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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