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_Hope_ that night, when the hunting party returned, much sooner than had been expected, with the whip cracking, the men cheering, the dogs howling, and the sledge well laden with fresh meat. CHAPTER EIGHT. THE CAUSE OF ICE-BERGS--FOX-CHASE--A BEAR. One day, long after the walrus-hunt just described, Joe Davis stood on the deck of the _Hope_, leaning over the side and looking out to sea--at least in the direction of the sea, for, although mid-day, it was so dark that he could not see very far in any direction. Joe was conversing with Mr Dicey on the appearance of things around him. "Do you know, Mr Dicey," said he, "wot it is as causes them there ice-bergs?" Mr Dicey looked very grave and wise for a few seconds without answering. Then he said, in rather a solemn tone, "Well, Davis, to tell you the real truth, I _don't_ know!" Now, as this question is one of considerable interest, I shall endeavour to answer it for the benefit of the reader. The whole of the interior of Greenland is covered with ice and snow. This snowy covering does not resemble that soft snow which falls on our own hills. It is hard, and _never_ melts entirely away. The snow there is in some places a thousand feet thick! It covers all the hill-tops and fills up all the valleys, so that the country may be said to be a buried land. Since the world began, perhaps, snow has been falling on it every winter; but the summers there have been so short that they could not melt away the snow of one winter before that of another came and covered it up and pressed it down. Thus, for ages, the snow of one year has been added to that which was left of the preceding, and the pressure has been so great that the mass has been squeezed nearly as hard as pure ice. The ice that has been formed in this way is called _glacier_; and the glaciers of Greenland cover, as I have said, the whole country, so that it can never be cultivated or inhabited by man unless the climate change. There are glaciers of this kind in many other parts of the world. We have them in Switzerland and in Norway, but not on nearly so large a scale as in Greenland. Now, although this glacier-ice is clear and hard, it is not quite so solid as pure ice, and when it is pushed down into the valleys by the increasing masses above it, actually _flows_. But this flowing motion cannot be seen. It is like the motion of the hour hand of a watch, which cannot be perceived however
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