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t high, near the north end,* was selected by Sir John Franklin for the site of a lighthouse, the foundation of which he laid, after resigning the reins of government; it was the last benefit he was able to confer on the colony. (*Footnote. In latitude 40 degrees 43 minutes 36 seconds South, longitude 3 degrees 5 minutes 50 seconds West of Sydney, and 148 degrees 10 minutes 10 seconds East of Greenwich; variation, 10 east.) A well of indifferent water was found near the north-west end of the island; and some sealers had recently turned loose a couple of pigs, to which I added a third. Two small islets lie one mile and a half West-North-West from Swan Island, and a dangerous patch of rocks, one and a quarter North-West by West from the summit; they are all connected with the large island by shoal water. TIDES. We found the best anchorage to be a quarter of a mile off the south point of a sandy bay, near the outer end of the island. During the time we lay here for the purpose of obtaining a series of tidal observations,* and verifying a few of the principal points of Messrs. Forsyth and Pasco's survey, constant strong westerly gales prevailed; and from all the local information obtained it appeared that such was generally the case. (*Footnote. The result of these observations makes the time of high-water at the full and change of the moon 9 hours 36 minutes when the rise of the tide is six feet and three at neaps. The flood-stream comes from the eastward; and both it and the ebb is of 6 hours 15 minutes duration at springs; but during neaps the flood runs 7 hours 0 minutes and the ebb 5 hours 30 minutes. The interval of slack-water never exceeded a quarter of an hour, and the western stream begins 0 hours 30 minutes after low-water at springs, and 0 hours 50 minutes after it at neaps; whilst the eastern begins 0 hours 40 minutes after high-water at springs, and 0 hours 10 minutes before it at neaps. The velocity of the stream was from one to three knots, the strongest being the ebb, which at springs and with a strong westerly breeze attains a strength in the middle of the strait of nearly four knots, and causes, when opposed to the wind, a high-topping sea, dangerous for small craft. Whilst in other respects the tides are the same, the time of high-water at Preservation Island, though only at the northern side of the strait, is 1 hour 15 minutes later than at Swan Island. This great difference is caused by t
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