We walked in single file, headed by the hunter, who ascended3 by narrow tracks, where two could not have gone abreast4. There was therefore no room for conversation.
After we had passed the basaltic wall of the fiord of Stapi we passed over a vegetable fibrous peat bog5, left from the ancient vegetation of this peninsula. The vast quantity of this unworked fuel would be sufficient to warm the whole population of Iceland for a century; this vast turbary measured in certain ravines had in many places a depth of seventy feet, and presented layers of carbonized remains6 of vegetation alternating with thinner layers of tufaceous pumice.
As a true nephew of the Professor Liedenbrock, and in spite of my dismal7 prospects8, I could not help observing with interest the mineralogical curiosities which lay about me as in a vast museum, and I constructed for myself a complete geological account of Iceland.
This most curious island has evidently been projected from the bottom of the sea at a comparatively recent date. Possibly, it may still be subject to gradual elevation9. If this is the case, its origin may well be attributed to subterranean10 fires. Therefore, in this case, the theory of Sir Humphry Davy, Saknussemm's document, and my uncle's theories would all go off in smoke. This hypothesis led me to examine with more attention the appearance of the surface, and I soon arrived at a conclusion as to the nature of the forces which presided at its birth.
Iceland, which is entirely11 devoid12 of alluvial13 soil, is wholly composed of volcanic14 tufa, that is to say, an agglomeration15 of porous16 rocks and stones. Before the volcanoes broke out it consisted of trap rocks slowly upraised to the level of the sea by the action of central forces. The internal fires had not yet forced their way through.
But at a later period a wide chasm17 formed diagonally from south-west to north-east, through which was gradually forced out the trachyte which was to form a mountain chain. No violence accompanied this change; the matter thrown out was in vast quantities, and the liquid material oozing18 out from the abysses of the earth slowly spread in extensive plains or in hillocky masses. To this period belong the felspar, syenites, and porphyries.
But with the help of this outflow the thickness of the crust of the island increased materially, and therefore also its powers of resistance. It may easily be conceived what vast quantities of elastic19 gases, what masses of molten matter accumulated beneath its solid surface whilst no exit was practicable after the cooling of the trachytic crust. Therefore a time would come when the elastic and explosive forces of the imprisoned20 gases would upheave this ponderous21 cover and drive out for themselves openings through tall chimneys. Hence then the volcano would distend22 and lift up the crust, and then burst through a crater23 suddenly formed at the summit or thinnest part of the volcano.
To the eruption24 succeeded other volcanic phenomena25. Through the outlets26 now made first escaped the ejected basalt of which the plain we had just left presented such marvellous specimens27. We were moving over grey rocks of dense28 and massive formation, which in cooling had formed into hexagonal prisms. Everywhere around us we saw truncated29 cones30, formerly31 so many fiery32 mouths.
After the exhaustion33 of the basalt, the volcano, the power of which grew by the extinction34 of the lesser35 craters36, supplied an egress37 to lava38, ashes, and scoriae, of which I could see lengthened39 screes streaming down the sides of the mountain like flowing hair.
Such was the succession of phenomena which produced Iceland, all arising from the action of internal fire; and to suppose that the mass within did not still exist in a state of liquid incandescence40 was absurd; and nothing could surpass the absurdity41 of fancying that it was possible to reach the earth's centre.
So I felt a little comforted as we advanced to the assault of Snæfell.
The way was growing more and more arduous42, the ascent43 steeper and steeper; the loose fragments of rock trembled beneath us, and the utmost care was needed to avoid dangerous falls.
Hans went on as quietly as if he were on level ground; sometimes he disappeared altogether behind the huge blocks, then a shrill44 whistle would direct us on our way to him. Sometimes he would halt, pick up a few bits of stone, build them up into a recognisable form, and thus made landmarks45 to guide us in our way back. A very wise precaution in itself, but, as things turned out, quite useless.
