Narrative of a Survey of the Intertropical and Western Coasts of Australia — Vol. 2: Performed between the years 1818 and 1822King, Philip Parker
History
Narrative of a Survey of the Intertropical and Western Coasts of Australia — Vol. 2: Performed between the years 1818 and 1822
King, Philip Parker
Australia -- Description and travel; Natural history -- Australia
Hence the coast trends to the North-West by North towards a patch of bare
sand, which is remarkable because the coast is not so sandy as it is more
to the south. At ten o'clock a very thick haze spread over the land and
so enveloped it that nothing could be distinguished. At noon, the brig
being in 28 degrees 25 minutes 42 seconds South, and 114 degrees 7
minutes 0 seconds East, the haze partially cleared away and showed that
the coast had changed its character, being now steep, and in some parts
cliffy, but still occasionally studded with spots of bare sand. In the
interior a rocky, flat-topped hill was seen; it is probably the Mount
Naturaliste of the French. The coast trends here in a North by West
direction.
The passage or channel between the Abrolhos Bank and the coast has been
distinguished by the name of Vlaming's ship, The Geelvink, since she was
the first vessel that passed them (Anno 1697). Captain Hamelin in the
Naturaliste also passed within them, imagining that he perceived them to
the eastward, but what he saw must have been the summit of Moresby's
Flat-topped Range.*
(*Footnote. So M. De Freycinet also thinks, for he says: "quelques
personnes n'osent assurer que nous ayons vu les Abrolhos; d'autres, et je
suis de ce nombre, peusent que ce que nous avons pris pour ce groupe
d'iles est une portion du Continent." Freycinet page 180.)
The soundings of the coast upon our track between Rottnest Island and the
Abrolhos have been gradually of a gravelly nature, mixed sometimes with
shelly sand, and were generally coarser as we approached the shore. In
some parts, particularly near Cape Naturaliste and Rottnest Island, the
bottom appeared to be a bed of small water-worn quartzose pebbles not
larger than a pin's head. Off Moresby's Flat-topped Range the bottom is
of a soft dark-gray-coloured sand of a very fine quality that would
afford good anchorage was it not for the constant swell that pervades
this stormy coast; the water was however much smoother than in other
parts, which might have been occasioned either by the Abrolhos bank's
breaking the sea, or from the temporary cessation of the wind, for it was
comparatively light to what it had been since our leaving Rottnest
Island.
Public-domain text, read in full here on John Shaqi.
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