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determined the longitude to be 235 deg. 15' 26" E., which was 14' 11" less than what the time-keeper gave. This longitude is made use of for settling that of the coast; and I have not a doubt of its being within a very few miles of the truth. Our difficulties now began to increase. In the evening the wind came to the N.W., blowing in squalls, with hail and sleet; and the weather being thick and hazy, I stood out to sea till near noon the next day, when I tacked, and stood in again for the land, which made its appearance at two in the afternoon, bearing E.N.E. The wind and weather continued the same; but, in the evening, the former veered more to the W. and the latter grew worse, which made it necessary to tack and stand off till four the next morning, when I ventured to stand in again. At four in the afternoon we saw the island, which, at six, extended from N.E. 1/2 E. to S.E. by S. about eight leagues distant. In this situation we tacked, and sounded; but a line of a hundred and sixty fathoms did not reach the ground. I stood off till midnight, then stood in again; and at half-past six we were within three leagues of the land, which extended from N. by E. 1/2 E. to S. 1/2 E.; each extreme about seven leagues distant. Seeing no signs of a harbour, and the weather being still unsettled, I tacked, and stretched off S.W. having then fifty-five fathoms water, over a muddy bottom. That part of the land which we were so near when we tacked, is of a moderate height, though in some places it rises higher within. It was diversified with a great many rising grounds and small hills; many of which were entirely covered with tall, straight trees; and others, which were lower, and grew in spots like coppices; but the interspaces, and sides of many of the rising grounds, were clear. The whole, though it might make an agreeable summer prospect, had now an uncomfortable appearance; as the bare grounds towards the coast were all covered with snow, which seemed to be of a considerable depth between the little hills and rising grounds; and in several places, toward the sea, might easily have been mistaken, at a distance, for white cliffs. The snow on the rising grounds was thinner spread; and farther inland, there was no appearance of any; from whence we might, perhaps, conclude, that what we saw toward the sea, had fallen during the night; which was colder than any we had experienced since our arrival on the coast; and we had somet
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