indeed
the same substance, but in a vitreous or non-crystalline state. The
specific gravity of this lime spinel, which has been sold for blue
sapphire, is lower than that of sapphire or even than that of blue
spinel.
Turquoise.
The
turquoise acquired its name from having been imported into Western
Europe by way of Turkey. The best specimens come from the district of
Nishapur, in the Persian province of Khor-assan, where the gem occurs
in a porphyritic rock. The hardness of the stone is nearly 6, and its
specific gravity 2'75. There is a peculiar quality in the colour of the
best turquoises, which is partly dependent upon the delicate hue of its
blue, with which a slight infusion of green is mingled, and partly upon
the faint translucency of the stone. For turquoise is indeed not
opaque, thin splinter.; transmitting light easily.
It is very probable that turquoise was described by Pliny under the three names of callais, callaina, and callaica. Turquoise
is often now called callaite, while an allied mineral from a Celtic
grave near Mane-er H'roek in Lockmariaquer, and now preserved in the
Museum of the Polymathic Society of Morbihan, has been called callais
and callainite, but has lately been proved identical with the variscite
of Breithaupt, a mineral described in 1837.
The
true turquoise, which shows various hues and tones of blue, greenish
blue, and bluish green, is not to be confounded with the blue fossil
turquoise, or odontolite, which is in fact fossil ivory, generally of
Mastodon teeth. The true turquoise owes its colour to phosphate of
copper, and its powder becomes dark blue when moistened with strong
ammonia. Odontolite is coloured by phosphate of iron, is more opaque
and heavier than turquoise, and much softer, and shows its bony
structure under the microscope, Turquoise often becomes green by age ;
this change is frequently noticeable in the turquoise cameos of the
Italian cinque-cento.