I Am Quite
Convinced That At This Place, When The Banks Are Overflowed, The Waters
Must Extend From Thirty To Forty Miles On Each Side Of The Stream, As We
Are That Distance From Any Eminence.
If there had been any nearer to the
north, west, or south, we must have seen it from those
Extensive plains
on which we have travelled for the last three days; for looking
eastward, we can distinctly perceive Macquarie's Range, from which we
estimate ourselves to be about thirty-five miles west. The stream was
sounded in various places during the day, and its greatest depth never
exceeded seven feet; the bottom and sides a stiff bluish clay. Latitude
observed 33. 32. 22. S., longitude 145. 5. 50. E.; variation of the
compass 6. 49. E.
July 2. - At nine o'clock we again set forward down the stream; our
course, as it has hitherto done, lay over apparently interminable
plains, nothing relieving the eye but a few scattered bushes, and
occasionally some dwarf box-trees: the view was boundless as the ocean,
neither eminence nor hillock appearing. On the edges of the stream
alone, and the lagoons that occasionally branched from it, was any thing
like timber to be seen. The occasional openings on the stream enabled us
to perceive, that the north side was in every respect similar to the
south: I was so much deceived, by the semblance of the plains on the
other side to sheets of water, that I twice went down to the edge of the
stream to assure myself to the contrary.
A strong current of water must frequently pass over these plains, as is
evident from the traces left by the washings of shrubs, leaves, etc. The
soil was a brown hazel-coloured sandy loam, very soft and boggy; in
places it was more tenacious, water still remaining in many holes. By
the marks on the trees it would seem that the stream occasionally
overflows its banks to the depth of three or four feet; and five miles
back from it small trees were seen, that had evidently stood from twelve
to eighteen inches in the water. As usual we saw no recent signs of
natives having visited these parts; here and there the remains of
burnt muscle-shells would denote that at certain seasons the stream is
visited by them for the purpose of procuring these shell-fish: I am
clearly of opinion that, in dry summers, there is no running water in
the bed of the present stream, and thus it is easy for them to procure
the muscles from the shallow stagnant pools which would naturally be
formed at every bend of the stream. To procure any such shell-fish
whilst a stream like the present is running in it, is totally
impossible.
Although we did not travel above eleven miles, we were nearly seven
hours in performing it. Our halting place was within a few feet of the
river, and so wet and spongy, that the water sprung even from the
pressure of our feet; and this has been the case nearly ever since we
made the stream, though of course we chose the driest spots.
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