The sail (of pandanus matting) is a long parallelogram, twelve feet by three, its sides secured by two tough slender poles, between which it is stretched, and which serve both as masts and yards. In making sail one of the poles is shipped, two stays from the centre leading fore and aft are then set up, after which the second pole is fixed and secured by stays, so as to give the sail the requisite inclination. We frequently saw a second smaller sail set before the first, at the distance of eight or ten feet, and managed precisely in the same way, but, even with both sails set, owing to the disproportion between the spread of canvas and the bulk of the canoe, the latter moves slowly at all times, and on a wind makes much leeway.
SAIL FROM REDSCAR BAY.
December 31st.
We sailed yesterday from our anchorage in Redscar Bay, but did not clear the sunken ridge of coral in the offing—a submarine extension of the Barrier Reef, stretching between Low Island and the vicinity of South-west Cape—until this forenoon, when we got out of soundings. The Bramble is to remain behind for three or four weeks upon the coast, to fill up various blanks in the chart between this and Rossel Island, while we are to make the best of our way to the Duchateau Islands, to obtain a meridian distance, and thence proceed direct to Sydney.
January 6th, 1850.
Our passage to the Duchateau Isles, a distance of less than 400 miles, has been protracted by the prevalence of light winds, although these were generally favourable, or from the westward. Occasional calms, squalls, and rain occurred, but the weather generally was finer than during the South-East monsoon.
CLEARNESS OF THE ATMOSPHERE.
As an instance of the clearness of the atmosphere, so different from what we had usually experienced during our former visit to these shores, it may be mentioned, that on one occasion during a light breeze from the north-west we clearly saw Mount Yule (10,046 feet high) and the summit of Mount Owen Stanley, distant respectively, one hundred and twenty, and eighty miles from the ship. On this occasion also we had a full view of the whole of Mount Astrolabe, which although 3,824 feet in greatest height, and appearing to D’Urville as he ran past to be the highest land on this portion of the coast, is rendered quite insignificant by the lofty though distant range behind. Mount Astrolabe differs in character from any other of the New Guinea mountains seen by us, indicating a different geological formation. The summit extends thirteen miles, running parallel with the coastline and distant from it about eight miles. Viewed from the south-westward the outline is regular, exhibiting a series of nearly flat tops with slight interruptions, but from the southward it appears as a succession of terraces or projecting cliffs, precipitous in front near the summit, with a long steep slope below, probably of debris, while the flat top slopes backwards with a very gentle declivity. Owen Stanley Range again presented quite a different aspect as seen on the occasion alluded to, when nearly one half of its whole length (300 miles) from Mount Yule to Heath Bay was in full view: the outline was irregular but never suddenly so, and no peaks or other remarkable points were seen.