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Ch. 16: Formation of the Diamond

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126 THE DIAMOND MINES OF SOUTH AFRICA
After careful microscopical observations, Dr. Stelzner and others have reached the conclusion that the blue ground is of volcanic origin, and was forced up from below. This conclusion accords with the opinion which I formed of the origin of the
diamond-bearing deposit, during my visits to the Diamond Fields in 1884 and 1885. I then thought that the filling of the pipes was due to aqueous rather than igneous agencies, possibly to something in the nature of mud volcanoes.
The Genesis of the Diamond
The chemical composition of the diamond has long been determined, at least approximately. Sir Isaac Newton conjec­tured it to be of vegetable origin and combustible, but it was not until 1694 that Newton's assumption of its combustibility was actually proved by the famous burning glass experiment of the academicians of Cimento, at the prompting of the Grand Duke Cosmo III.
Lavoisier, Guyton de Morveau, and others practically deter­mined, later, that the burning of a diamond with a free supply of oxygen converted it into carbon dioxide ; and, finally, the ex­periments of Sir Humphry Davy, in 1816, showed that the diamond was almost entirely pure carbon. Davy's conclusions
1 See Appendix VII.
Ch. 16: Formation of the Diamond Page of 396 Ch. 16: Formation of the Diamond
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