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











































































 -  The rapids were usually formed by small stony islands,
which. dividing the stream rendered it shoaler in those places than - Page 157
Journals Of Two Expeditions Into The Interior Of New South Wales, 1817-18 - By John Oxley - Page 157 of 354 - First - Home

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The Rapids Were Usually Formed By Small Stony Islands, Which.

Dividing the stream rendered it shoaler in those places than in others, but they never extended above one hundred yards, and were none of them fordable.

Limestone of the best quality and of various species abounded; and it appeared to me to be as common as the other stone forming the hills, which was a fine and hard granite. We passed through this charming country for upwards of twelve miles, the course of the river during that time being nearly north, and from appearances we thought it must continue in that direction for a considerable distance farther. A perpendicular limestone rock overhanging the river terminated our excursion; adjoining to this rock (which was called Hove's Rock, from its being covered with a beautiful new species of hovia), a stratum of fine blue-slate was found. A little lower down, the bank on the east side was formed of perpendicular red earth cliffs at least sixty feet high, extending along the reach nearly three quarters of a mile; this bank was named Red Bank: a fine grassy hill thinly covered with wood rose eastward of it.

The timber was unusually fine, consisting chiefly of very large and straight blue guns; beautiful large casuarina trees were occasionally growing at the very edge of the water. The tops and sides of the rocky precipices on the west side of Wellington Vale were clothed with cypress trees, which had all the appearance of the pinus silvestris, that adorns the mountains and glens of Scotland.

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