Without at present entering minutely into this feature of the climate, it may be remarked that the Kuruman district presents evidence of this dry southern region having, at no very distant date, been as well watered as the country north of Lake Ngami is now.  Ancient river-beds and water-courses abound, and the very eyes of fountains long since dried up may be seen, in which the flow of centuries has worn these orifices from a slit to an oval form, having on their sides the tufa so abundantly deposited from these primitive waters; and just where the splashings, made when the stream fell on the rock below, may be supposed to have reached and evaporated, the same phenomenon appears.  Many of these failing fountains no longer flow, because the brink over which they ran is now too high, or because the elevation of the western side of the country lifts the land away from the water supply below; but let a cutting be made from a lower level than the brink, and through it to a part below the surface of the water, and water flows perennially.  Several of these ancient fountains have been resuscitated by the Bechuanas near Kuruman, who occasionally show their feelings of self-esteem by laboring for months at deep cuttings, which, having once begun, they feel bound in honor to persevere in, though told by a missionary that they can never force water to run up hill.

It is interesting to observe the industry of many Boers in this region in making long and deep canals from lower levels up to spots destitute of the slightest indication of water existing beneath except a few rushes and a peculiar kind of coarse, reddish-colored grass growing in a hollow, which anciently must have been the eye of a fountain, but is now filled up with soft tufa.  In other instances, the indication of water below consists of the rushes growing on a long, sandy ridge a foot or two in height instead of in a furrow.  A deep transverse cutting made through the higher part of this is rewarded by a stream of running water.  The reason why the ground covering this water is higher than the rest of the locality is that the winds carry quantities of fine dust and sand about the country, and hedges, bushes, and trees cause its deposit.  The rushes in this case perform the part of the hedges, and the moisture rising as dew by night fixes the sand securely among the roots, and a height, instead of a hollow, is the result.  While on this subject it may be added that there is no perennial fountain in this part of the country except those that come from beneath the quartzose trap, which constitutes the “filling up” of the ancient valley; and as the water supply seems to rest on the old silurian schists which form its bottom, it is highly probable that Artesian wells would in several places perform the part which these deep cuttings now do.