As there was still a great deal of ice to windward, we continued our southwesterly course, keeping as close to the wind as possible. The weather was clear, and at 8 o'clock we sighted the mainland, with Dickson's Island ahead. It had been our intention to run in and anchor here, in order to put letters for home under a cairn, Captain Wiggins having promised to pick them up on his way to the Yenisei. But in the meantime the wind had fallen: it was a favorable chance, and time was precious. So we gave up sending our post, and continued our course along the coast. The country here was quite different from Yalmal. Though not very high, it was a hilly country, with patches and even large drifts of snow here and there, some of them lying close down by the shore. Next morning I sighted the southernmost of the Kamenni Islands. We took a tack in under it to see if there were animals of any kind, but could catch sight of none. The island rose evenly from the sea at all points, with steep shores. They consisted for the most part of rock, which was partly solid, partly broken up by the action of the weather into heaps of stones. It appeared to be a stratified rock, with strongly marked oblique strata. The island was also covered with quantities of gravel, sometimes mixed with larger stones; the whole of the northern point seemed to be a sand heap, with steep sand-banks towards the shore. The most noticeable feature of the island was its marked shore-lines. Near the top there was a specially pronounced one, which was like a sharp ledge on the west and north sides, and stretched across the island like a dark band. Nearer the beach were several other distinct ones. In form they all resembled the upper one with its steep ledges, and had evidently been formed in the same way--by the action of the sea, and more especially of the ice. Like the upper one, they also were most marked on the west and north sides of the island, which are those facing most to the open sea. To the student of the history of the earth these marks of the former level of the sea are of great interest, showing as they do that the land has risen or the sea sunk since the time they were formed. Like Scandinavia, the whole of the north coast of Siberia has undergone these changes of level since the Great Ice Age. It was strange that we saw none of the islands which, according to Nordenskiöld's map, stretch in a line to the northeast from Kamenni Islands. On the other hand, I took the bearings of one or two other islands lying almost due east, and next morning we passed a small island farther north. We saw few birds in this neighborhood--only a few flocks of geese, some Arctic gulls (Lestris parasitica and L. buffonii), and a few sea-gulls and tern.