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Ch. 13: Principal Diamond Mines of S. Africa

Ch. 13: Principal Diamond Mines of S. Africa Page of 448 Ch. 13: Principal Diamond Mines of S. Africa Text size:minus plus Restore normal size   Mail page  Print this page
PRINCIPAL SOUTH AFRICAN MINES 293
of clay having been sufficient until lately to more than offset the greater proportion of bort which is found in it.
The Kimberley is a true volcanic chimney or pipe and the contents carry diamonds throughout. When disĀ­covered, volcanic pipes of diamondiferous material were unrecognized. The surface was staked out in claims and worked as a very rich alluvial deposit, until it was discovered that the supposed deposit was a circumscribed area within well-defined limits, and the bed rock on which it rested was simply an unoxidized continuation of the same material to an unknown depth.
There were 470 full claims on this pipe, which at one time were split up among 1,600 owners, but which later fell year by year into fewer hands, and finally became absorbed into the De Beers Consolidation in 1889, as described elsewhere.
What the output of this mine was, in the early days of individual claims, is unknown. It has always been comparatively large, but different parts of the chimney have varied greatly, not only in the quantity of diamonds contained in the earth, but in the character of them also. Some spots have been very rich, others poor. In the west end the crystals are perfect octahedrons or white glassy stones; elsewhere they are rounded or the edges are beveled. In the southeast section, the diamonds have shown a color tendency resembling those of the Dutoits-pan. The north and northwest section of it, held many smoky stones, bort and broken crystals, many of them mere fragments. Owing to the number of owners, the great amount of stealing that went on, and an entire
Ch. 13: Principal Diamond Mines of S. Africa Page of 448 Ch. 13: Principal Diamond Mines of S. Africa
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