While the desire to penetrate into the mysteries of the North held the mind of mankind from the earliest times, the very existence of a similar world of ice, at the opposite pole, was undreamed of until a few centuries back. At the time when the world was generally held to be a flat disc, this is not to be wondered at, seeing that there could only be one other side possible under that belief, and that side the "under world," into which it was not desirable that human beings should ever penetrate. But the time came when the world was demonstrated to be a sphere, and the more thoughtful of men realised the necessity of having some theory wherewith to explain what form the world would take at the opposite pole to the North. The theory which found most general acceptance was that which contended for a similar distribution of sea and land at the South as was currently supposed to exist at In the Middle Ages, when the Portuguese and Spaniards were sailing from sea to sea, and later, when their successors, the Dutch, roamed the ocean, carrying their flags to the East and the West, none seem to have penetrated into the ice-bound regions of the South. The Cape of Good Hope was doubled. Cape Horn was sailed round. Australia was located, and even the south of Tasmania was visited. But further south the world was still unknown. An explanation of this may be found in the fact that in southern latitudes the drift of ice is very much further away from the Pole than is the case in the north. In the northern hemisphere massive ice-floes are not encountered until the 70th parallel of latitude has been passed, while it is not until the 75th parallel is passed that the ice becomes so packed as to appear to be stationary. In the southern latitudes, on the other hand, drift ice is encountered in the 50th parallel, and by the time This may be due, in a large measure, to the small quantity of land existing in the south, as compared with the north. The heat of the sun does not radiate from the sea with the same intensity as it does from the earth, whence the ice, drifting from the south into the oceans nearer the equator, melts more slowly, and is consequently enabled to travel longer distances, thus lowering the temperature of the surrounding atmosphere and still further delaying the melting process. At a comparatively recent period, the limit of the floes, in the southern oceans, was much nearer the equator than it is to-day, for the most southerly parts of Africa, Australia, and America all show unmistakable evidences of having, within recent times, been under a great ice covering. It was not until 1600 that the first contact was made with the southern world of ice. Dirk Gerritz, a Dutch navigator, sailing with a squadron for the East Indies, was separated from his other ships while passing through the Straits of Magellan and was driven as far as 64° S. He discovered, in that latitude, a rocky coast line covered with snow. The discovery did not excite any great interest at the time, and, for a period of nearly two centuries, In 1772, Captain Cook, who had already done so much to reveal the southern hemisphere to the knowledge of man, left the Cape of Good Hope with two ships, the Resolution and the Adventure, in search of the continent believed to exist somewhere beyond the regions hitherto visited. In 48° 41' S. latitude, and 18° 24' E. longitude, a sudden fall in the temperature from 67° to 38° Fahr. was experienced. On the following day an iceberg, fifty feet in height and nearly half a mile in length, was sighted. The course was continued to the south, but the third day after sighting the first berg the sea had become so full of ice that no further progress to the south was possible, although the latitude was only 54° 50' S., the corresponding latitude in the northern hemisphere being that of the city of Hull. Skirting the ice-packs and working always to the southward, the vessels managed to reach 55° 16' S. during the next three days, some few seals, penguins, and other birds being seen on the floating ice as the ships passed. The temperature was never After a winter passed in the Pacific Ocean, Captain Cook took his ships again to the south, towards the end of the year, and by January 30, 1774, they were in 71° 10' S. latitude and 106° 54' W. longitude. Further progress to the south was barred by a line of high ice cliffs. Describing the circumstances Captain Cook wrote:— "At four o'clock A.M. we perceived the clouds, over the horizon to the south, to be of an unusual snow-white brightness, which we knew announced our approach to field ice. Soon after, it was seen from the topmast head, and at eight o'clock we Returning again to the Pacific in order that his men might recuperate after their hardships in the ice region, Captain Cook made a third attack upon the Antarctic problem the following year—1775—when he sailed to the south along the 27th meridian of west longitude. In latitude 59° S. three rocky As there appeared to be more probability of success being won on this voyage, the ships proceeded to explore the seas in the neighbourhood of these new lands; but a repetition of the trials and difficulties met in the previous year brought the hopes to nought. Whichever way they sailed they encountered ice, either in massive bergs, or lines of cliffs, miles in length. On February 6, 1775, the cold hostility of the region daunted even the brave heart of Captain Cook. He decided to turn back, writing in his log: "The risk one runs in exploring a coast in these unknown and icy seas is so great, that I can be bold enough to say that no man will ever venture further than I have done, and that the lands which lie to the south will never be explored." Modern achievement in the Antarctic regions forms a curious commentary on this outspoken Amongst others, Powell, in 1821, discovered land to the south of the South Shetlands, naming it Trinity Land; while Palmer, an American skipper, sailed along a coast to which he gave the name These repeated additions to the general knowledge gradually discredited Captain Cook's assertion. The newly opened areas were found to be replete with whales, seals, and other commercially valuable animals, and ships of the mercantile marine continued to push nearer and nearer the Pole. In 1822 a firm of traders sent out two vessels to the Antarctic under the command of Captain Weddell, after whom the great Antarctic seal is named. The vessels were small ships in comparison with the modern build. One, the larger, was the Jane, a brig of 160 tons, and the other a cutter, the Beaufoy, 65 tons. As Captain Weddell had already done much geographical service in the South, his employers instructed him to do all he could to discover fresh lands, and to penetrate as far into the ice to the South as was possible. He succeeded so well in carrying out the latter part of his instructions that, on February 28, 1823, he carried the flag to 74° 1' S. For some years nothing more of note was done, but in 1831, Captain Biscoe, on board the brig Tula, located land—named Enderby's Land, after his employers—in 65° 57' S. latitude and 47° 20' E. longitude. Wind and storms intervening, he was Two years earlier the French Government had taken up the work the British Government had neglected from the time of Captain Cook's condemnation, and had despatched two ships, the Astrolabe and the ZelÉe, to try and get into higher latitudes than those reached by Weddell. The Government of the United States also sent out vessels to continue the work already so successfully done by American whaling skippers. The voyages did not add materially to the discovery of land, although some valuable scientific facts were observed and recorded. The British Government then bestirred itself, and two ships, the Erebus and Terror, were placed under the command of Sir James C. Ross, with Captain Crozier as second in command, to proceed to the Antarctic regions and explore them. |