The light-coloured water extends for fourteen miles North West by West 1/2 West from Adele Island, but there is reason to think that the water is deep over the greater part of it; for we crossed over its tail, and sounded in forty-five fathoms without finding bottom, whilst in the darker-coloured water on either side of it, we had forty-two and forty-four fathoms.
POINT SWAN is the north-easternmost point of the land of Cape Leveque; it has an island close off its extremity, round which the tide rushes with great force, and forms a line of ripplings for ten miles to the West-North-West, through which, even in the Bathurst, we found it dangerous to pass.

Five miles to the north-eastward of the point are two small rocky islets, two miles apart from each other.
CAPE LEVEQUE is low and rocky, with a small islet close to its extremity: its extreme is in latitude 16 degrees 21 minutes 50 seconds, and longitude 122 degrees 56 minutes 35 seconds.

Between the cape and Point Swan, there is a sandy bay, fronted by a bed of rocks.

It was in this bay that the Buccaneers anchored, which Dampier has so well described.
The coast between CAPES LEVEQUE and BORDA extending South 40 degrees West nineteen miles, is low and rocky, and the country sandy and unproductive.
Between Cape Borda and Point Emeriau is a bay ten miles deep, backed by very low sandy land; and five miles further is another bay, that appeared to be very shoal: thence the coast extends to the South-West for twenty-three miles to CAPE BASKERVILLE; it is low and sandy, like that to the northward, but the interior is higher, and with some appearance of vegetation.
Thirteen miles from the shore are the LACEPEDE ISLANDS; they are three in number, and surrounded by a reef nine miles long by five wide.

They lie in a North-West direction, and are two miles apart: the north-westernmost is in latitude 16 degrees 49 minutes 40 seconds, and longitude 122 degrees 7 minutes 20 seconds: they are low and slightly clothed with bushes, and seem to be little more than the dry parts of the reef, on which a soil has been accumulated, and in time produced vegetation.