Australia Twice Traversed - The Romance Of Exploration, Through Central South Australia, And Western Australia, From 1872 To 1876 By Ernest Giles









































































 -  The longer it remains the thicker it gets, until at last it
dries in cakes which shine like tiles; these - Page 46
Australia Twice Traversed - The Romance Of Exploration, Through Central South Australia, And Western Australia, From 1872 To 1876 By Ernest Giles - Page 46 of 394 - First - Home

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The Longer It Remains The Thicker It Gets, Until At Last It Dries In Cakes Which Shine Like Tiles; These At Length Crumble Away, And The Clay Pan Is Swept By Winds Clean And Ready For The Next Shower.

In the course of time it becomes enlarged and deepened.

They are very seldom deep enough for ducks.

The grass and herbage here were excellent. There were numerous kangaroos and emus on the plain, but they preferred to leave us in undisturbed possession of it. There were many evidences of native camping places about here; and no doubt the natives look upon this little circle as one of their happy hunting grounds. To-day I noticed a tree in the mallee very like a Currajong tree. This being the most agreeable and fertile little spot I had seen, we did not shift the camp, as the horses were in clover. Our little plain is bounded on the north by peculiar mountains; it is also fringed with scrub nearly all round. The appearance of the northern mountains is singular, grotesque, and very difficult to describe. There appear to be still three distinct lines. One ends in a bluff, to the east-north-east of the camp; another line ends in a bluff to the north-north-east; while the third continues along the northern horizon. One point, higher than the rest in that line, bears north 26 degrees west from camp. The middle tier of hills is the most strange-looking; it recedes in the distance eastwards, in almost regular steps or notches, each of them being itself a bluff, and all overlooking a valley. The bluffs have a circular curve, are of a red colour, and in perspective appear like a gigantic flat stairway, only that they have an oblique tendency to the southward, caused, I presume, by the wash of ocean currents that, at perhaps no greatly distant geological period, must have swept over them from the north. My eyes, however, were mostly bent upon the high peak in the northern line; and Mr. Carmichael and I decided to walk over to, and ascend it. It was apparently no more than seven or eight miles away.

As my reader is aware, I left the Finke issuing through an impracticable gorge in these same ranges, now some seventy-five miles behind us, and in that distance not a break had occurred in the line whereby I could either get over or through it, to meet the Finke again; indeed, at this distance it was doubtful whether it were worth while to endeavour to do so, as one can never tell what change may take place, in even the largest of Australian streams, in such a distance. When last seen, it was trending along a valley under the foot of the highest of three tiers of hills, and coming from the west; but whether its sources are in those hills, or that it still runs on somewhere to the north of us, is the question which I now hope to solve.

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