and many of their affluents, take their rise; its subsoil consists of the grey limestone which I have so frequently mentioned. We only passed two farms hereabouts, Pitfontein and Witfontem, and these lay in small depressions that seemed to lead down to the Harts River.
On the 22nd we commenced a gradual descent, and entered the valley of the Makokspruit, in which the Makokskraal is situated. In this valley was a farm, the owner of which was a relative of a man whom I had attended in the diamond-fields. Although they were very poor, the people were very anxious to treat us hospitably. Next day we came to the valley of the upper Schoenspruit; the stream was flowing freely, and all along its shores farm followed farm in close succession. Between the Schoenspruit and Potchefstroom we had to cross several low ridges, the south-western spurs of the Hooge Veldt lying parallel to the Mooi and to the affluents of the Schoen.
I discovered an interesting rocky pass on the first ridge on the way to Potchefstroom, with walls of quartzite nearly semicircular, and rising almost perpendicularly. The farm shut in by them was called Klipport; another, a little further on, was called Klipfontein, the quartzite veins in the ferruginous slate being here also quite apparent. Arrived at Potchefstroom, I carried out my intention of selling two of my bullocks, as I had come to the end of my resources. Here, too, I said good-bye to my three companions, two of whom, Eber-