Three hours' fatiguing46 march had only brought us to the base of the mountain. There Hans bid us come to a halt, and a hasty breakfast was served out. My uncle swallowed two mouthfuls at a time to get on faster. But, whether he liked it or not, this was a rest as well as a breakfast hour and he had to wait till it pleased our guide to move on, which came to pass in an hour. The three Icelanders, just as taciturn as their comrade the hunter, never spoke47, and ate their breakfasts in silence.
We were now beginning to scale the steep sides of Snæfell. Its snowy summit, by an optical illusion not unfrequent in mountains, seemed close to us, and yet how many weary hours it took to reach it! The stones, adhering by no soil or fibrous roots of vegetation, rolled away from under our feet, and rushed down the precipice48 below with the swiftness of an avalanche49.
At some places the flanks of the mountain formed an angle with the horizon of at least 36 degrees; it was impossible to climb them, and these stony50 cliffs had to be tacked51 round, not without great difficulty. Then we helped each other with our sticks.
I must admit that my uncle kept as close to me as he could; he never lost sight of me, and in many straits his arm furnished me with a powerful support. He himself seemed to possess an instinct for equilibrium52, for he never stumbled. The Icelanders, though burdened with our loads, climbed with the agility53 of mountaineers.
To judge by the distant appearance of the summit of Snæfell, it would have seemed too steep to ascend2 on our side. Fortunately, after an hour of fatigue54 and athletic55 exercises, in the midst of the vast surface of snow presented by the hollow between the two peaks, a kind of staircase appeared unexpectedly which greatly facilitated our ascent. It was formed by one of those torrents57 of stones flung up by the eruptions58, called 'sting' by the Icelanders. If this torrent56 had not been arrested in its fall by the formation of the sides of the mountain, it would have gone on to the sea and formed more islands.
Such as it was, it did us good service. The steepness increased, but these stone steps allowed us to rise with facility, and even with such rapidity that, having rested for a moment while my companions continued their ascent, I perceived them already reduced by distance to microscopic59 dimensions.
At seven we had ascended the two thousand steps of this grand staircase, and we had attained60 a bulge61 in the mountain, a kind of bed on which rested the cone proper of the crater.
Three thousand two hundred feet below us stretched the sea. We had passed the limit of perpetual snow, which, on account of the moisture of the climate, is at a greater elevation in Iceland than the high latitude62 would give reason to suppose. The cold was excessively keen. The wind was blowing violently. I was exhausted63. The Professor saw that my limbs were refusing to perform their office, and in spite of his impatience64 he decided65 on stopping. He therefore spoke to the hunter, who shook his head, saying:
"Ofvanför."
"It seems we must go higher," said my uncle.
Then he asked Hans for his reason.
"Mistour," replied the guide.
"Ja Mistour," said one of the Icelanders in a tone of alarm.
"What does that word mean?" I asked uneasily.
"Look!" said my uncle.
I looked down upon the plain. An immense column of pulverized66 pumice, sand and dust was rising with a whirling circular motion like a waterspout; the wind was lashing67 it on to that side of Snæfell where we were holding on; this dense veil, hung across the sun, threw a deep shadow over the mountain. If that huge revolving68 pillar sloped down, it would involve us in its whirling eddies69. This phenomenon, which is not unfrequent when the wind blows from the glaciers70, is called in Icelandic 'mistour.'
"Hastigt! hastigt!" cried our guide.
Without knowing Danish I understood at once that we must follow Hans at the top of our speed. He began to circle round the cone of the crater, but in a diagonal direction so as to facilitate our progress. Presently the dust storm fell upon the mountain, which quivered under the shock; the loose stones, caught with the irresistible71 blasts of wind, flew about in a perfect hail as in an eruption. Happily we were on the opposite side, and sheltered from all harm. But for the precaution of our guide, our mangled72 bodies, torn and pounded into fragments, would have been carried afar like the ruins hurled73 along by some unknown meteor.
