Page:The Worst Journey in the World volume 1.djvu/282

Rh 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.