eld of ice extend as far as N.E. But
this happened not to be the northern point; for at eleven o'clock we were
obliged to tack to avoid it.

At two o'clock the next morning we stood again to the northward, with the
wind at N.W. by W., thinking to weather the ice upon this tack; on which we
stood but two hours, before we found ourselves quite imbayed, being then in
latitude 55 deg. 8', longitude 24 deg. 3'. The wind veering more to the north, we
tacked and stood to the westward under all the sail we could carry, having
a fresh breeze and clear weather, which last was of short duration. For at
six o'clock it became hazy, and soon after there was thick fog; the wind
veered to the N.E., freshened and brought with it snow and sleet, which
froze on the rigging as it fell. We were now enabled to get clear of the
field of ice: but at the same time we were carried in amongst the ice
islands, in a manner equally dangerous, and which with much difficulty we
kept clear of.

Dangerous as it is to sail among these floating rocks (if I may be allowed
to call them so) in a thick fog, this, however, is preferable to being
entangled with immense fields of ice under the same circumstances. The
great danger to be apprehended in this latter case, is the getting fast in
the ice; a situation which would be exceedingly alarming. I had two men on
board that had been in the Greenland trade; the one of them in a ship that
lay nine weeks, and the other in one that lay six weeks, fast in this kind
of ice, which they called packed ice. What they called field ice is
thicker; and the whole field, be it ever so large, consists of one piece.
Whereas this which I call field-ice, from its immense extent, consists of
many pieces of various sizes, both in thickness and surface, from thirty or
forty feet square to three or four, packed close together, and in places
heaped one upon another. This, I am of opinion, would be found too hard for
a ship's side, that is not properly armed against it. How long it may have
lain, or will lie here, is a point not easily determined. Such ice is found
in the Greenland seas all the summer long; and I think it cannot be colder
there in the summer, than it is here. Be this as it may, we certainly had
no thaw; on the contrary, the mercury in Fahrenheit's thermometer kept
generally below the freezing point, although it was the middle of summer.

It is a general opinion, that the ice I have been speaking of, is formed in
bays