Narrative of a Survey of the Intertropical and Western Coasts of Australia — Vol. 1: Performed between the years 1818 and 1822King, Philip Parker
History
Narrative of a Survey of the Intertropical and Western Coasts of Australia — Vol. 1: Performed between the years 1818 and 1822
King, Philip Parker
Australia -- Description and travel; Natural history -- Australia
Mount Trafalgar is a conspicuous object on the north-eastern side of the
basin; and another hill close to it being equally remarkable was called
Mount Waterloo. These two hills rise precipitously from the plain; and
being capped by a wall-like battlement bear a strong resemblance to Steep
Head in Port Warrender.
Upon leaving the cutter we crossed St. George's Basin which appeared to
receive several streams on the south side and landed on a small wooded
islet for bearings; from which the summits of Mounts Waterloo and
Trafalgar bore in a line. About two miles farther on the banks of the
river again contracted and trended to the south-east on so direct a
course that, from the distant land being hidden by the horizon, the river
bore the appearance of being a strait. We were now twenty-two miles from
the sea and as there was every appearance of this proving a considerable
stream it was honoured by the title of Prince Regent.
While I was employed upon the island with the theodolite Mr. Hunter, my
companion, shot seven or eight brace of birds: they were of two kinds;
one a species of oyster-catcher and the other a sandpiper.
The island is of small extent and is connected to the land by a shoal
communication; it is rocky and thickly wooded; the trees were chiefly
acacias. The marks of considerable floods were noticed upon its shores;
and the wrecks of very large trees were thrown up ten or twelve feet
above the high-water mark.
We re-embarked at a quarter to twelve o'clock and pulled fourteen miles
farther up the river when a slight turn hid the island on which we had
landed from our view; from the width of a mile and a half at the entrance
it had decreased to about two-thirds of a mile and still continued
gradually to get narrower: its banks throughout are bounded by steep
rocky hills rising to the height of two or three hundred feet which, in
some parts, were nearly overhanging the water; several mangrove-inlets
communicated with the river on either side but they were all salt-water
creeks.
The rocks on the hills are formed of a close-grained siliceous sandstone;
and the ground is covered with loose masses of the same rock, with
spinifex growing between them; this plant is of itself sufficient to
indicate the poverty of the soil. As we passed a small round islet an
alligator which had been basking in the sun alarmed at our approach,
rushed into the water, and, as we came near the spot, rose to reconnoitre
us, but instantly sunk again.
The sea-breeze being unimpeded by the intervention of land blew so strong
that, when the flood ceased, we were enabled to proceed for some time
against the ebb-tide. It also prevented our suffering from the heat which
would otherwise have been very oppressive for the thermometer stood all
day at 96 and 98 degrees.
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