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. It was nearly five o'clock before
we returned to our tent, highly gratified with our day's excursion.
Nothing can afford a stronger contrast than the two rivers, Lachlan and
Macquarie; different in their habit, their appearance, and the sources
from which they derive their waters, but above all differing in the
country bordering on them; the one constantly receiving great accession
of water from four streams, and as liberally rendering fertile a great
extent of country; whilst the other, from its source to its termination,
is constantly diffusing and extenuating the waters it originally
receives over low and barren deserts, creating only wet flats and
uninhabitable morasses, and during its protracted and sinuous course is
never indebted to a single tributary stream. The contrast indeed
presents a most remarkable phenomenon in the natural history of the
country, and will furnish matter in other parts of this Journal, for
such conclusions as my observations have enabled me to form.
August 22 - Among the other agreeable consequences that have resulted
from discovering the river in this second Vale of Tempe, may be
enumerated, as not the least, the abundance of fish and emus with which,
we have been supplied; swans, and ducks, were also within our reach, but
we had no shot. Very large muscles were found growing among the reeds
along some of the reaches; many exceeded six inches in length, and
three and a half in breadth. Traces of cattle were found in various
places as low as Hove's Rock, which are now doubtless straying through
the country.
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