Journals Of Two Expeditions Into The Interior Of New South Wales, 1817-18 - By John Oxley











































































 -  The valley down
which we had travelled was called Lushington's Valley (after the
Secretary to His Majesty's Treasury); the extensive - Page 121
Journals Of Two Expeditions Into The Interior Of New South Wales, 1817-18 - By John Oxley - Page 121 of 184 - First - Home

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The Valley Down Which We Had Travelled Was Called Lushington's Valley (After The Secretary To His Majesty's Treasury); The Extensive

One to the north-east, leading to Hardwicke's Range, Camden Valley (after the noble Marquis); the plains to the east

And south-east were honoured with the name of Lord Liverpool; the hills bounding Lushington's Valley, on the south side, Vansittart's Hills, after the Chancellor of the Exchequer; while several less remarkable hills were designated after persons endeared to our recollections by early friendship. A great variety of new plants rewarded the exertions of our botanist, in ascending Mount Tetley; and many, hitherto only known on the coast, were discovered on the hills and in the valleys: the acacia pendula was also seen; it had hitherto been the usual characteristic of wet lands, but it was here growing on the most dry and elevated situations. The timber on the plains and hills was chiefly those species of eucalyptus called apple tree, box, and gum trees; and on the banks of the rivulet were a few large casuarina. So much time was consumed in ascending hills and examining the country, that we did not go more than ten miles on a direct course: it was however time well bestowed. Three native fires were seen in Lushington's Valley, but the whole of this part of the country appears to be very thinly inhabited; a few wandering families making up the total of its population. The small rivulet in Lushington's Valley was named Yorke's Rivulet, in honour of Sir J. S. Yorke.

August 27. - Pursuing our course to the eastward, towards the range of low hills bordering the plains in that quarter, between five and six miles, we came to a fine stream of water, crossing the plains from the south to the north. There had been a flood in this rivulet within these few days, marks of which were observed about fifteen feet high; but still within the banks. It appears that the plains are chiefly flooded from Yorke's Rivulet, the remaining waters of which, together with rain-water, were in several places still standing on the surface; but not to the extent that the horizontal level of these plains would have led me to suppose would probably be the case. The far greater portion was a rich dry soil, and that the water is never permanent on any part of them is clearly demonstrated by the total absence of any aquatic or bog plants. From this rivulet, the three main branches of these immense plains were clearly visible to the east by south-south-east, and north-east. Of the extent of the two former, we could only judge from the lofty bounding chains of hills in those quarters; and which we could not estimate to be nearer than from forty-five to fifty miles. Hardwicke's Range bounded these to the north-east, with many intervening beautiful hills and valleys. We found the distance across the plains to the hill where we stopped, to be upwards of fourteen miles on an east line.

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