n one morning, as he looked round at the
cold glaciers and naked cliffs, not knowing where he was, he heard a dog
bark. Intensely excited, he started towards the sound, to be met by the
leader of the English Jackson-Harmsworth Expedition whose party was
wintering there, and who first gave him the definite news that he was on
Franz Josef Land. Nansen and Johansen were finally landed at Vardo in the
north of Norway, to learn that no tidings had yet been heard of the Fram.
That very day she cleared the ice which had imprisoned her for nearly
three years.
I cannot go into the Fram's journey save to say that she had drifted as
far north as 85 deg. 55' N., only eighteen geographical miles south of
Nansen's farthest north. But the sledge journey and the winter spent by
the two men has many points in common with the experience of our own
Northern Party, and often and often during the long winter of 1912 our
thoughts turned with hope to Nansen's winter, for we said if it had been
done once why should it not be done again, and Campbell and his men
survive.
Before Nansen started, the spirit of adventure, which has always led men
into the unknown, combined with the increased interest in knowledge for
its own sake to turn the thoughts of the civilized world southwards. It
was becoming plain that a continent of the extent and climate which this
polar land probably possessed might have an overwhelming influence upon
the weather conditions of the whole Southern Hemisphere. The importance
of magnetism was only rivalled by the mystery in which the whole subject
was shrouded: and the region which surrounded the Southern Magnetic Pole
of the earth offered a promising field of experiment and observation. The
past history, through the ages, of this land was of obvious importance to
the geological story of the earth, whilst the survey of land formations
and ice action in the Antarctic was more useful perhaps to the
physiographer than that of any other country in the world, seeing that he
found here in daily and even hourly operation the conditions which he
knew had existed in the ice ages of the past over the whole world, but
which he could only infer from vestigial remains. The biological
importance of the Antarctic might be of the first magnitude in view of
the significance which attaches to the life of the sea in the
evolutionary problem.
And it was with these objects and ideals that Scott's first expedition,
known officially as the
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