Journals of Two Expeditions into the Interior of New South WalesOxley, John
History
Journals of Two Expeditions into the Interior of New South Wales
Oxley, John
New South Wales -- Discovery and exploration; Oxley, John, 1783-1828
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. Neither
hunting nor fishing were successful today, but as we had become from
experience not over sanguine, our expectations were not much
disappointed, and the aspect of the country promised nothing.
It had been remarked by all, for some days past, that a putrid sour
smell seemed to proceed from the plains, and we were at first at some
loss to discover the cause of it, as there did not appear sufficient
vegetable matter in a decayed state to produce such an effect. Mr.
Cunningham discovered that it proceeded from decayed plants of the
salsolae, which produce the same effect as decayed sea-weed does in salt
marshes; in short, all the plants found in our journey over these plains
are the natural productions of low wet situations.
July 3.--So thick a fog arose during the night, that in the morning we
could not see in any direction above one hundred yards; this delayed us
considerably, and it was the middle of the day before we could proceed.
Our course lay over the same description of country as we had previously
passed. The soil in some parts a red loamy mould; in others, a dark
hazel-coloured sandy soil: this last appears to have its origin in the
depositions left by floods, the former being the original or prevailing
soil. The plants and shrubs the same as yesterday.
Public-domain text, read in full here on John Shaqi.
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