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Ch. 15: Turquoise

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XV
TURQUOISE
This mineral is known to scientists as " callaite." Al­though not transparent, its beautiful color, and the fact that it is considered peculiarly suited to blond complexions, make it a favorite jewel with many. The color, equally good by artificial light, is due to phosphate of copper, of which it contains, according to different analyses, two to eight per cent. It is found only in compact form in irregular veins within a matrix. It has no cleavage, and the fracture is conchoidal. Heat sweats the water out of the stone and crackles it.
The most celebrated mines are the Persian, and the tur­quoises taken from them are renowned for their beauty and credited with holding the color better than others, though the stones of different localities vary in this respect, some fading badly soon after being released from the matrix. The mines are situated in the northeastern part of Persia, in a district of the Nishapur province, and the turquoise is taken from a stratum of eruptive and altered rock at a height of nearly seven thousand feet. An old mine called the Abdur-rezzagi produces the finest. Many of the Persian turquoises lose color as they dry; others change to a greenish tint. This is the prevailing fault of turquoises, and though many are treated to preserve the color, and are guaranteed, they are liable, under certain conditions, to turn more or less green. And this is true of all turquoises, wherever they are mined. The mines are worked in a careless and irregular way by the natives. There is an abundance of good material, but the shafts and cuttings are so choked with debris and in such a dangerous condition that no European cares to make
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Ch. 14: Opal Page of 237 Ch. 15: Turquoise
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