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ORIGIN OF THE DIAMOND           383
ened mud. It has been said that the sharp edges of the diamond crystals found in the kimberlite would be im­possible had they been formed in a molten mass, but as Moissan produced such diamond crystals, though small, from charcoal confined in fused iron, and diamond will not burn without a free supply of oxygen, the argument appears invalid.
Geologists assert that the center of the earth is solid, but that between the crust and that solid center, lies a mass of molten material. They also claim to have in­dubitable evidence that the earth's bulk is gradually shrinking, while at the same time by astronomical forces it assumes a somewhat elliptical form at the equator. In the process of shrinking, the uneven thickness and strength of the crust would produce uneven results. Some weaker parts of the area would settle lower, toward the center of gravity, leaving other stronger parts elevated above the general level, and they would become, thereby, mountain ranges where the buckling occurred, and high plateaus, if the area was large, within the mountainous border lines of greatest strain, marking the junction of the weaker sinking portions of the crust and the thicker and more stable part.
It seems reasonable to suppose that some such oc­currence took place during past ages in South Africa, whereby the earth's crust seaward, east, west, and south from the mountains surrounding the diamond plateau, sank, leaving the plateau at an elevation, with undis­turbed horizontal strata, except for occasional vertical rents in it extending probably to the underlying magma. This hypothesis seems more probable than that of a deep explosive or expansive force sufficiently extensive