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Ch. 30: Garnet

Ch. 30: Garnet Page of 252 Ch. 30: Garnet Text size:minus plus Restore normal size   Mail page  Print this page
'             Though of good quality the stones are small, those as large as a
hazelnut being found but rarely. Although the Bohemian garnets have been known for many centuries, the industry of mining and cutting them on a large scale is said not to have assumed any special proportions until the advent of foreigners to Karlsbad. They spread a knowledge of the stones to other countries, and a demand sprang up which has led to the establishment of a great industry, and made Bohemia the garnet center of the world. There are over three thousand men employed at the present time simply in cutting the stones, and if to these be added the number of miners and gold and silver smiths occupied in the mining and mounting of the garnets, it is estimated that a total of ten thousand persons is engaged in the Bohemian garnet industry. The stones are used not alone for jewelry and for ornamenting gold and silver plate, but also extensively for watch jewels and for polishing, f Excellent pyropes are found in Arizona, New Mexico, and southern Colorado in our own country. They occur in the beds of streams as rolled pebbles, and often associated with the green chrysolite or peridot of the eruptive rock from which they came. They are especially abundant about anthills, being removed by the ants because their size stands in the way of the excava­tions of the busy insects. The name pyrope comes from the Greek word for fire, and is applied on account of the color of the stone.
Of quite similar origin is the name carbuncle, a term applied to nearly all fiery red stones in Roman times, but now used to designate garnets cut in the oval form known as cabochon. The word carbuncle comes from the Latin word carbo, coal, and refers to the internal fire-like color and reflection of garnets.
The calcium-aluminum variety of garnet, called grossularite, cinna­mon stone, or essonite, is less used in jewelry than those above mentioned. It is usually yellow to brown in color, but may be rose-red or pink. The yellow grossularites resemble in color the hyacinth, and are sometimes sold in place of the latter, but true hyacinth is much heavier and doubly refracting. About the only essonites or cinnamon stones avail­able for gems come from Ceylon. These are of good size and color, Those from Italy, shown in the accompanying plate, are too small to cut into gems, but surrounded as they are by light green chlorite and pyroxene, make very pretty mineral specimens. Grossularite is almost always found in crystalline limestone.
Green garnets are of two kinds, the calcium-iron garnet, known as demantoid, and the calcium-chromium garnet, known as uvarovite. The demantoid garnets come only from the Urals. They have a rich green color, and make beautiful gems when clear and flawless. The name
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Ch. 30: Garnet Page of 252 Ch. 30: Garnet
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