a pink core and a green
exterior. The author has found both of the two latter types in the
Haddam, Conn., tourmalines, and on one occasion was surprised to get
back a wine-colored tourmaline from a cutter to whom he had sent a green
crystal. There was but a thin shell of the green material on the
outside of the crystal.
Some of the Madagascar tourmaline is of a fine brownish red, almost as
deep as a light garnet, and much clearer than most garnet.
Would it not be fitting on account of its occurrence in several
localities in the United States, for Americans to use more tourmaline in
their jewels? The quality of some of the tourmalines of Maine, and of
California especially, is not excelled
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