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sandy watercourse, winding through a grassy valley, which everywhere presents indications of the most violent floods. Beyond this is an extensive grassy plain; and for three or four miles scarcely a trace of the creek could be seen. We then came to a clump of trees, amongst which were two large waterholes surrounded by polygonum bushes, and containing great numbers of small fish. These holes appear to be permanent. We found about sixty blacks camped here. Above these waterholes, which are together about half a mile long, the creek again disappears on the plain. The land for the next ten or twelve miles in a north-north-easterly direction is very fine for pastoral purposes, being alternately grassy plains and ridges. At twelve or thirteen miles we crossed the creek where it has cut for itself a deep narrow channel, the banks of which are densely timbered and well grassed, but the waterholes are small, and contained very little water. For a distance of six miles the creek is of a very insignificant character. It appears to be divided into several branches, which traverse clay flats badly grassed. Here and there are some lines of low sandy rises, with plenty of feed on them. All the watercourses are distinctly marked by lines of box timber. At about nine miles from where we crossed the creek, and after traversing some loose polygonum ground, which was covered with mussel shells and a shell resembling a periwinkle, we came to a branch of the creek containing a splendid waterhole 150 links broad and about half a mile long. A little above this the creek again disappears for a short distance, and then there is a long narrow channel of undoubtedly permanent water, being nearly four feet deep in the shallowest places; it is only on an average about fifty links broad, and well sheltered by overhanging box trees. The temperature of the water on the morning of the 7th November, at six o'clock, was 68 degrees; the temperature of the air at the same time being 50.5 degrees. Our camp at this place is indicated by a box tree marked B over LII in square, the geographical position of which is by account 28 degrees 26 minutes 9 seconds south latitude, and longitude 143 degrees 0 minutes east. In proceeding from here in a north-north-easterly direction up the course of the creek, or rather of the water, for the creek is again lost on the plains for five or six miles, we passed the southernmost point of a prominent sandstone range, the nea
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