Page:Journal of the Royal Geographical Society of London, volume 2.djvu/152

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128
Interior Discovery in New South Wales.

tion of two hundred feet, and in which 'coral and fossil remains' were remarked to be plentifully imbedded. At this stage of their passage, those long ranges of forest hills, which extend along the eastern shore of the Gulf of St. Vincent became discernible, indicating to the exploring party their approach to the coast. On the 3d February, the river having reached the meridian of 139j°, the disposition of the bounding cliff's gave its course a decided bend to the southward, through a continuation of the glen, which at length opened into a valley.

Here the river was observed to have lost the sandy bottom which it had exhibited throughout its long course from the eastward, for its bed having now dipped to almost the level of the sea, its waters had become 'deep, still, and turbid.' Its course to the south was followed by the voyagers along reaches of from two to four miles in length; and upon their passing the parallel of 35°, a more open country appeared before them, for the cliff's having partially ceased, had given place to picturesque hills and lower undulations, beneath which extended 'thousands of acres of the richest flats;' but, as Captain Sturt adds that these were covered with reeds, and were evidently liable to inundation from the river, the value to the agriculturist of such marshy grounds, scarcely at all elevated above the sea-shore, may be easily estimated.

On the 8th of February (the thirty-second day of the voyage from the depot) the hills 'wore a bleak appearance,' and the few trees, which had at one period fringed their ridges, were for the most part broken off, 'as if by the prevalent winds.' At noon, upon entering the river's last reach, no land could be discerned at its extremity; some low hills continued, however, along its left bank, whilst its right was hid by high reeds. Immediately afterwards, these enterprising voyagers entered an extensive lake, the body of which stretched away far to the south-west, in which direction 'the line of water met the horizon.' This lake, which received the name of 'Alexandrina,' was estimated at from fifty to sixty miles in length, and from thirty to forty in breadth. A large bight was observed in it to the south-east, and an extensive bay at the opposite point; still, notwithstanding these dimensions, this very considerable sheet of water appears to be but a mere shoal throughout, since Captain Sturt states 'its medium depth' is but 'four feet'!

Upon this vast but shallow lake, he pursued his voyage to the southward, remarking that its waters, which at seven miles from the point of discharge of the Murray into it were brackish, were at twenty-one miles across perfectly salt, and there the force of the tide was perceived. As the party approached the southern shore, the navigation of the boats was interrupted by mud flats,