Farthest North, Vol. I: Being the Record of a Voyage of Exploration of the Ship 'Fram' 1893-1896Nansen, Fridtjof
History
Farthest North, Vol. I: Being the Record of a Voyage of Exploration of the Ship 'Fram' 1893-1896
Nansen, Fridtjof
"Fram" Expedition (1893-1896); Arctic regions -- Discovery and exploration; Nansen, Fridtjof, 1861-1930 -- Travel -- Arctic regions
These lanes never attained any great width, and there was consequently
no question of getting the Fram afloat in any of them; and even could
we have done so, it would have been of very little avail, as none of
them was large enough to have taken her more than a few cable-lengths
farther north. Sometimes there were indications in the sky that there
must be large stretches of open water in our vicinity, and we could
now and then see from the crow's-nest large spaces of clear water in
the horizon; but they could not have been large enough to be of much
use when it came to a question of pushing forward with a ship.
Sanguine folk on board, however, attached more importance to such
open stretches. June 15th I wrote in my diary: "There are several
lanes visible in different directions, but none of them is wide or
of any great extent. The mate, however, is always insisting that we
shall certainly get open water before autumn, and be able to creep
along northward, while with the rest, Sverdrup excepted, it seems
to be a generally accepted belief. Where they are to get their open
water from I do not know. For the rest, this is the first ice-bound
expedition that has not spent the summer spying after open water, and
sighing and longing for the ice to disperse. I only wish it may keep
together, and hurry up and drift northward. Everything in this life
depends on what one has made up one's mind to. One person sets forth
to sail in open water, perhaps to the very Pole, but gets stuck in
the ice and laments; another is prepared to get stuck in the ice, but
will not grumble even should he find open water. It is ever the safest
plan to expect the least of life, for then one often gets the most."
The open spaces, the lanes, and the rifts in the ice are, of course,
produced, like the pressure and packing, by the shifting winds and
the tidal currents that set the ice drifting first in one direction,
then in another. And they best prove, perhaps, how the surface of
the Polar Sea must be considered as one continuous mass of ice-floes
in constant motion, now frozen together, now torn apart, or crushed
against each other.
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