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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