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









































































 -  50'
E. The latitude was determined by the meridian altitude of the sun, which
appeared, now and then, for a - Page 127
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50' E. The Latitude Was Determined By The Meridian Altitude Of The Sun, Which Appeared, Now And Then, For A

Few minutes, till three in the afternoon. Indeed the sky was, in general, so cloudy, and the weather so thick

And hazy, that we had very little benefit of sun or moon; very seldom seeing the face of either the one or the other. And yet, even under these circumstances, the weather, for some days past, could not be called very cold. It, however, had not the least pretension to be called summer weather, according to my ideas of summer in the northern hemisphere, as far as 60 deg. of latitude, which is nearly as far north as I have been.

In the evening we had three islands of ice in sight, all of them large; especially one, which was larger than any we had yet seen. The side opposed to us seemed to be a mile in extent; if so, it could not be less than three in circuit. As we passed it in the night, a continual cracking was heard, occasioned, no doubt, by pieces breaking from it.[4] For, in the morning of the 6th, the sea, for some distance round it, was covered with large and small pieces; and the island itself did not appear so large as it had done the evening before. It could not be less than 100 feet high; yet such was the impetuous force and height of the waves which were broken against it, by meeting with such a sudden resistance, that they rose considerably higher.

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