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Bentarasko Benta Section 14
Page 10
Five bells were hung at regular intervals on a round hoop erected on a sort of stage. A rope was attached to each bell after the manner of church bells. At a given signal from their master, they all sprang to their feet, and at a second signal, each advanced to the ropes, and standing on their hind feet, stuck their front claws firmly into the ropes, which were in that part covered with worsted, or something of the kind, so as to give the claws a firmer hold. There was a moment's pause--then No. 1 pulled his or her rope, and so sounded the largest bell; No. 2 followed, then No. 3, and so on, till a regular peal was rung with almost as much precision and spirit as though it were human hands instead of cats' claws that effected it.
It is never right or useful to take revenge, for if you wait long enough you are always avenged by Providence. That afternoon my men saw some wild chestnuts on a tree, and they insisted on landing to pick them. They knocked down the tree, as usual, to get the chestnuts, although it was fully 3 ft. in diameter. They picked a great many of the wild chestnuts and proceeded to eat them--Alcides, much to my amazement, actually offering me one. I asked them if they knew what they were eating, as I quickly observed when the tree fell down that not a single chestnut had been touched by birds or monkeys.
Briefly, then, the geologist assures us that when the cold of the Glacial Age was at its maximum glaciers streamed down from all the mountains of Scotland, Wales, and Northern England; that the ice was thick enough to overtop all the smaller hills, and on the plains it united in one great sea of ice some thousands of feet in thickness, that it stretched as far south as the latitude of London, England. But that to the west the ice streamed out across, the Irish Sea, the islands to the west of Scotland, and ended far out into what is now the Atlantic.<23> But these glaciers, vast as they were, were very small compared with the glaciers that streamed out from the mountains of Norway and Sweden. These great glaciers invaded England to the southwest, beat back the glacier ice of Scotland from the floor of the North Sea, overran Denmark, and spread their mantle of bowlder clay far south into Germany.
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