Journals of Two Expeditions into the Interior of New South WalesOxley, John
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Journals of Two Expeditions into the Interior of New South Wales
Oxley, John
New South Wales -- Discovery and exploration; Oxley, John, 1783-1828
August 21--At eight o'clock, accompanied by Mr. Evans and
Mr. Cunningham, set out on our intended excursion down the Macquarie
River. Crossing Bell's River in the valley, we came in a mile to where
the steep rocky hills forming the west side of the vale advance their
perpendicular cliffs directly over the river. These hills we soon
rounded, and entered the vale north of them: I shall not in this place
attempt to describe the rich and beautiful country that opened to our
view in every direction. Alternate fine grazing hills, fertile flats and
valleys, formed its general outline; whilst the river, an object to us
of peculiar interest, was sometimes contracted to a width of from sixty
to eighty feet between rocky cliffs of vast perpendicular height, and
again expanded into noble and magnificent reaches of the width of at
least two hundred feet, washing some of the richest tracts of land that
can be found in any country; the banks were in those reaches low and
shelving, and covered with pebbles, whilst even at the highest floods
secondary banks restrained the river from doing the smallest damage:
these secondary banks might be from six to eight hundred feet in width,
and I think the highest marks of flood did not exceed twenty feet
perpendicular. 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.
Public-domain text, read in full here on John Shaqi.
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