A Hand-book of Precious StonesRothschild, Meyer D.
Science
A Hand-book of Precious Stones
Rothschild, Meyer D.
Precious stones
Sphene or titanite is also a brittle mineral, 5 to 5.5 in hardness;
specific gravity, 3.4 to 3.56; transparent, doubly refractive; lustre,
adamantine to resinous; colors, brown, gray, yellow, green, black, and
colorless; and composition:
Silica 31
Titanium oxide 41
Lime 27
Ferrous oxide 1
When transparent in colorless, greenish, or yellow colors, this mineral
presents an appearance like the fire opal.
Sphene is found in Switzerland, the Urals, Tyrol, Finland, Wales,
Ireland, Germany, Canada, and the United States.
PHENACITE.
This mineral, rarely used as a gem stone, is 7.5 to 8 in hardness;
specific gravity, 2.96 to 3; lustre, vitreous; transparent to
semi-translucent, doubly refractive, it does not melt before the
blow-pipe, and contains:
Silica 54.2
Glucina 45.8
Phenacite occurs colorless, and also bright wine-yellow inclining to
red, and brown. This stone is found in Russia, Mexico, and Alsace.
The colorless or transparent variety approaches the diamond in
brilliancy, especially under artificial light.
EPIDOTE.
Epidote usually occurs in a peculiar yellowish-green, called pistachio
green, a color that is seldom found in other minerals. Besides
this color, olive, brownish-green, greenish-black and black, red,
yellow-gray, and grayish-white occur. The hardness of epidote is 6
to 7; specific gravity, 3.32 to 3.50; lustre, vitreous to pearly;
refraction, double. The stone is transparent to opaque, is attacked by
acids, and is slightly affected by the blow-pipe. It is composed of:
Silica 38
Alumina 22
Ferric oxide 15
Lime 23
Water 2
Epidote is found in Norway, Saxony, Siberia, Brazil, on the St.
Gothard, in Switzerland, in the Tyrol, and in the Hartz.
AXINITE.
Axinite is a brittle mineral which has occasionally furnished some
pretty gem stones.
The hardness of this stone is 6.5 to 7; specific gravity, 3. to 3.3;
lustre, vitreous. It is transparent to translucent, is not attacked by
acids, and melts readily before blow-pipe. It is composed of:
Silica 43
Lime 20
Alumina 16
Ferric oxide 10
Boron trioxide 5
Manganese dioxide 3
Magnesia 2
Potash 1
Axinite occurs in clove-brown, plum-blue, and pearl-gray, and exhibits
trichroism. The best specimens come from St. Christophe in Dauphiny,
but it is also found at Santa Maria, and in Switzerland, Sweden,
England, Chili, Saxony, the Hartz Mountains, and the United States.
Axinite is usually cut, like the opal, cabochon, but is rarely used as
a gem stone.
DIOPSIDE.
Diopside is cut and sometimes sold in Turin and in Chamouny as a gem
stone, but no great quantity of this mineral is used for ornamental
purposes.
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