good forest land; and on the
10th we had the satisfaction to fall in with the first stream
running northerly. This renewed our hopes of soon falling in with
the Macquarie, and we continued upon the same course,
occasionally inclining to the eastward, until the 19th passing
through a fine luxuriant country, well watered, crossing in that
space of time _nine_ streams, having a northerly course
through rich vallies; the country in every direction being
moderately high and open, and generally as fine as can be
imagined.
No doubt remained upon our minds that those streams fell into
the Macquarie, and to view it before it received such an
accession, was our first wish. On the 19th we were gratified by
falling in with a river running through a most beautiful country,
and which I would have been well contented to have believed the
river we were in search of. Accident led us down this stream
about a mile, when we were surprised by its junction with a river
coming from the south, of such width and magnitude, as to dispel
all doubts as to this last being the river we had so long
anxiously looked for. Short as our resources were, we could not
resist the temptation this beautiful country offered us, to
remain two days on the junction of the river, for the purpose of
examining the vicinity to as great an extent as possible.
Our examination increased the satisfaction we had previously
felt: as far as the eye could reach in every direction, a rich
and picturesque country extended, abounding in limestone, slate,
good timber, and every other requisite that could render an
_uncultivated_ country desirable. The soil cannot be
excelled, whilst a noble river of _the first magnitude_
affords the means of conveying its productions from one part to
the other. Where I quitted it its course was northerly, and we
were then north of the parallel of Port Stevens, being in
latitude 32 degrees 45' South, and 148 degrees 58' East
longitude.
It appeared to me that the Macquarie had taken a north
north-west course from Bathurst, and that it must have received
immense accessions of water in its course from that place. We
viewed it at a period best calculated to form an accurate
judgment of its importance, when it was neither swelled by floods
beyond its natural and usual height, nor contracted within its
limits by summer droughts: of its magnitude when it should have
received the streams we had crossed, independent of any it may
receive from th
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