Another correspondent states, on the ground of observations made during Tschikanovski's expedition, that in 1875 the sea off the Olonek was completely free of ice, but adds at the same time that the year in this respect was an exceptional one. The Arctic Ocean, not only in summer, but also during winter, is occasionally free of ice, and at a distance of 200 versts from the coast, the sea is open even in winter, in what direction, however, is uncertain. The latter fact is also confirmed by Wrangel's journeys with dog-sledges on the ice in 1821-1823.

A third person says, "According to the information which I have received, the north coast, from the mouth of the Lena to that of the Indigirka, is free from ice from July to September. The north wind drives the ice towards the coast, but not in large masses. According to the observations of the men who search for mammoth tusks, the sea is open as far as the southern part of the New Siberia Islands. It is probable that these islands form a protection against the ice in the Werchnojan region. It is otherwise on the Kolyma coast; and if the Kolyma can be reached from Behring's Straits, so certainly can the Lena."

The circumstance that the ice during summer is driven from the coast by southerly winds, yet not so far but that it returns, in larger or smaller quantity, with northerly winds, is further confirmed by other correspondents, and appears to me to show that the New Siberian Islands and Wrangel's Land only form links in an extensive group of islands, running parallel with the north coast of Siberia, which, on the one hand, keeps the ice from the intermediate sea from drifting away altogether, and favours the formation of ice during winter, but, on the other hand, protects the coast from the Polar ice proper, formed to the north of the islands. The information I have received besides, refers principally to the summer months. As in the Kara Sea, which formerly had a yet worse reputation, the ice here, too, perhaps, melts away for the most part during autumn, so that at this season we may reckon on a pretty open sea.

Most of the correspondents, who have given information about the state of the ice in the Siberian Polar Sea, concern themselves further with the reports current in Siberia, that American whalers have been seen from the coast far to the westward. The correctness of these reports was always denied in the most decided way: yet they rest, at least to some extent, on a basis of fact. For I have myself met with a whaler, who for three years in a steamer carried on trade with the inhabitants of the coast from Cape Yakan to Behring's Straits. He was quite convinced that some years at least it would be possible to sail from Behring's Straits to the Atlantic. On one occasion he had returned through Behring's Straits as late as the 17th October. From what I have thus stated, it follows,—

That the ocean lying north of the north coast of Siberia, between the mouth of the Yenisej and Tschaun Bay, has never been ploughed by the keel of any proper sea-going vessel, still less been traversed by any steamer specially fitted out for navigation among ice:

That the small vessels with which it has been attempted to traverse this part of the ocean never ventured very far from the coast:

That an open sea, with a fresh breeze, was as destructive for them, indeed more destructive, than a sea covered with drift ice:

That they almost always sought some convenient winter harbour, just at that season of the year when the sea is freest of ice, namely, late summer or autumn:

That, notwithstanding the sea from Cape Chelyuskin to Bearing's Straits has been repeatedly traversed, no one has yet succeeded in sailing over the whole extent at once:

That the covering of ice formed during winter along the coast, but probably not in the open sea, is every summer broken up, giving origin to extensive fields of drift ice, which are driven, now by a northerly wind towards the coast, now by a south wind out to sea, yet not so far but that it comes back to the coast after some days' northerly wind; whence it appears probable that the Siberian Sea is, so to say, shut off from the Polar Sea proper, by a series of islands, of which, for the present, we know only Wrangel's Land and the islands which form New Siberia.