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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