southward, without any bays to Cape Leeuwin. Off the cape is Naturaliste
Reef, in latitude 33 degrees 12 minutes, and longitude 114 degrees 59
minutes 8 seconds; it was seen by the French expedition. The land is here
of a moderate height, but of level aspect. There is a remarkable patch of
bare sand, in latitude 34 degrees 12 minutes, and longitude 114 degrees
57 minutes. It is the Tache blanche remarquable of De Freycinet's chart.
It lies about seven miles from the south extreme of the island.
...
APPENDIX A. SECTION 6.
OF THE WINDS AND WEATHER UPON THE SOUTH COAST. DIRECTIONS FOR KING GEORGE
THE THIRD'S SOUND, AND HYDROGRAPHICAL REMARKS RELATING TO BASS STRAIT.
SOUTH COAST.
Between the meridians of Cape Leeuwin and Bass Strait, the weather is
generally very unsettled and tempestuous; and, at certain seasons, very
much against a ship making the western passage from Port Jackson, which
is by passing through Bass Strait, and along the south coast; but it so
happens that at the time when ships cannot proceed through Torres Strait,
by reason of the Westerly Monsoon, namely, from the month of December to
that of March, easterly winds prevail upon the south coast, and are more
regular and strong in that space between the land and the parallel of
Bass Strait.* I have been told that the south-westerly gales that
sometimes occur during that season, seldom, if ever, blow home upon the
coast; and that when they do reach the land, they partake more of the
character of the sea breeze; be that as it may, a ship steering to the
westward should keep to the north of 40 degrees, in order to benefit by
the regularity of the wind, which to the south of that parallel generally
blows from some western quarter. From April to October the westerly gales
are very constant, and veer between South by West and North by East; but,
in the months of June and July, seldom veer to the southward of
South-West or northward of North-West; they are then accompanied by a
deep and heavy sea. The wind, in the summer season, generally revolves
with the sun, and, as the atmosphere becomes more dense, veers to the
South-East, with fine weather.
(*Footnote. Horsburgh volume 2 page 506.)
The marine barometer is here of considerable importance, as its rise
always precedes a south-east wind, and its fall a change from the
North-West; it seldom, however, stands lower than twenty-nine and a half
inches. The currents generally set to the north, and seld
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