The Worst Journey in the World Apsley Cherry-Garrard (novel books to read TXT) 📖
- Author: Apsley Cherry-Garrard
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Oates trained them and fed them as though they were to run in the Derby. They were exercised whenever possible throughout the winter and spring by those who were to lead them on the actual journey. Fresh and good food was found in the shape of oil-cake and oats, a limited quantity of each of which had been brought and was saved for the actual Polar Journey, and everything which care and foresight could devise was done to save them discomfort. It is a grim life for animals, but in the end we were to know that up to the time of that bad blizzard almost at the Glacier Gateway, which was the finishing post of these plucky animals, they had fed all they needed, slept as well and lived as well as any, and better than most horses in ordinary life at home. “I congratulate you, Titus,” said Wilson, as we stood under the shadow of Mount Hope, with the ponies’ task accomplished, and “I thank you,” said Scott.
Titus grunted and was pleased.
Transport difficulties for the Polar Journey were considerable, but in every other direction the outlook was bright. The men who were to do the sledging had been away from Winter Quarters for three months. They had had plenty of sledging experience, some of it none too soft. The sledges, clothing, man-food, and outfit generally were excellent, although some changes were suggested and could be put into effect. There was no obvious means, however, of effecting the improvement most desired, a satisfactory snowshoe for the ponies.
The work already accomplished was enormous. On the Polar Journey the ponies and dogs could now travel light for the first hundred and thirty geographical miles, when, at One Ton Camp, they would for the first time take their full loads: the advantage of being able to start again with full loads when so far on your way is obvious when it is considered that the distance travelled depends upon the weight of food that can be carried. During the geological journey on the western side of the Sound, Taylor and his party had carried out much useful geological work in Dry Valley and on the Ferrar and Koettlitz Glaciers, which had been accurately plotted for the charts, and had been examined for the first time by an expert physiographer and ice specialist. The ordinary routine of scientific and meteorological observations usual with all Scott’s sledging parties was observed.
Further, at Cape Evans there had been running for more than three months a scientific station, which rivalled in thoroughness and exactitude any other such station in the world. I hope that later a more detailed account may be given of this continuous series of observations, some of them demanding the most complex mechanism, and all of them watched over by enthusiastic experts. It must here suffice to say that we who on our return saw for the first time the hut and its annexes completely equipped were amazed; though perhaps the gadget which appealed most to us at first was the electric apparatus by which the cook, whose invention it was, controlled the rising of his excellent bread.
Glad as we were to find it all and to enjoy the food, bath and comfort which it offered, we had no illusions about Cape Evans itself. It is uninteresting, as only a low-lying spit of black lava covered for the most part with snow, and swept constantly by high winds and drift, can be uninteresting. The kenyte lava of which it is formed is a remarkable rock, and is found in few parts of the world: but when you have seen one bit of kenyte you have seen all. Unlike the spacious and lofty Hut Point Peninsula, thirteen miles to the south, it has no outstanding hills and craters; no landmarks such as Castle Rock. Unlike the broad folds of Cape Royds, six miles to the north, it has none of the rambling walks and varied lakes, in which is found most of the limited plant life which exists in these latitudes, and though a few McCormick skuas meet here, there is no nursery of penguins such as that which makes Cape Royds so attractive in summer. Nor has the Great Ice Sheet, which reached up Erebus and spread over the Ross Sea in the past, spilled over Cape Evans in its retreat a wealth of foreign granites, dolerites, porphyrys and sandstone such as cover the otherwise dull surface round Shackleton’s old Winter Quarters.
Cape Evans is a low lava flow jutting out some three thousand feet from the face of the glaciers which clothe the slopes of Erebus. It is roughly an equilateral triangle in shape, at its base some three thousand feet (9/16th mile) across. This baseline, which divides the cape from the slopes of Erebus and the crevassed glaciers and giant icefalls which clothe them, consists of a ramp with a slope of thirty degrees, and a varying height of some 100 to 150 feet. From our hut, four hundred yards away, it looks like a great embankment behind which rises the majestic volcano Erebus, with its plume of steam and
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