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this plain resumes, in many parts, the arboreous covering, the general feature of this portion of Australia.
On the higher elevations the rock formation continues of the description already mentioned, the claystone partaking of a more or less ferruginous nature, and agglomerating with fragments of quartz, feldspar, and granite, which, although not particularly detailed hitherto, have been generally common. The lower eminences, however, often exposed a perpendicular, and still more frequently an excavated front of a fine and friable clayey sandstone, of a cream colour, fine, granular, and almost too little tenacious to be unreservedly recommended for building.
On the 30th April I ascended (if ascent it be entitled to) the right bank of the river W. ½ N. three quarters of a mile, then W. ½ S. and W. over one mile and three quarters of a good grassy inclined plain, ornamented with white gum; afterwards over a sandy and gravelly soil and height for one quarter; and then over, first, a plain of sandy soil, and white gum and yeit trees; secondly, a moderate elevation of sandy soil and shrub; and lastly, across a lower level of good soil, white gum, wattle and grass near the river, which, in its windings, opportunely crossed our path.
On the last-mentioned piece of good soil, Mokare detected and pointed out to me the footsteps of horned cattle and of a horse; they were not recent, but sufficiently evident to show that they bore the form attributed to them; and as a further confirmation, Mokare had previously told me that two bullocks and a horse had been near this some months ago, and seen by the natives, who informed him.
