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uese to India, and Japan; and in case our expedition succeeds in reaching the Suez Canal, after having circumnavigated Asia, there will meet us there a splendid work, which, more than any other, reminds us, that what to-day is declared by experts to be impossible, is often carried into execution to-morrow. I am also fully convinced that it is not only possible to sail along the north coast of Asia, provided circumstances are not too unfavourable, but that such an enterprise will be of incalculable practical importance, by no means directly, as opening a new commercial route, but indirectly, by the impression which would thereby be communicated of the practical utility of a communication by sea between the ports of North Scandinavia and the Obi and Yenisej, on the one hand, and between the Pacific Ocean and the Lena on the other. Should the expedition, contrary to expectation, not succeed in carrying out the programme which has been arranged in its entirety, it ought not to be looked upon as having failed. In such a case the expedition will remain for a considerable time at places on the north coast of Siberia, suitable for scientific research. Every mile beyond the mouth of the Yenisej is a step forward to a complete knowledge of our globe--an object which sometime or other must be attained, and towards which it is a point of honour for every civilised nation to contribute in its proportion. Men of science will have an opportunity, in these hitherto unvisited waters, of answering a number of questions regarding the former and present state of the Polar countries, of which more than one is of sufficient weight and importance to lead to such an expedition as the present. I may be permitted here to refer to only a few of these. If we except that part of the Kara Sea which has been surveyed by the two last Swedish expeditions, we have for the present no knowledge of the vegetable and animal life in the sea which washes the north coast of Siberia. Quite certainly we shall here, in opposition to what has been hitherto supposed, meet with the same abundance of animals and plants as in the sea round Spitzbergen. In the Siberian Polar sea, the animal and vegetable types, so far as we can judge beforehand, exclusively consist of survivals from the glacial period, which next preceded the present, which is not the case in the Polar Sea, where the Gulf Stream distributes its waters, and whither it thus carries types from
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