On the 6th our course led us across a plain, always sandy and occasionally wooded; and it was quite late in the evening when we reached the Letlosespruit, a stream which never precipitates itself over the granite boulders with much violence, except after heavy rain. The upper strata of the adjacent hills, where ground game is abundant, consist in considerable measure of red sandstone, interspersed with quartzite and black schist, the lower being entirely granite.
The limit of our next day’s march was to be the pools at Kanne. Ranged in a semicircle to our right were more than thirty conical hills, connecting the Bamangwato with the Serotle heights. There was a kraal close to the pools, and the natives, as soon as they were aware of our approach, drove their cattle down to drink, so that by the time we arrived all the water was exhausted, and fresh holes had to be dug.
On the 8th we reached the valley of the Lualaspruit, where the vegetation and surrounding scenery were charming. The formation of the rocks, and especially the signs of erosion in the river-bed were very interesting; in one place were numerous grottoes, and in another were basins or natural arches washed out by the water, which nevertheless only flowed during a short period of the year. The ford was deep and difficult. On crossing it I met with two ivory-traders, one of whom, Mr. Anderson, had been formerly known to me by name as a gold-digger; they had been waiting camped out here for several days, while their servants were ascertaining whether the district towards the Maque plain was really as devoid of water as it
