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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