New Zealand - A General History And Collection Of Voyages And Travels - Volume 14 - By Robert Kerr









































































 -  When the infusion was made
strong, it proved emetic to some in the same manner as green tea.

The inhabitants - Page 48
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When The Infusion Was Made Strong, It Proved Emetic To Some In The Same Manner As Green Tea.

The inhabitants of this bay are of the same race of people with those in the other parts of this country, speak the same language, and observe nearly the same customs.

These indeed seem to have a custom of making presents before they receive any, in which they come nearer to the Otaheiteans than the rest of their countrymen. What could induce three or four families (for I believe there are not more) to separate themselves so far from the society of the rest of their fellow-creatures, is not easy to guess. By our meeting with inhabitants in this place, it seems probable that there are people scattered over all this southern island. But the many vestiges of them in different parts of this bay, compared with the number that we actually saw, indicates that they live a wandering life; and, if one may judge from appearances and circumstances, few as they are, they live not in perfect amity, one family with another. For, if they did, why do they not form themselves into some society? a thing not only natural to man, but observed even by the brute creation.

I shall conclude this account of Dusky Bay with some observations made and communicated to me by Mr Wales. He found by a great variety of observations, that the latitude of his observatory at Pickersgill Harbour, was 45 deg. 47' 26" half south; and, by the mean of several distances of the moon from the sun, that its longitude was 106 deg. 18' E., which is about half a degree less than it is laid down in my chart constructed in my former voyage. He found the variation of the needle or compass, by the mean of three different needles, to be 13 deg. 49' E, and the dip of the south end 70 deg. 5' three quarters. The times of high water, on the full and change days, he found to be at 10 deg. 57', and the tide to rise and fall, at the former eight feet, at the latter five feet eight inches. This difference, in the rise of the tides between the new and full moon, is a little extraordinary, and was probably occasioned at this time by some accidental cause, such as winds, &c., but, be it as it will, I am well assured there was no error in the observations.

Supposing the longitude of the observatory to be as above, the error of Mr Kendal's watch, in longitude, will be 1 deg. 48' minus, and that of Mr Arnold's 39 deg. 25'. The former was found to be gaining 6",461 a-day on mean time, and the latter losing 99",361. Agreeably to these rates the longitude by them was to be determined, until an opportunity of trying them again.

I must observe, that in finding the longitude by Mr Kendal's watch, we suppose it to have gone mean time from the Cape of Good Hope. Had its cape rate been allowed, the error would not have been so great.

SECTION VI.

Passage from Dusky Bay to Queen Charlottes Sound, with an Account of some Water Spouts, and of our joining the Adventure.

After leaving Dusky Bay, as hath been already mentioned, I directed my course along shore for Queen Charlotte's Sound, where I expected to find the Adventure. In this passage we met with nothing remarkable, or worthy of notice, till the 17th at four o'clock in the afternoon. Being then about three leagues to the westward of Cape Stephens; having a gentle gale at west by south, and clear weather, the wind at once flattened to a calm, the sky became suddenly obscured by dark dense clouds, and seemed to forebode much wind. This occasioned as to clew up all our sails, and presently after six water-spouts were seen. Four rose and spent themselves between us and the land; that is, to the south-west of us, the fifth was without us, the sixth first appeared in the south-west, at the distance of two or three miles at least from us. Its progressive motion was to the north-east, not in a straight but in a crooked line, and passed within fifty yards of our stern, without our feeling any of its effects. The diameter of the base of this spout I judged to be about fifty or sixty feet; that is, the sea within this space was much agitated, and foamed up to a great height. From this a tube, or round body, was formed, by which the water or air, or both, was carried in a spiral stream up to the clouds. Some of our people said they saw a bird in the one near us, which was whirled round like the fly of a jack, as it was carried upwards. During the time these spouts lasted, we had now and then light puffs of wind from all points of the compass, with some few slight showers of rain, which generally fell in large drops; and the weather continued thick and hazy for some hours after, with variable light breezes of wind. At length the wind fixed in its old point, and the sky resumed its former serenity. Some of these spouts appeared at times to be stationary; and at other times to have a quick but very unequal progressive motion, and always in a crooked line, sometimes one way and sometimes another; so that, once or twice, we observed them to cross one another. From the ascending motion of the bird, and several other circumstances, it was very plain to us that these spouts were caused by whirlwinds, and that the water in them was violently hurried upwards, and did not descend from the clouds as I have heard some assert. The first appearance of them is by the violent agitation and rising up of the water; and, presently after, you see a round column or tube forming from the clouds above, which apparently descends till it joins the agitated water below.

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