The great object of Antarctic exploration is to discover the outline of the Antarctic continent, and to study its physiography so far as the great ice-cap will admit of such researches. Among those who took an intelligent interest in this important question was the late Duke of Argyll’s father, who had the firmest grasp of the subject and the deepest insight. His view was that our efforts should be directed to discovering the physiography of this continental land previous to its being almost entirely concealed by the ice-cap. In that way alone—combined with series of deep sea soundings radiating from the shores of Antarctica to lands to the north—could its geological history, and possible former connection with other lands, be ascertained. Impressed with these views, we saw that those coasts must be sought where the mountains are more or less clear of the assumed ice-cap. The northern coasts forming the eastern half of the Victoria and all the Enderby Quadrant appeared to be ice cliffs only, and therefore unsuited. It was evident that coasts and mountains with an eastern aspect would alone enable us to obtain the desired knowledge. There are two such eastern coasts. These are the western side of the Ross Sea facing east, and the western side of the Weddell Sea, the coast of Graham Land facing east.

Victoria Land was selected for the first attempt, and a grand result was achieved by Captain Scott in his two expeditions. The great Victorian chain of mountains was traced from the Antarctic Circle to the apex of the quadrant, a distance of 1200 miles. The volcanic region of Ross Island was thoroughly explored. The basaltic irruptions were observed, together with the primitive rocks; the great unaltered formation now known as the “Beacon Sandstone” was discovered, the movements and character of its glaciers were noted, a complete geological survey was made from Granite Harbour to Koettlitz Glacier, and the peaks were measured. To crown all, Captain Scott and Dr Wilson made a large collection of the fossil flora which established the geological period of the rock formation. These fossils weighed 35 lb., but though worn out, and with strength failing fast, the gallant explorers would not leave them, but dragged these records, until they died. There is no more glorious and more touching event in the whole range of polar history.

Captain Scott observed that the Victorian mountains turned in the direction of Graham Land, and this conclusion now has to be proved. A branch seems to run down to the coast and to terminate in the heights of King Edward VII Land, thus enclosing the vast bay filled with Mr Ferrar’s “Ross piedmont.” It would not be surprising to find a minor range branching off to Enderby Land, which Biscoe described as mountainous.

The land and islands with an eastern aspect on the other side of Antarctica were partly explored by Captain Larsen, who made an important voyage down the east coast of Graham Land, and the fossil remains have been collected and described by Nordenskiöld and Gunnar Andersson. Next to Captain Scott’s great discoveries, the work of the Swedes has thrown most light on the former history of Antarctica.

There is something very fascinating in considering the analogy between the Ross and Weddell Seas and their shores on opposite sides of Antarctica. The Victorian Mountains on one side match the Graham Land mountains on the other. The interest is increased by the probability that they form one chain, and by the discovery that there are volcanic rocks peculiar to the Andes which have been found in Graham Land. Then there are the enormous icebergs in both seas pointing to the need for the further study of the wonderful ice-cap which conceals so much of Antarctica from our knowledge.

The Antarctic ice-cap was discovered and explored by Captain Scott, who penetrated into its solitudes for two hundred miles from the mountain range. Dr Mawson has also examined it from another direction. There is little or no interest in travelling over its monotonous surface, but numerous borings would reveal its depth and solid contents, as suggested by the late Sir John Murray. The greatest interest connected with the Antarctic ice-cap is to be found in the study of its glaciers, and of its edges, possibly mighty cliffs like the Ross piedmont, whence the vast icebergs are discharged.

The most important geographical discoveries which remain to be revealed in the Antarctic regions are the coasts and interiors of the Weddell and Ross Quadrants. A great part of the eastern side of Graham Land is still undiscovered, and it is not known whether it is a peninsula or an island. A plan for the exploration of this important area was ably sketched out by Lieut. Barne, but nothing has yet been done. The continuation of the Victorian chain of mountains possibly to Graham Land, 800 miles in length, likewise calls for investigation as a part entirely unknown. An ancient connection between Antarctica and South America may be revealed, when the warm current flowing south down the east side of the latter continent was not diverted but flowed directly into the far south. But these are but a tithe of the problems which Antarctica still offers. There is the enterprise of crossing the mountains to ascertain the character of the much smaller section of the continent in the Ross Quadrant; there is the survey of the southern part of Graham Land; the exploration of the coast to the eastward; the problem of the origins of the great icebergs. The Weddell Quadrant calls for an immense amount of geographical and other scientific work, which would give full occupation for more than one expedition.

In the Ross Quadrant there is a coast line of 1100 miles in extent to be discovered. Captain Scott’s work on King Edward VII Land on one side, Alexander and Charcot Lands on the other, are the boundary posts to this undiscovered Edwardian coast. All we know is that Captain Cook saw land in 71° S., that Bellingshausen sighted Peter Island a little further to the east, and that the Belgian expedition wintered over the continental shelf in about 71° S. The land is probably not a hundred miles further south. The ice-pack floats north from the coast during the navigable season, and in that case a ship might navigate along the Edwardian coast. It is possible that there may be one or more deep indentations, like the Ross Sea, when there would be a coast or coasts facing east whose exploration would throw further important light on the history of Antarctica.

Finally, in the Enderby Quadrant there is the “Challenger Gap” to be explored, so as to complete an examination of the region from Gaussberg to Kempe Land.

Fixed stations for meteorological, magnetic, and tidal observations ought to be established to carry out this excellent and useful work within the Antarctic Circle during a course of years, similar to that which Captain Scott achieved in M’Murdo Sound during four years. In no other part of the Arctic or Antarctic regions have observations been taken in one place for so long a time. But they are needed on other spots all round Antarctica.

There are many true lovers of geographical exploration for its own sake in the present generation, who look upon achievement as its own reward. We may, therefore, hope that the great work initiated by the Societies with such splendid results will be renewed by successors to Scott and Wilson, and that they will again and again raise the standard of duty and useful, if perilous, achievement. For such men there is a note of encouragement and sympathy deep down in the hearts of all true Britons.