When Wrangel wrote that, he did not believe in the existence of the land which is to be found set out on his map in 177°E.L. and 71° N.L., and which, afterwards discovered by the Englishman Kellet, according to the saying, lucus a non lucendo, obtained the name of Wrangel Land. Now we know that the land spoken of by tradition actually exists, and therefore there is much that even tells in favour of its extending as far as to the archipelago on the north coast of America.

With this fresh light thrown upon it, the old Chukch woman's story ought to furnish a valuable hint for future exploratory voyages in the sea north of Behring's Straits, and an important contribution towards forming a judgment of the fate which has befallen the American Jeannette expedition, of which, while this is being written, accounts are still wanting.[245] Between us and the inhabitants of the present Chukch village at Irkaipij there soon arose very friendly relations. A somewhat stout, well-grown, tall and handsome man named Chepurin, we took at first to be chief. He was therefore repeatedly entertained in the gunroom, on which occasions small gifts were given him to secure his friendship. Chepurin had clearly a weakness for gentility and grandeur, and could now, by means of the barter he carried on with us and the presents he received, gratify his love of show to a degree of which he probably had never before dreamed. When during the last days of our stay he paid a visit to the Vega he was clad in a red woollen shirt drawn over his "pesk," and from either ear hung a gilt watch-chain, to the lower end of which a perforated ten-öre piece was fastened. Already on our arrival he was better clothed than the others, his tent was larger and provided with two sleeping apartments, one for each of his wives. But notwithstanding all this we soon found that we had made a mistake, when, thinking that a society could not exist without government, we assigned to him so exalted a position. Here, as in all Chukch villages which we afterwards visited, absolute anarchy prevailed.

At the same time the greatest unanimity reigned in the little headless community. Children, healthy and thriving, tenderly cared for by the inhabitants, were found in large numbers. A good word to them was sufficient to pave the way for a friendly reception in the tent. The women were treated as the equals of the men, and the wife was always consulted by the husband when a more important bargain than usual was to be made; many times it was carried through only after the giver of advice had been bribed with a neckerchief or a variegated handkerchief. The articles which the man purchased were immediately committed to the wife's keeping. One of the children had round his neck a band of pearls with a Chinese coin having a square hole in the middle, suspended from it; another bore a perforated American cent piece. None knew a word of Russian, but here too a youngster could count ten in English. They also knew the word "ship." In all the tents, reindeer stomachs were seen with their contents, or sacks stuffed full of other green herbs. Several times we were offered in return for the bits of sugar and pieces of tobacco which we distributed, wrinkled root-bulbs somewhat larger than a hazel nut, which had an exceedingly pleasant taste, resembling that of fresh nuts. A seal caught in a net among the ice during our visit was cut up in the tent by the women. On this occasion they were surrounded by a large number of children, who were now and then treated to bloody strips of flesh. The youngsters carried on the work of cutting up con amore, coquetting a little with their bloody arms and faces.

The rock which prevails in this region consists mainly of gabbro, which in the interior forms several isolated, black, plateau-formed hills, 100 to 150 metres high, between which an even, grassy, but treeless plain extends. It probably rests on sedimentary strata. For on the western side of Irkaipij the plutonic rock is seen to rest on a black slate with traces of fossils, for the most part obscure vegetable impressions, probably belonging to the Permian Carboniferous formation.

Uneasy at the protracted delay here I made an excursion to a hill in the neighbourhood of our anchorage, which, according to a barometrical measurement, was 129 metres high, in order, from a considerable height, to get a better view of the ice than was possible by a boat reconnaisance. The hill was called by the Chukches Hammong-Ommang. From it we had an extensive view of the sea. It was everywhere covered with closely packed drift-ice. Only next the land was seen an open channel, which, however, was interrupted in an ominous way by belts of ice. The plutonic rock, of which the hill was formed, was almost everywhere broken up by the action of the frost into angular blocks of stone, so that its surface was converted into an enormous stone mound. The stones were on the wind side covered with a translucent glassy ice-crust, which readily fell away, and added considerably to the difficulty of the ascent. I had previously observed the formation of such an ice-crust on the northernmost mountain summits of Spitzbergen.[246] It arises undoubtedly from the fall of super-cooled mist, that is to say of mist whose vesicles have been cooled considerably below the freezing-point without being changed to ice, which first takes place when, after falling, they come in contact with ice or snow, or some angular hard object. It is such a mist that causes the icing down of the rigging of vessels, a very unpleasant phenomenon for the navigator, which we experienced during the following days, when the tackling of the Vega was covered with pieces of ice so large, and layers so thick, that accidents might have happened by the falling of the ice on the deck.[247]

The dredgings here yielded to Dr. Kjellman some algæ, and to Dr. Stuxberg masses of a species of cumacea, Diastylis Rathkei Kr., of Acanthostephia Malmgreni Goës, and Liparis gelatinosus Pallas, but little else. On the steep slopes of the north side of Irkaipij a species of cormorant had settled in so large numbers that the cliff there might be called a true fowl-fell. A large number of seals were visible among the ice, and along with the cormorant a few other birds, principally phalaropes. Fish were now seen only in exceedingly small numbers.

Even in the summer, fishing here does not appear to be specially abundant, to judge from the fact that the Chukches had not collected any stock for the winter. We were offered, however, a salmon or two of small size.

On the 18th September[248] the state of the ice was quite unchanged. If a wintering was to be avoided, it was, however, not advisable to remain longer here. It had besides appeared from the hill-top which I visited the day before that an open water channel, only interrupted at two places by ice, was still to be found along the coast. The anchor accordingly was weighed, and the Vega steamed on, but in a depth of only 6 to 8 metres. As the Vega's draught is from 4.8 to 5 metres, we had only a little water under the keel, and that among ice in quite unknown waters. About twenty kilometres from the anchorage, we met with a belt of ice through which we could make our way though only with great difficulty, thanks to the Vega's strong bow enabling her to withstand the violent concussions. Our voyage was then continued, often in yet shallower water than before, until the vessel, at 8 o'clock in the morning, struck on a ground ice foot. The tide was falling, and on that account it was not until next morning that we could get off, after a considerable portion of the ground-ice, on whose foot the Vega had run up, had been hewn away with axes and ice-hatchets. Some attempts were made to blast the ice with gunpowder, but they were unsuccessful. For this purpose dynamite is much more efficacious, and this explosive ought therefore always to form part of the equipment in voyages in which belts of ice have to be broken through.