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A General History & Collection of Voyages and Travels ... - Nauticus

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then squatted herself down, on her heels, on the top <strong>of</strong> all; thus making a kind <strong>of</strong> Dutch warming-pan, onwhich she sat as close as a hare on her seat. I should hardly have mentioned this operation, if I had thoughtit had no other view than to warm the old woman's backside. I rather suppose it was intended to cure somedisorder she might have on her, which the steams arising from the green celery might be a specific for. Iwas led to think so by there being hardly any celery in the place, we having gathered it long before; <strong>and</strong>grass, <strong>of</strong> which there was great plenty, would have kept the stones from burning the mat full as well, if thathad been all that was meant. Besides, the woman looked to me sickly, <strong>and</strong> not in a good state <strong>of</strong> health.Mr Wales, from time to time, communicated to me the observations he had made in this Sound fordetermining the longitude, the mean results <strong>of</strong> which give 174° 25' 7" 1/2 east, for the bottom <strong>of</strong> ShipCove, where the observations were made; <strong>and</strong> the latitude <strong>of</strong> it is 41° 5' 50" 1/2 south. In my chart,constituted in my former voyage, this place is laid down in 184° 54' 30" west, equal to 175° 5' 30" east.The error <strong>of</strong> the chart is therefore 0° 40' 0", <strong>and</strong> nearly equal to what was found at Dusky Bay; by which itappears that the whole <strong>of</strong> Tavai-poenamoo is laid down 40' too far east in the said chart, as well as in thejournal <strong>of</strong> the voyage. But the error in Eaheino-mauwe, is not more than half a degree, or thirty minutes;because the distance between. Queen Charlotte's Sound <strong>and</strong> Cape Palliser has been found to be greater by10' <strong>of</strong> longitude than it is laid down in the chart. I mention these errors, not from a fear that they will affecteither navigation or geography, but because I have no doubt <strong>of</strong> their existence; for, from the multitude <strong>of</strong>observations which Mr Wales took, the situation <strong>of</strong> few parts <strong>of</strong> the world is better ascertained than QueenCharlotte's Sound. Indeed, I might, with equal truth, say the same <strong>of</strong> all the other places where we madeany stay; for Mr Wales, whose abilities are equal to his assiduity, lost no one observation that couldpossibly be obtained. Even the situation <strong>of</strong> those isl<strong>and</strong>s, which we passed without touching at them, is, bymeans <strong>of</strong> Kendal's watch, determined with almost equal accuracy. The error <strong>of</strong> the watch from Otaheite tothis place was only 43' 39" 1/2 in longitude, reckoning at the rate it was found to go at, at that isl<strong>and</strong> <strong>and</strong> atTanna; but by reckoning at the rate it was going when last at Queen Charlotte's Sound, <strong>and</strong> from the time<strong>of</strong> our leaving it, to our return to it again, which was near a year, the error was 19' 31", 25 in time, or 4° 52'48" 1/4 in longitude. This error cannot be thought great, if we consider the length <strong>of</strong> time, <strong>and</strong> that we hadgone over a space equal to upwards <strong>of</strong> three-fourths <strong>of</strong> the equatorial circumference <strong>of</strong> the earth, <strong>and</strong>through all the climates <strong>and</strong> latitudes from 9° to 71°. Mr Wales found its rate <strong>of</strong> going here to be that <strong>of</strong>gaining 12",576, on mean time, per day.The mean result <strong>of</strong> all the observations he made for ascertaining the variation <strong>of</strong> the compass <strong>and</strong> the dip <strong>of</strong>the south end <strong>of</strong> the needle, the three several times we had been here, gave 14° 9' 1/5 east for the former;<strong>and</strong> 64° 36" 2/3 for the latter. He also found, from very accurate observations, that the time <strong>of</strong> high-waterpreceded the moon's southing, on the full <strong>and</strong> change days, by three hours; <strong>and</strong> that the greatest rise <strong>and</strong>fall <strong>of</strong> the water was five feet ten inches, <strong>and</strong> a half; but there were evident tokens on the beach, <strong>of</strong> itshaving risen two feet higher than ever it did in the course <strong>of</strong> his experiments.CHAPTER IV.FROM LEAVING NEW ZEALAND TO OUR RETURN TO ENGLAND.SECTION I.The Run from New Zeal<strong>and</strong> to Terra del Fuego, with the Range from Cape Deseada to Christmas Sound,<strong>and</strong> Description <strong>of</strong> that Part <strong>of</strong> the Coast.

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