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
Off the entrance of Van Diemen's Gulf (Dundas Strait) we passed through
large quantities of sea sawdust, some of which was put into a bottle; and
when the process of putrefaction had taken place the substance sunk to
the bottom and coloured the water with a crimson tinge.
1820. September 3.
After passing the meridian of Cape Van Diemen our course was directed
towards Captain Baudin's Banc des Holothuries near Cape Bougainville; but
being impeded by calms and light winds did not reach it until the 3rd of
September, when we passed between its south-east extremity and Troughton
Island. Before dark we passed over the north extremity of the long reef
to the westward of Cape Bougainville.
September 5.
The following day at noon we were near Condillac Island, after which a
sea-breeze from the westward enabled us to pass Cape Voltaire, at which
point our last year's survey terminated. When we were within the Cape we
found an ebb-tide setting out of a bight, which trended deeply in to the
southward and appeared to be studded with rocky islands. This adverse
tide continued to run all the evening and prevented our reaching the
bottom; so that at sunset we dropped the anchor a few miles to the south
of Cape Voltaire.
To the westward of this position we counted twenty-three islands, the
northernmost of which were supposed to be the Montalivet Isles of Baudin.
The whole have an uninteresting and rocky appearance but are not
altogether destitute of vegetation: a greenish tinge upon the nearest
islet saved them from being condemned as absolutely sterile.
September 6.
The next morning a boat visited the outer north-easternmost islet, named
in the chart Water Island, which was found to be as rocky in reality as
it was in appearance. It is formed of a hard granular quartzose
sandstone, of a bluish-gray colour; the basis is disposed in horizontal
strata but the surface is covered with large amorphous rocks of the same
character that have evidently been detached and heaped together by some
convulsion of nature: over these a shallow soil is sprinkled, which
nourishes our old acquaintance spinifex, and a variety of plants of which
Mr. Cunningham collected more than twenty distinct known genera. The
exposed surfaces of the rocks are coloured by the oxide of iron, which is
so generally the case upon the northern and north-western coasts that the
name of Red Coast might with some degree of propriety be applied to a
great portion of this continent.
Mr. Hunter found a large quantity of bulbous-rooted plants; they proved
to be a liliaceous plant of the same species as those which we had before
found upon Sims' Island, the islands of Flinders' Group on the eastern
coast, and at Percy Island.
Public-domain text, read in full here on John Shaqi.
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