Was the expert opinion going to be verified? Would the ship, held by the grip of the pack, be slowly crushed into fragments directly she was caught in the line of movement? It was evidently not impossible, and precautions were taken so as to insure escape if she were to be caught and crushed. All the boats were taken out on to the ice and filled with provisions; the dogs were put in kennels also on the ice where they would be free to escape, and every one was constantly on the alert for the first sign of the "nip."
At last it came. They were all at meals when the increased uproar of the moving ice told them that the movement was nearing the vessel. Then, for the first time, they heard the ominous sounds of creaking timber. The Fram was being "nipped."
Every one hurried out of the cabin to see to the boats and the dogs and the stores. When they reached the open they found that, close upon her port side, the ice was heaving and piling up into a great massive wall, while all around the noise of the fracturing and cracking of huge blocks was deafening. Slowly the wall rose in the air higher than the vessel's deck, higher than the bulwarks, and then it began steadily to glide towards her. For the moment it seemed that nothing could save her, and that the stupendous weight of the gliding wall would soon grind her solid timbers into splinters, while part of it crashed over her decks and swept spars and everything away.
Silent the members of the crew stood on the ice on the starboard side watching and expecting every second to see the moving mass creep up to her and pulverise the bold little Fram, rendering them homeless and shipless. Some of the crushed ice, pushed forward in a huge roll like a frozen billow, was actually against her side and rising over the tent covering on the deck. The line of pressure had now reached exactly where she lay in the ice, and if she did not yield to it and slip from the grip that held her, she was doomed.
There was a sound of rending; a groaning crash; the Fram shivered till the breathless watchers thought they saw her spars tremble. Then, with a mighty wrench, she broke from the bonds that held her, and slowly rose from her nest in the ice, slipping upwards and away from the crushing force. A cheer burst from the lips of every one as she moved, for it meant not only the realisation of the hopes and ideals of those concerned in her construction and the complete vindication of their faith in her, but also the guarantee that the explorers were safely and securely housed, whatever might transpire.
When the movement in the ice had subsided, it was found that the Fram had slipped out of harm's way in a marvellous manner. So firmly had she been frozen in that the spot from whence she had been driven contained a complete mould of her shape, every seam and mark being reproduced in the ice. This proved that the test had not only been a severe one, but conclusive as well, since the vessel had really been frozen so solid into a mass of ice as to be a part of the mass. Her escape was an overwhelming disproof of the adverse theories expressed against her, and an entire victory for Nansen. There was now no question in any one's mind as to the result of the expedition; the Fram, having stood one test, would stand any, and nothing could stop her emerging in due course out on to the open sea again, having drifted very near to the Pole, if not quite up to it.
With a feeling of absolute security against further pressures and movements, the crew returned on board, and once more the cabin echoed to the light-hearted laughter which had been interrupted by the "nip." The hardy Norsemen who formed the party were as happy as they were brave, and throughout the years they were together there was nothing but good-humour and merriment among them. After the preliminary experience of how the Fram conducted herself during a "nip," little attention was paid to the ceaseless noise and roaring set up by the moving ice. Often she was forced up out of the line of movement, but the men in her cabin sat quiet; she was able to "sail herself" without any help on that ice-locked sea.
The existence of this constant movement of the ice formed a very important discovery in Arctic knowledge. A brief explanation of the causes and the effects may make this clear, and, at the same time, show how it is that such huge mountains of ice are formed in the depth of winter when the Polar Sea was currently supposed to be frozen into one great silent moveless ice-field.
As winter sets in within the Arctic Circle, the sea which flows between the northern coasts of Europe, Asia, and America becomes covered with ice to the shores, thus forming an enormous field of ice some two thousand miles across. This, lying on the surface of the water, often having a thickness of from thirty to fifty feet, checks, but cannot control the tides. The ebb, on one hand, leaves vast tracks of ice, previously afloat, straining on the ground, cracking so as to form enormous fissures and weakening the surface resistance. On the other hand, the flood tide is welling and pressing against the overlying barrier of ice and lifting it up until it cracks and opens, the pressure underneath lifting the separated masses on to their neighbours, which in turn resist with all their weight and grind back upon the masses beyond, until with the turn of the tide the forced-up masses gravitate down again, tumbling, crashing, bounding and rebounding one upon the other. Meanwhile the ice lowered by the ebb tide has formed a restricted crust against which the flood tide, backed up by the weight of the disturbed masses, uses its energy as a man uses his shoulder to lift a load. It is a battle between the resistance and the energy of nature, and usually energy wins along the line of the least resistance. Here, when once a point gives way, the accumulated energy concentrates. The "point" may be an area of ice a hundred miles square and fifty feet thick, and this tremendous mass, moved by the immeasurable force of the water pressure beneath it, grinds upon its surroundings and upon itself. Huge masses are pushed up on to the surface of the pack, crushing, grinding, and splintering as they go, their weight causing the under ice to bend and crack, and so add to the confusion of the struggle. Mass meets mass in a test of strength, and, failing to climb over one another, crush together, closer and higher, until there is a diminution of the pressure from below and they surge back, shattering themselves in the commotion and yet binding themselves into a single unit strong enough to resist the next onslaught of the tidal energy.
Along the shores, where the solid compactness of beetling cliffs holds back the sweep of the tide, the ice piles itself in mountainous ridges and chains. Those of greater bulk, taking the ground, offer a resistance against which the lesser masses can only strain and grind; but away out in the unfathomable depths of the Polar Sea there is no chance of the ice ever grounding. It is always floating, and so always susceptible to the force of wind, tide, and current. Consequently it is always moving and feeling the pressure of the water below, of the grinding strain of the drift, and of the surface disturbances brought about by the constant displacement.