The Swedish port from which the expedition is to start will probably be Gothenburg. The time of departure is fixed for the beginning of July, 1878. The course will be shaped at first along the west coast of Norway, past North Cape and the entrance to the White Sea, to Matotschkin Sound in Novaya Zemlya.

The opening of a communication by sea between the rest of Europe and these regions, by Sir Hugh Willoughby and Richard Chancelor in 1553, was the fruit of the first exploring expedition sent out from England by sea. Their voyage also forms the first attempt to discover a north-east passage to China. The object aimed at was not indeed accomplished; but on the other hand, there was opened by the voyage in question the sea communication between England and the White Sea; the voyage thus forming a turning-point not only in the navigation of England and Russia, but also in the commerce of the world. It also demanded its sacrifice, Sir Hugh Willoughby himself, with all the men in the vessels under his command, having perished while wintering on the Kola peninsula. In our days thousands of vessels sail safely along this route.

With the knowledge we now possess of the state of the ice in the Murman Sea—so the sea between Kola and Novaya Zemlya is called on the old maps—it is possible to sail during the latter part of summer from the White Sea to Matotschkin without needing to fear the least hindrance from ice. For several decades back, however, in consequence of want of knowledge of the proper season and the proper course, the case has been quite different—as is sufficiently evident from the account of the difficulties and dangers which the renowned Russian navigator, Count Lütke, met with during his repeated voyages four summers in succession (1821-1824) along the west coast of Novaya Zemlya. A skilful walrus-hunter can now, with a common walrus-hunting vessel, in a single summer, sail further in this sea than formerly could an expedition, fitted out with all the resources of a naval yard, in four times as long time.

There are four ways of passing from the Murman Sea to the Kara Sea, viz:—

a. Yugor Sound—the Fretum Nassovicum of the old Dutchmen—between Vaygats Island and the mainland.

b. The Kara Port, between Vaygats Island and Novaya Zemlya.

c. Matotschkin Sound, which between 73° and 74° N. Lat. divides Novaya Zemlya into two parts, and, finally,

d. The course north of the double island. The course past the northernmost point of Novaya Zemlya is not commonly clear of ice till the beginning of the month of September, and perhaps ought, therefore, not to be chosen for an expedition having for its object to penetrate far to the eastward in this sea. Yugor Sound and the Kara Port are early free of fast ice, but instead, are long rendered difficult to navigate by considerable masses of drift ice, which are carried backwards and forwards in the bays on both sides of the sound by the currents which here alternate with the ebb and flow of the tide. Besides, at least in Yugor Sound, there are no good harbours, in consequence of which the drifting masses of ice may greatly inconvenience the vessels, which by these routes attempt to enter the Kara Sea. Matotschkin Sound, again, forms a channel nearly 100 kilometres long, deep and clear, with the exception of a couple of shoals, the position of which is known, which indeed is not usually free from fast ice until the latter half of July, but, on the other hand, in consequence of the configuration of the coast, is less subject to be obstructed by drift ice than the southern straits. There are good harbours at the eastern mouth of the sound. In 1875 and 1876 both the sound and the sea lying off it were completely open in the end of August, but the ice was much earlier broken up also on the eastern side, so that a vessel could without danger make its way among the scattered pieces of drift ice. The part of Novaya Zemlya which is first visited by the walrus-hunters in spring is usually just the west coast off Matotschkin.

In case unusual weather does not prevail in the regions in question during the course of early and mid-summer, 1878— for instance, very steady southerly winds, which would early drive the drift ice away from the coast of the mainland—I consider, on the grounds which I have stated above, that it will be safest for the expedition to choose the course by Matotschkin Sound.

We cannot, however, reckon on having, so early as the beginning of August, open water direct to Port Dickson at the mouth of the Yenisej, but must be prepared to make a considerable detour towards the south in order to avoid the masses of drift ice, which are to be met with in the Kara Sea up to the beginning of September. The few days' delay which may be caused by the state of the ice here, will afford, besides, to the expedition an opportunity for valuable work in examining the natural history and hydrography of the channel, about 200 fathoms deep, which runs along the east coast of Novaya Zemlya. The Kara Sea is, in the other parts of it, not deep, but evenly shallow (ten to thirty fathoms), yet without being fouled by shoals or rocks. The most abundant animal life is found in the before-mentioned deep channel along the east coast, and it was from it that our two foregoing expeditions brought home several animal types, very peculiar and interesting in a systematic point of view. Near the coast the algæ, too, are rich and luxuriant. The coming expedition ought, therefore, to endeavour to reach Matotschkin Sound so early that at least seven days' scientific work may be done in those regions.