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











































































 -  Indeed we had the utmost difficulty to
get them back again. Three of them actually rolled over, and were saved - Page 68
Journals Of Two Expeditions Into The Interior Of New South Wales, 1817-18 - By John Oxley - Page 68 of 94 - First - Home

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Indeed We Had The Utmost Difficulty To Get Them Back Again.

Three of them actually rolled over, and were saved only by the trees from being precipitated to the bottom.

Quitting this place, we proceeded up the glen, into which many small streams fell from the most awful heights, forming so many beautiful cascades. After travelling five or six miles, we arrived at that part of the river at which, after passing through a beautiful and level though elevated country, it is first received into the glen. We had seen many fine and magnificent falls, each of which had excited our admiration in no small degree, but the present one so far surpassed any thing which we had previously conceived even to be possible, that we were lost in astonishment at the sight of this wonderful natural sublimity, which perhaps is scarcely to be exceeded in any part of the eastern world. The river, after passing through an apparently gentle rising and fine country, is here divided into two streams, the whole width of which is about seventy yards. At this spot, the country seems cleft in twain, and divided to its very foundation: a ledge of rocks, two or three feet higher than the level on either side, divides the waters in two, which, falling over a perpendicular rock two hundred and thirty-five feet in height, forms this grand cascade. At a distance of three hundred yards, and an elevation of as many feet, we were wetted with the spray which arose like small rain from the bottom: the noise was deafening; and if the river had been full, so as to cover its entire bed, it would have been perhaps more awfully grand, but certainly not so beautiful. After winding through the cleft rocks about four hundred yards, it again falls in one single sheet upwards of one hundred feet, and continues in a succession of smaller falls about a quarter of a mile lower, where the cliffs are of a perpendicular height, on each side exceeding one thousand two hundred feet, the width at the edges about two hundred yards. From thence it descends as before described until all sight of it is lost, from the vast elevation of the rocky hills which it divides and runs through. The different points of this deep glen seem as if they would fit into the opposite fissures which form the smaller glens alternately on either side. The whole is indeed a grand natural spectacle, and is an indubitable mark of the vast convulsions which this country must at one period have undergone. The rocks are all slate, the upper romanae of which are of a light brown colour, rotten, and easily separated. Nearer the base or surface of the water they are of a dark blue, and of a firmer texture. The waters are quite discoloured, owing to the nature of the bed over which they run, the soluble particles of coal among the slate tinging them a dark brown. This fine fall is not more than five miles below the place where we crossed the river on the 9th instant, and we were doubtless prevented from hearing the noise of the waters, by the numerous smaller falls in the vicinity. This most magnificent fall and the river itself were respectively named Bathurst and Apsley, in honour of the Noble Secretary of State for the colonies. Although a week had elapsed in effecting the passage of this river, we could not consider it as entirely lost, especially as it enabled us to ascertain that its direction was to the coast; and we hoped that the nature of the country would permit us to fix its embouchure.

September 16. - The weather for some days past has been very unseasonable, cold and tempestuous, with frequent heavy and continued showers of rain: this remarkable coldness of temperature in such a latitude (31 degrees,) I cannot but attribute to the considerable elevation of the country above the sea, being certainly between four and five thousand feet. We proceeded to the south-east during this day's journey, on purpose to avoid the broken land in the vicinity of the river. It was good travelling though hilly: the soil, for the most part, a poor clay; and the timber not so good or large as usual. There was however much good land, particularly in the valleys, through every one of which a stream of water took its course to the river. At twelve miles, we halted on the banks of a considerable and rapid stream watering an extensive and wide valley. The many waters which fall into Apsley River must very considerably increase its magnitude; and I am in hopes after it has cleared this mountainous tract and we again fall in with it, that we shall find it a useful as well as fine stream. The river on which we encamped was named Croker's River, in honour of the First Secretary of the Admiralty.

September 17. - We proceeded on an easterly course during this day's journey; and seven miles from Croker's River crossed a smaller stream running to the north-east. For the first ten miles the country was very poor and badly timbered, with barren stony hills; but from the last mentioned stream to our halting-place, at the end of twelve miles, though the land was hilly the soil was excellent, consisting of a rich, dark mould. The hills were particularly rich and thickly clothed with fine timber, blue gum, and stringy bark. We halted on the side of a hill, from the top of which we could see a great distance to the north and east. In the first quarter, lofty hills were seen from eighty to one hundred miles off, and generally very irregular. To the east the land was elevated, but more divided by sloping valleys, and we augured that at least for thirty miles in the direction of our course, we should not meet with any such serious obstruction as the last: indeed we imagined we could trace the course of the river nearly on a parallel line with us.

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