Quantcast

Ch. 8: Opening the Craters

Ch. 8: Opening the Craters Page of 449 Ch. 8: Opening the Craters Text size:minus plus Restore normal size   Mail page  Print this page
232 THE DIAMOND MINES OF SOUTH AFRICA
But as the cutting passed farther and farther down through the reef-circled funnels without disclosing any barren stratum or break in the body of breccia, the surmise rose gradually to the point of conviction that the funnels were craters of extinct vol­canoes, filled by successive eruptions of steam or gas under great pressure with a diamantiferous breccia, carrying fragments of vol­canic and sedimentary rocks and crystals of many kinds of min­erals. This conclusion, however, was hardly more than one of several varying assumptions in advance of the thorough re­searches and analyses of later years, when the prosecution of deep mining works determined positively the existence of craters, the character of the breccia, and the composition of its encasing reef. So the progress of mining on the Diamond Fields was long a hesitating and tentative advance, groping step by step into the depths of the blue ground.
After the device of staging and hoisting ropes had solved, for a time, the problem of open excavation in the Kimberley mine crater, and the caving of the blue ground was no longer a terror to the diggers, the collection of water in the pits was a serious annoyance. Most of this water was surface drainage,
Ch. 8: Opening the Craters Page of 449 Ch. 8: Opening the Craters
Suggested Illustrations
Other Chapters you may find useful
bullet Tag
This Page