The cantons which have suffered most terribly are those of Tessin, Grisons, and St. Gall11. The St. Gothard, Splugen, and St. Bernhardin routes have been rendered impassable. Twenty-seven lives were lost in the St. Gothard Pass, besides horses and waggons12 full of merchandise. It is stated that on the three routes upwards13 of eighty persons perished. In the village of Loderio alone, no less than fifty deaths occurred. So terrible a flood has not taken place since the year 1834. Nor have the cantons of Uri and Valais escaped. From Unterwalden we hear that the heavy rains which took place a fortnight ago have carried away several large bridges, and many of the rivers continue still very swollen14. I have already described how enormous the material losses are which have been caused by these floods. Many places are under water; others in ruins or absolutely destroyed. In Tessin alone the damage is estimated at forty thousand pounds sterling15.
A country like Switzerland must always be liable to the occurrence, from time to time, of catastrophes16 of135 this sort. Or rather, perhaps, we should draw a distinction between the two divisions of Switzerland referred to above. Of these the one may be termed the mountain half, and the other the lake half of the country. It is the former portion of the country which is principally subject to the dynamical action of water. A long-continued and heavy rainfall over the higher lands cannot fail to produce a variety of remarkable effects, where the arrangement of mountains and passes, hills, valleys, and ravines is so complicated. There are places where a large volume of water can accumulate until the barriers which have opposed its passage to the plains burst under its increasing weight; and then follow those destructive rushes of water which sweep away whole villages at once. It is, in fact, the capacity of the Swiss mountain region for damming up water, far more than any other circumstance, which renders the Swiss floods so destructive.
And then it must be remembered that there are at all times suspended over the plains and valleys which lie beneath the Alpine ranges enormous masses of water in the form of snow and ice. Although in general these suffer no changes but those due to the partial melting which takes place in summer, and the renewed accumulation which takes place in winter, yet when heavy rains fall upon the less elevated portions of the Alpine snow, they not only melt that snow much more rapidly than the summer sun would do, but they wash down large masses, which add largely to the destructive power of the descending17 waters.
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The most destructive floods which have occurred in Switzerland have usually been those which take place in early summer. The floods which inundated18 the plains of Martigny in 1818 were a remarkable instance of the effects which result from the natural damming up of large volumes of water in the upper parts of the Alpine hill-country. The whole of the valley of Bagnes, one of the largest of the lateral19 branches of the main valley of the Rhone above Geneva, was converted into a lake, in the spring of 1818, by the damming up of a narrow pass into which avalanches20 of snow and ice had been precipitated21 from a lofty glacier22 overhanging the bed of the river Dranse. The ice barrier enclosed a lake no less than half a league in length and an eighth of a mile wide, and in places two hundred feet deep. The inhabitants of the neighbouring villages were terrified by the danger which was to be apprehended23 from the bursting of the barrier. They cut a gallery seven hundred feet long through the ice, while the waters had as yet risen to but a moderate height; and when the waters began to flow through this channel, its course was deepened by the melting of the ice, and at length nearly half the contents of the lake were safely carried off. It was hoped that the process would continue, and the country be saved from the danger which had been so long impending24 over it. But as the heat of the weather increased, the central part of the barrier slowly melted away, until it became too weak to bear the enormous weight of water which was pressing against it. At length it gave way, so137 suddenly and completely that all the water which remained in the lake rushed out in half an hour. The downward passage of the water illustrated, in a very remarkable way, the fact that the chief mischief25 of floods is occasioned where water is checked in its outflow. For it is related that, ‘in the course of their descent the waters encountered several narrow gorges26, and at each of these they rose to a great height, and then burst with new violence into the next basin, sweeping27 along forests, houses, bridges, and cultivated land.’ Along the greater part of its course the flood resembled rather a moving mass of rock and mud than a stream of water. Enormous masses of granite28 were torn out of the sides of the valleys and whirled for hundreds of yards along the course of the flood. M. Escher relates that one of the fragments thus swept along was no less than sixty yards in circumference29. At first the water rushed onwards at a rate of more than a mile in three minutes, and the whole distance (forty-five miles) which separates the valley of Bagnes from the Lake of Geneva was traversed in little more than six hours. The bodies of persons who had been drowned in Martigny were found floating on the farther side of the lake of Geneva, near Vevey. Thousands of trees were torn up by the roots, and the ruins of buildings which had been overthrown30 by the flood were carried down beyond Martigny. In fact, the flood at this point was so high that some of the houses in Martigny were filled with mud up to the second storey138.‘ Beyond Martigny the flood did but little damage, as it here expanded over the plain, and was reduced both in depth and velocity31.
(From the Daily News for October 20, 1868.)
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1 remarkable | |
adj.显著的,异常的,非凡的,值得注意的 | |
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2 disturbance | |
n.动乱,骚动;打扰,干扰;(身心)失调 | |
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3 subterranean | |
adj.地下的,地表下的 | |
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4 disastrous | |
adj.灾难性的,造成灾害的;极坏的,很糟的 | |
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5 alpine | |
adj.高山的;n.高山植物 | |
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6 pointed | |
adj.尖的,直截了当的 | |
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7 ravaged | |
毁坏( ravage的过去式和过去分词 ); 蹂躏; 劫掠; 抢劫 | |
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8 illustrated | |
adj. 有插图的,列举的 动词illustrate的过去式和过去分词 | |
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9 philosophical | |
adj.哲学家的,哲学上的,达观的 | |
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10 drawn | |
v.拖,拉,拔出;adj.憔悴的,紧张的 | |
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11 gall | |
v.使烦恼,使焦躁,难堪;n.磨难 | |
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12 waggons | |
四轮的运货马车( waggon的名词复数 ); 铁路货车; 小手推车 | |
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13 upwards | |
adv.向上,在更高处...以上 | |
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14 swollen | |
adj.肿大的,水涨的;v.使变大,肿胀 | |
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15 sterling | |
adj.英币的(纯粹的,货真价实的);n.英国货币(英镑) | |
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16 catastrophes | |
n.灾祸( catastrophe的名词复数 );灾难;不幸事件;困难 | |
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17 descending | |
n. 下行 adj. 下降的 | |
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18 inundated | |
v.淹没( inundate的过去式和过去分词 );(洪水般地)涌来;充满;给予或交予(太多事物)使难以应付 | |
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19 lateral | |
adj.侧面的,旁边的 | |
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20 avalanches | |
n.雪崩( avalanche的名词复数 ) | |
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21 precipitated | |
v.(突如其来地)使发生( precipitate的过去式和过去分词 );促成;猛然摔下;使沉淀 | |
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22 glacier | |
n.冰川,冰河 | |
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23 apprehended | |
逮捕,拘押( apprehend的过去式和过去分词 ); 理解 | |
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24 impending | |
a.imminent, about to come or happen | |
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25 mischief | |
n.损害,伤害,危害;恶作剧,捣蛋,胡闹 | |
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26 gorges | |
n.山峡,峡谷( gorge的名词复数 );咽喉v.(用食物把自己)塞饱,填饱( gorge的第三人称单数 );作呕 | |
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27 sweeping | |
adj.范围广大的,一扫无遗的 | |
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28 granite | |
adj.花岗岩,花岗石 | |
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29 circumference | |
n.圆周,周长,圆周线 | |
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30 overthrown | |
adj. 打翻的,推倒的,倾覆的 动词overthrow的过去分词 | |
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31 velocity | |
n.速度,速率 | |
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