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ver, after crossing much open plain, fell into another coming from E.S.E., and columns of smoke far in the N.W. showed that there was water, by showing there were inhabitants. The grass on these downs was of the richest sort, chiefly PANICUM LOEVINODE, and I was not sorry to recognise amongst it, SALSOLOE, and the ACACIA PENDULA, amongst the shrubs. As we followed the river downwards, the open downs appeared on the W.N.W. horizon as if interminable. This river, unlike that I had called the Nive, had no sand in its bed, which consisted of firm clay, and contained deep hollows, and the beds of long reaches, then, however, all dry, while abundance of large UNIO shells lay upon the banks, and proved that the drought was not of common occurrence. The general course of the river I found to be about W.N.W. true. We continued to follow it through its windings all day, which I certainly should not have done, but for the sake of water, as our progress downwards was thus much retarded. Towards evening, Corporal Graham discovered water in a small tributary coming from the S.E., while Yuranigh found some also in the main channel, where that tributary fell into it. We encamped on Graham's ponds, as this was called, and turned our horses loose on the wide plain, up to the knees in grass half dry, half green, that they might be the more fit "for the field to-morrow." The sky had been lowering all day, and the heat was intense; but during the night, the air was delicious for sleeping in, under heaven's canopy and protection. 16TH SEPTEMBER.--The "gorgeous curtains of the East" over grandly formed clouds harmonised well with my sentiments on awaking, again to trace, as if I had been the earliest man, the various features of these fine regions of earth. At 7 A.M. the temperature was 63 deg.; and (from observations registered then) the height above the sea has been found to be 1216 feet. Throughout the day we travelled over fine downs and plains covered with the finest grass, having the river on our right. Beyond it, we saw hills, which seemed to be of greater height in proportion as we descended with the river. Some were much broken, and appeared to present precipices on the other side. A broad valley extended westward from between the farthest of these broken ranges, which range seemed to be an offshoot from one further eastward. On examining the river, below the supposed junction of a tributary from the east, I found its character alte
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