An Historical Journal of the Transactions at Port Jackson and Norfolk IslandHunter, John
History
An Historical Journal of the Transactions at Port Jackson and Norfolk Island
Hunter, John
New South Wales -- History -- Sources
The gentlemen spoke highly in favour of the country as far as
they walked; it was perfectly clear of any kind of under-wood;
the trees upon it were all very tall, and stood very wide apart;
the soil was also examined, and found very good: a small patch
was dug up, and a few potatoes, Indian-corn, melon, and other
seeds sown. This was a common practice, when a piece of ground,
favourable from its soil, and being in an unfrequented situation,
was found, to sow a few seeds of different kinds: some of the
little gardens, which had been planted in this manner, and left
to nature, have been since visited and found thriving, others
have miscarried.
After making these observations, the tide being made, we put
off in the boats, and endeavoured to get higher up, but were
frequently aground: by the time we had reached half a mile higher
than the foot of Richmond-hill, we met the stream setting down so
strong, that it was with much difficulty we could get the boats
so high. We here found the river to divide into two narrow
branches, from one of which the stream came down with
considerable velocity, and with a fall over a range of stones
which seemed to lye across its entrance: this was the fall which
we had heard the night before from our situation on the side of
Richmond-hill.
We found too little water for the boats which we had with us
to advance any farther, and the stream was very strong, although
weak to what it may reasonably be conjectured to be after heavy
rains; for here we had evident marks of the vast torrents which
must pour down from the mountains, after heavy rains. The low
grounds, at such times, are entirely covered, and the trees with
which they are overgrown, are laid down (with their tops pointing
down the river,) as much as I ever saw a field of corn after a
storm; and where any of these trees have been strong enough to
resist in _any degree_ the strength of the torrent, (for
they are all less or more bent downwards) we saw in the clifts of
the branches of such trees, vast quantities of large logs which
had been hurried down by the force of the waters, and lodged from
thirty to forty feet above the common level of the river; and at
that height there were great quantities of grass, reeds, and such
other weeds as are washed from the banks of the river, hanging to
the branches.
The first notice we took of these signs of an extraordinary
swelling of the water, was twelve or fourteen miles lower down,
and where the river is not so confined in its breadth: there we
measured the same signs of such torrents twenty-eight feet above
the surface of the water: the common rise and fall of the tide
did not appear to be more than six feet.
Public-domain text, read in full here on John Shaqi.
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