The Voyages and Adventures of Captain Hatteras. Jules Verne. Читать онлайн. Newlib. NEWLIB.NET

Автор: Jules Verne
Издательство: Bookwire
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Жанр произведения: Языкознание
Год издания: 0
isbn: 9783746746333
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face.

      The three sailors, Clifton, Gripper, and Pen, seemed to be the least enthusiastic and determined; they were inclined to grumbling. Gripper had even wished to break his engagement when the time came for sailing, and only a feeling of shame prevented him. If things went well, if they encountered no excessive dangers, and their toil was not too severe, these three men could be counted on; but they were hard to please with their food, for they were inclined to gluttony. In spite of their having been forewarned, they were by no means pleased with being teetotalers, and at their meals they used to miss their brandy or gin; but they made up for it with the tea and coffee which were distributed with a lavish hand.

      As for the two engineers, Brunton and Plover, and the stoker, Warren, they had been so far well satisfied with having nothing to do.

      Shandon knew therefore what to expect from each man. On the 14th of April, the Forward crossed the Gulf Stream, which, after following the eastern coast of America as far as Newfoundland, turns to the northeast and moves towards the shore of Norway. They were then in latitude 51°37', and longitude 22°37', two hundred miles from the end of Greenland. The weather grew colder; the thermometer fell to 32°, the freezing-point.

      The doctor, without yet putting on his arctic winter dress, was wearing a suit of sea-clothes, like all the officers and sailors; he was an amusing sight in his high boots, in which he could not bend his legs, his huge tarpaulin hat, his trousers and coat of the same material; in heavy rain, or when the brig was shipping seas, the doctor used to look like a sort of sea-monster, a comparison which always flattered him.

      For two days the sea was very rough; the wind veered to the northwest, and delayed the Forward. From the 14th to the 16th of April there was still a high sea running; but on Monday there fell a heavy shower which almost immediately had the effect of calming the sea. Shandon called the doctor's attention to it.

      “Well,” said the doctor, “that confirms the curious observations of the whaler Scoresby, who was a member of the Royal Society of Edinburgh, of which I have the honor to be a corresponding member. You see that while the rain is falling the waves are hardly to be noticed, even when the wind is strong. On the other hand, in dry weather the sea would be rougher even with a gentler wind”

      “But what is the explanation of it, Doctor?”

      “It's very simple; there is no explanation.”

      At that moment the ice-master, who as on watch in the topmast cross-trees, cried out that there was a floating mass on the starboard quarter, about fifteen miles to windward.

      “An iceberg in these latitudes!” cried the doctor.

      Shandon turned his glass in that direction, and corroborated the lookout's words.

      “That's strange,” said the doctor.

      “Are you surprised?” asked the commander, laughing. “What! are we lucky enough to find anything that will surprise you?”

      “I am surprised without being surprised,” answered the doctor, smiling, “since the brig Ann Poole, of Greenspond, was caught in the ice in the year 1813, in the forty-fourth degree of north latitude, and Dayement, her captain, saw hundreds of icebergs.”

      “Good,” said Shandon; “you can still teach us a great deal about them.”

      “O, not so very much!” answered Clawbonny, modestly, “except that ice has been seen in very much lower latitudes.”

      “That I know, my dear Doctor, for when I was a cabin-boy on the sloop-of-war, Fly—”

      “In 1818,” continued the doctor, “at the end of March, or it might have been the beginning of April, you passed between two large fields of floating ice, in latitude forty-two.”

      “That is too much!” exclaimed Shandon.

      “But it's true; so I have no need to be surprised, now that we are two degrees farther north, at our sighting an iceberg.”

      “You are bottled full of information, Doctor,” answered the commander; “one needs only draw the cork.”

      “Very well, I shall be exhausted sooner than you think; and now, Shandon, if we can get a nearer view of this phenomenon, I should be the gladdest of doctors.”

      “Exactly, Johnson,” said Shandon, summoning the boatswain; “I think the wind is freshening.”

      “Yes, Commander,” answered Johnson, “we are making very little headway, and soon we shall feel the currents from Davis Strait.”

      “You are right, Johnson, and if we mean to make Cape Farewell by the 20th of April, we must go under steam, or we shall be cast on the coast of Labrador.—Mr. Wall, give the order to light the fires.”

      The mate's orders were obeyed; an hour later the engines were in motion; the sails were furled; and the screw, turning through the waves, was driving the Forward rapidly in the teeth of the northwest wind.

      Chapter VI.

      The Great Polar Current.

      Soon more numerous flocks of birds, petrels, puffins, and others which inhabit those barren shores, gave token of their approach to Greenland. The Forward was moving rapidly northward, leaving behind her a long line of dark smoke.

      Tuesday, the 17th of April, the ice-master caught the first sight of the blink[2] of the ice. It was visible at least twenty miles off to the north-northwest. In spite of some tolerably thick clouds it lighted up brilliantly all the air near the horizon. No one of those on board who had ever seen this phenomenon before could fail to recognize it, and they felt assured from its whiteness that this blink was due to a vast field of ice lying about thirty miles farther than they could see, and that it came from the reflection of its luminous rays.

      Towards evening the wind shifted to the south, and became favorable; Shandon was able to carry sail, and as a measure of economy they extinguished the furnace fires. TheForward under her topsails, jib, and foresail, sailed on towards Cape Farewell.

      At three o'clock on the 18th they made out an ice-stream, which, like a narrow but brilliant band, divided the lines of the water and sky. It was evidently descending rather from the coast of Greenland than from Davis Strait, for the ice tended to keep on the western side of Baffin's Bay. An hour later, and the Forward was passing through the detached fragments of the ice-stream, and in the thickest part the pieces of ice, although closely welded together, were rising and falling with the waves.

      At daybreak the next morning the watch saw a sail; it was the Valkyria, a Danish corvette, sailing towards the Forward, bound to Newfoundland. The current from the strait became perceptible, and Shandon had to set more sail to overcome it.

      At that moment the commander, the doctor, James Wall, and Johnson were all together on the poop-deck, observing the force and direction of the current. The doctor asked if it were proved that this current was felt throughout Baffin's Bay.

      “There's no doubt of it,” answered Shandon; “and sailing-vessels have hard work in making headway against it.”

      “And it's so much the harder,” added James Wall, “because it's met on the eastern coast of America, as well as on the western coast of Greenland.”

      “Well,” said the doctor, “that serves to confirm those who seek a Northwest Passage. The current moves at the rate of about five miles an hour, and it is hard to imagine that it rises at the bottom of a gulf.”

      “That is very likely. Doctor,” answered Shandon, “because, while this current flows from north to south, there is a contrary current in Behring Strait, which flows from south to north, and which must be the cause of this one.”

      “Hence,” said the doctor, “you must admit that America is completely separated from the polar regions, and that the water from the Pacific skirts its whole northern coast, until it reaches the Atlantic. Besides, the greater elevation of the water of the Pacific is another reason for its flowing towards the European