my intention of landing. The course was shaped southwards towards the sound, of so bad repute in the history of the Siberian Polar Sea, which separates Ljachoff's Island from the mainland.

So far as we could judge at a distance from the appearance of the rocks, Stolbovoj consisted of stratified rocks, Ljachoff's Island, on the contrary, like the mainland opposite, of high hills, much shattered, probably formed of Plutonic stone-masses. Between these there are extensive plains, which, according to a statement by the land surveyor CHVOINOFF, who by order of the Czar visited the island in 1775, are formed of ice and sand, in which lie imbedded enormous masses of the bones and tusks of the mammoth, mixed with the horns and skulls of some kind of ox and with rhinoceros' horns. Bones of the whale and walrus are not mentioned as occurring there, but "long small screw-formed bones," by which are probably meant the tusks of the narwhal.[233]

All was now clear of snow, with the exception of a few of the deeper clefts between the mountains. No traces of glaciers were visible, not even such small collections of ice as are to be found everywhere on Spitzbergen where the land rises a few hundred feet above the surface of the sea. Nor, to judge by the appearance of the hills, have there been any glaciers in former times, and this is certainly the case on the mainland. The northernmost part of Asia in that case has never been covered by such an ice-sheet as is assumed by the supporters of a general ice age embracing the whole globe.

The large island right opposite to Svjatoinos was discovered in 1770 by LJACHOFF, whose name the island now bears. In 1788 Billings' private secretary, MARTIN SAUER, met with Ljachoff at Yakutsk, but he was then old and infirm, on which account, when Sauer requested information regarding the islands in the Polar Sea, he referred him to one of his companions, ZAITAI PROTODIAKONOFF. He informed him that the discovery was occasioned by an enormous herd of reindeer which Ljachoff, in the month of April 1770, saw going from Svjatoinos towards the south, and whose track came over the ice from the north. On the correct supposition that the reindeer came from some land lying to the north, Ljachoff followed the track in a dog-sledge, and thus discovered the two most southerly of the New Siberian Islands, a discovery which was rewarded by the Czarina Catherine II. with the exclusive right to hunt and collect ivory on them.[234]

Ljachoff states the breadth of the sound between the mainland and the nearest large island at 70 versts or 40'. On Wrangel's map again the breadth is not quite 30'. On the mainland side it is bounded by a rocky headland projecting far into the sea, which often formed the turning point in attempts to penetrate eastwards from the mouth of the river Lena, and perhaps just on that account, like many other headlands dangerous to the navigator on the north coast of Russia, was called Svjatoinos (the holy cape), a name which for the oldest Russian Polar Sea navigators appears to have had the same signification as "the cape that can be passed with difficulty." No one however now thinks with any apprehension of the two "holy capes," which in former times limited the voyages of the Russians and Fins living on the White Sea to the east and west, and this, I am quite convinced, will some time be the case with this and all other holy capes in the Siberian Polar Sea.

The sea water in the sound was much mixed with river water and had a comparatively high temperature, even at a depth of nine to eleven metres. The animal life at the sea bottom was poor in species but rich in individuals, consisting principally of Idothea entomon, of which Dr. Stuxberg counted 800 specimens from a single sweep of the dredge. There were obtained at the same time, besides a few specimens of Idothea Sabinei, sponges and bryozoa in great abundance, and small mussels, crustacea, vermes, &c. Various fishes were also caught, and some small algæ collected. The trawl-net besides brought up from the bottom some fragments of mammoth tusks, and a large number of pieces of wood, for the most part sticks or branches, which appear to have stood upright in the clay, to judge from the fact that one of their ends was often covered with living bryozoa. These sticks often caused great inconvenience to the dredgers, by tearing the net that was being dragged along the bottom.

On the night preceding the 31st of August, as we steamed past Svjatoinos, a peculiar phenomenon was observed. The sky was clear in the zenith and in the east; in the west, on the other hand, there was a bluish-grey bank of cloud. The temperature of the water near the surface varied between +1° and +1°.6, that of the air on the vessel between +1°.5 and +1°.8. Although thus both the air and the water had a temperature somewhat above the freezing-point, ice was seen to form on the calm, mirror-bright surface of the sea. This ice consisted partly of needles, partly of a thin sheet. I have previously on several occasions observed in the Arctic seas a similar phenomenon, that is to say, have observed the formation of ice when the temperature of the air was above the freezing-point. On this occasion, when the temperature of the uppermost stratum of water was also above the freezing-point, the formation of ice was clearly a sort of hoar-frost phenomenon, caused by radiation of heat, perhaps both upwards towards the atmosphere and downwards towards the bottom layer of water, cooled below the freezing-point.

The whole day we continued our voyage eastwards with glorious weather over a smooth ice-free sea, and in the same way on the 1st September, with a gentle southerly wind, the temperature of the air at noon in the shade being +5°.6. On the night before the 2nd September the wind became northerly and the temperature of the air sank to -1°. Little land was seen, though we were still not very far from the coast. Near to it there was a broad ice-free, or nearly ice-free, channel, but farther out to sea ice commenced. The following night snow fell, so that the whole of the deck and the Bear Islands, which we reached on the 3rd September, were sprinkled with it.