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368                      THE DIAMOND
claimed that the form of the carbon depends upon the amount of pressure existing at the temperature which permits transformation.
Some argue that these explosions are due to gas held under great pressure in the interior of the crystal. Mr. Williams declares that to be an argument against the theory of formation in an igneous magma at high temĀ­perature. Broken diamonds are frequently found in the diamondiferous pipes of South Africa. Though the cause of the fracture is unknown, it has been ascribed to the volcanic action by which the diamond-bearing clay was forced through intervening strata to the surface.
Many theories have been advanced as to the source from which Nature obtained the carbon. Newton and later eminent scientists believed it to be of vegetable origin, some basing their conclusions mainly on the microscopic study of the residual ash. Crookes on the other hand asserts that iron is the chief constituent of the ash, and uses that as an argument in favor of deep-seated masses of molten iron saturated with carbon, a larger process of the method employed in the laboratory by himself and Moissan. In opposition to this Mr. Williams states that many exhaustive tests which he has made with all kinds of diamonds for iron, metallic or oxidized, with powerful magnetic apparatus, indicated either an entire absence of iron, or infinitesimal traces only. Inasmuch, however, as the crystallization appears to depend largely on the complete segregation of the carbon from that with which it was previously combined, this argument against the theory of Crookes does not appear forcible. As science has made diamonds from saturated molten iron, Nature may certainly have used