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Ch. 16: Corundum

Ch. 16: Corundum Page of 252 Ch. 16: Corundum Text size:minus plus Restore normal size   Mail page  Print this page
Previous to the working of the mines by the English the mining was performed by domestic labor under control of the native govern­ment, all rubies above a certain size going to the king. Whenever a ruby of unusual size was found a procession of grandees, with soldiers and elephants, was sent out to meet it. One of the titles of the King of Burmah was Lord of the Rubies.
The Siamese rubies come from near Bangkok, on the Gulf of Siam. They occur in a clay which seems to be the product of alteration of a basalt. These rubies are not equal in quality to those of Burmah. Rubies are also found in the gem gravels of Ceylon, and in 'Afghanistan, thirty-two miles east of Cabul.
In our own country ruby corundum is occasionally found in connec­tion with opaque corundum in Macon County, North Carolina. In the gravels of Caler Fork of Cowee Creek of this county good rubies are found in sufficient quantity to reward systematic mining for them. They are known as "Cowee Creek" rubies.
The gravels containing them are "washed" by methods described by Dr. J. H. Pratt as similar to those used in the West for washing gold-bearing gravels. Both the gravel and the soil which overlies it are washed into a line of sluice boxes which lead into a sieve box. From the latter the dirt and fine gravel are. washed away. The material that remains is shoveled into a rocker, into the bottom of which the rubies, being heavier, gradually work, and are then removed by hand picking. These rubies are mostly small, but some gems of three or four carats' weight and of excellent color have been obtained.
Among the Montana sapphires an occasional red stone is found, but they do not have the choicest red color.
Another source of rubies is their artificial production, after the method discovered by the French chemist Fremy. The artificial rubies are made by heating a mixture of aluminum sesquioxide, carbonate of lime, barium fluoride, and potassium chromate in a porous clay crucible to a tem­perature of 1500° C, and keeping the mixture fluid for eight days. Well-formed, clear crystals up to one-third of a carat in weight -are thus produced, which have the hardness and color of native ruby. They are not considered so valuable as gems as the latter, and can usually be distinguished by the minute air bubbles which they contain. The expense of making them is nearly equal to the value of native rubies, so that their production is likely to be limited.
Other substitutes for the ruby are garnet, that from South Africa being known as Cape ruby, hyacinth, red tourmaline, known as Siberian ruby, rose topaz, sometimes known as Brazilian ruby, and spinel. None
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Ch. 16: Corundum Page of 252 Ch. 16: Corundum
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