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Ch. 2: Gems in Ceylon

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222                                           GOLD AND GEMS.
Beryl, Emerald.—There appears to be no record of the green variety of the beryl, which is known as the emerald, ever having been found in India. This gem, so highly esteemed by the natives of India, especially by the Mahomedans, is imported from the European markets. The pale-coloured beryl or aquamarine, is, however, obtainable in several ports of the country.
Garnet or Carbuncle.—The cutting of precious garnels which are found in many parts of India, en cabochon, appears to have been practised since early times, and there is, at present, a small export trade in these so-called carbuncles.
Lapis Lazuli.—The most famous mines of this stone are situated in Badak-shan. It is not known to occur, though it is much esteemed in India.
Turquoise.—This stone, which is much worn by some of the Himalayan tribes, is of very doubtful occurrence in India. The supply, it is believed, comes from certain famous mines in Persia.
Many ornamental stones may be mentioned, as, for example, cornelian, jasper, agate, jade or serpentine. The first three are found in great abundance in parts of Western and Southern India. Their cutting and polishing constit­utes a famed industry of great antiquity, and which still exists in certain re­gions. Jade is found, but not worked, in several parts of the peninsula. In native Burma and in Karakash, to the north of the Himalayas, there are famous mines of it. Serpentine is found at many localities', both in peninsula and extra-peninsular India. A very superior class of steatite, much used for carvings, is found in Rajputana, but upon it heavy royalties and other dues are levied.
METALS.
Omitting from consideration on the present occasion, the less important metals, of the presence of which more or less abundant indications exist in India, I shall limit my observations to a few brief remarks on the following— gold, silver, copper, lead, zinc, iron, and tin.
Gold.—Regarding gold, especially in reference to the position it at present occupies in the eyes of British capitalists, I regret that I am obliged to write very much as an outsider, as, although when lait in India, I was most anxious to visit Kolar and the Wynaad, I was unable to do so. My opinion of these southern regions is founded upon what I have read and what I have heard; I am, therefore, not unnaturally reluctant to press it upon my present hearers. All who have any interest in the matter are aware that the testimony as to the extent of the auriferous character of the quartz reefs is of a most conflicting character. The value of this testimony is now about to be put, at great cost, to a test which must decide it one way or the other, and such large sums of money having been embarked in the enterprise, the time for giving opinions or making useful predictions has, in one sense, at least, passed away. Any attempt at generalisation from all the available facts would be of little avail, and specific information regarding particular properties is not at my disposal. In my " Economic Geology" I have given an account, based on all the information available to me when it was written, of the many and widely separated tracts in India where the presence of gold has indisputably been proved. In some of these tracts the mode of occurrence precludes the possibility of a plentiful supply, while, in others, the abundance can only be ascertained from operations which, from the nature of the case, must be costly.
That a vast quantity of gold has been raised from the soil of India has, * I consider, been fully demonstrated by the amplest testimony; but when we attempt, by facts at our disposal, to estimate the time and labour which have been expended to produce that quantity, we may feel doubt as to the profitable character of the industry. I know of numerous regions in India, where tne indigenous gold washers eke out a precarious existence by the practice of th . profession. All experience, however warns us against attaching too much vaelr to the bare fact of the existence of gold in alluvial depoits. It may in somee
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