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Ch. 1: Early History of Diamonds

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THE EARLY HISTORY OF DIAMONDS
one inquiring whether diamonds grow again after three or four years in the same places where they have been dug out. The answer sent back was, "Never, or at least as the memory of man can remember."
The most generally accepted theory is that diamonds are a form of carbon produced by heat and pressure, but how Nature obtained the carbon, held it inert from its affinities, and subjected it to the necessary forces, still keeps scien­tists guessing. The fact that some diamonds taken from the African mines burst as artificial ones do is accepted as evidence that they were formed under great pressure. Dia­monds in different mines have different forms of crystals, and properties, therefore, must have been formed under different conditions.
Liebig, Dana and others concluded that diamond is the product of the gradual decay of organic matter under in­fluences at present unknown. The theory advanced by Pro­fessor Carvill Lewis, that the carbon was derived from car­bonaceous shales decomposed by the action of an igneous magma forced through them by volcanic action, is consid­ered disproved by the fact that there are no carbonaceous shales in the pipes near Pretoria though they contain many diamonds. Such shales do overlay the lower strata surround­ing most diamond pipes and, as the volcanic filling of the Pretoria pipes may have come from foreign sources, the theory is tenable.
Some have thought that diamonds may have been formed from anthracite coal, possibly without passing from a solid state. Several eminent men advocated the theory that pure
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Ch. 1: Early History of Diamonds Page of 153 Ch. 1: Early History of Diamonds
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