umb of comfort comes on finding that we have not drifted to the
eastward appreciably.

_Friday, December_ 23.--The wind fell light at about ten last night
and the ship swung round. Sail was set on the fore, and she pushed a
few hundred yards to the north, but soon became jammed again. This
brought us dead to windward of and close to a large berg with the
wind steadily increasing. Not a very pleasant position, but also
not one that caused much alarm. We set all sail, and with this help
the ship slowly carried the pack round, pivoting on the berg until,
as the pressure relieved, she slid out into the open water close
to the berg. Here it was possible to 'wear ship,' and we saw a fair
prospect of getting away to the east and afterwards south. Following
the leads up we made excellent progress during the morning watch,
and early in the forenoon turned south, and then south-west.

We had made 8 1/2' S. 22 E. and about 5' S.S.W. by 1 P.M., and could
see a long lead of water to the south, cut off only by a broad strip
of floe with many water holes in it: a composite floe. There was just
a chance of getting through, but we have stuck half-way, advance and
retreat equally impossible under sail alone. Steam has been ordered
but will not be ready till near midnight. Shall we be out of the pack
by Christmas Eve?

The floes to-day have been larger but thin and very sodden. There
are extensive water pools showing in patches on the surface, and one
notes some that run in line as though extending from cracks; also here
and there close water-free cracks can be seen. Such floes might well
be termed '_composite_' floes, since they evidently consist of old
floes which have been frozen together--the junction being concealed
by more recent snow falls.

A month ago it would probably have been difficult to detect
inequalities or differences in the nature of the parts of the floes,
but now the younger ice has become waterlogged and is melting rapidly,
hence the pools.

I am inclined to think that nearly all the large floes as well as
many of the smaller ones are 'composite,' and this would seem to show
that the cementing of two floes does not necessarily mean a line of
weakness, provided the difference in the thickness of the cemented
floes is not too great; of course, young ice or even a single season's
sea ice cannot become firmly attached to the thick old bay floes,
and hence one finds these isolated even at this season of the year.