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Ch. 2: Gems in Ceylon

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316
GOLD AND GEMS.
Passing over much detail of a more or less interesting character, we quote as follows:—
But if the diamond, amber, coal, and petroleum are absent from our rock formations, happily there can be no question as to either the quality or the quantity of our mineral carbon in the shape of plumbago, of which indeed, in the form most valuable for the manufacture of metal-melting crucibles, Ceylon seems to have as much a natural monopoly as she has of first-class cinnamon in the vegetable world. There are, no doubt, vast deposits of graphite in North America, especially in Canada, but the mineral seems to be generally diffused in rock from which it is difficult and expensive (labour being scarce and dear) to separate the >mall particles. Graphite, although rare in a form economically valuable, seems very widely distributed over the face of the earth. In India plumbago has been found in a large number of places, and has been the subject of many experiments and much discussion, but the results have been hitherto disappointing. It generally app-ars sparingly in very quartzy rock, and in heavy ferruginous gneiss. The mineral is deficient in lustre, contains much iron, and one specimen gave 35 per cent of lime. Lime is, perhaps, even more fatal to the value of plumbago than iron, and although graphite may occur in the magnesian limestones of Ceylon (I never heard of but one instance), it is quite mmifest that digging in the dolomite need never be resorted to, the min­eral being so plentiful in our quartzy gneiss, where the only enemy encount­ered, and that, happily, not very frequently, is iron. Like some other advers­aries, this one sometimes appears in guises the most radiantly beautiful, in the present case as pyrites varying from splendidly crystallized masses, with facets polished like finest silver, and again simulating auriferous treasures by putting on the most glorious colourings of gold, shading away to a lovely and delicate green, indicative, this tint, it is supposed, of the presence of sulphate of copper.                                                  *
This auriferous coloured pyrites is appropriately named in Sinhalese diya rat-ran, or " water gem-gold," the recognition of water as the agent to which the formation and its brilliant colours are largely due being, curiously enough, in perfect accord with the conclusions of the most advanced geological scientists.
To Mr. Williams, Acting Government Agent of the North-Western Pro­vince, I am indebted for a collection of interesting specimens from Polgola on the road to Dambulla, showing how plumbago is associated with and forms round a nucleus of crystalline or semi-opaque and sometimes garnetiferous quartz (the position of the minerals being, I am told, occasionally reversed), and quite a number of pieces of rock wViich the non-scientific might well be ex­cused for regarding as coated and permeated with brilliant golden ore. These may be regarded as the flowers of the subterrannean regions where plumbago is mined. I am bound to state, however, that the brilliancy of iron pyrites has no effect in modifying the inimical feelings with which those connected with the plumbago enterprise regard the mineral, while they talk with disapproval and disgust of the yabora=(a)va iron, bora dross: iron dross, the hard iron­like form of plumbago; and anyone desirous of procuring specimens will be, made heartily welcome to what in the eyes of the plumbago dealer is associ­ated with a rocky inferior and unsaleable product. But truly the pure soft mineral itself, in its various forms of crystallization, the most prevalent being a radiatin» star-like arrangement, and its variation of sparkling colours from steel grey to plates of jet black, may be regarded as a veritable "thing of bnautv." A collection of first-class lumps, each highly polished and lustrous, intended for shipment to Germany, which could be seen at -Mr. VV. A. Fernando's store recently, was certainly a striking sight. In connection with this collection of silvery masses, Mr. Fernando showed us specimens of a dark-coloured variety, of needle-like formation, which he said he had been requested by his customers to make up separately, as the ordinary mills could not easily grind that panic-
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