Yet Hans did not think it prudent74 to spend the night upon the sides of the cone. We continued our zigzag75 climb. The fifteen hundred remaining feet took us five hours to clear; the circuitous76 route, the diagonal and the counter marches, must have measured at least three leagues. I could stand it no longer. I was yielding to the effects of hunger and cold. The rarefied air scarcely gave play to the action of my lungs.
At last, at eleven in the sunlight night, the summit of Snæfell was reached, and before going in for shelter into the crater I had time to observe the midnight sun, at his lowest point, gilding77 with his pale rays the island that slept at my feet.
点击收听单词发音
1 cone | |
n.圆锥体,圆锥形东西,球果 | |
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2 ascend | |
vi.渐渐上升,升高;vt.攀登,登上 | |
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3 ascended | |
v.上升,攀登( ascend的过去式和过去分词 ) | |
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4 abreast | |
adv.并排地;跟上(时代)的步伐,与…并进地 | |
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5 bog | |
n.沼泽;室...陷入泥淖 | |
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6 remains | |
n.剩余物,残留物;遗体,遗迹 | |
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7 dismal | |
adj.阴沉的,凄凉的,令人忧郁的,差劲的 | |
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8 prospects | |
n.希望,前途(恒为复数) | |
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9 elevation | |
n.高度;海拔;高地;上升;提高 | |
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10 subterranean | |
adj.地下的,地表下的 | |
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11 entirely | |
ad.全部地,完整地;完全地,彻底地 | |
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12 devoid | |
adj.全无的,缺乏的 | |
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13 alluvial | |
adj.冲积的;淤积的 | |
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14 volcanic | |
adj.火山的;象火山的;由火山引起的 | |
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15 agglomeration | |
n.结聚,一堆 | |
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16 porous | |
adj.可渗透的,多孔的 | |
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17 chasm | |
n.深坑,断层,裂口,大分岐,利害冲突 | |
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18 oozing | |
v.(浓液等)慢慢地冒出,渗出( ooze的现在分词 );使(液体)缓缓流出;(浓液)渗出,慢慢流出 | |
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19 elastic | |
n.橡皮圈,松紧带;adj.有弹性的;灵活的 | |
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20 imprisoned | |
下狱,监禁( imprison的过去式和过去分词 ) | |
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21 ponderous | |
adj.沉重的,笨重的,(文章)冗长的 | |
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22 distend | |
vt./vi.(使)扩大,(使)扩张 | |
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23 crater | |
n.火山口,弹坑 | |
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24 eruption | |
n.火山爆发;(战争等)爆发;(疾病等)发作 | |
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25 phenomena | |
n.现象 | |
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26 outlets | |
n.出口( outlet的名词复数 );经销店;插座;廉价经销店 | |
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27 specimens | |
n.样品( specimen的名词复数 );范例;(化验的)抽样;某种类型的人 | |
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28 dense | |
a.密集的,稠密的,浓密的;密度大的 | |
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29 truncated | |
adj.切去顶端的,缩短了的,被删节的v.截面的( truncate的过去式和过去分词 );截头的;缩短了的;截去顶端或末端 | |
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30 cones | |
n.(人眼)圆锥细胞;圆锥体( cone的名词复数 );球果;圆锥形东西;(盛冰淇淋的)锥形蛋卷筒 | |
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31 formerly | |
adv.从前,以前 | |
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32 fiery | |
adj.燃烧着的,火红的;暴躁的;激烈的 | |
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33 exhaustion | |
n.耗尽枯竭,疲惫,筋疲力尽,竭尽,详尽无遗的论述 | |
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34 extinction | |
n.熄灭,消亡,消灭,灭绝,绝种 | |
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35 lesser | |
adj.次要的,较小的;adv.较小地,较少地 | |
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36 craters | |
n.火山口( crater的名词复数 );弹坑等 | |
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37 egress | |
n.出去;出口 | |
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38 lava | |
n.熔岩,火山岩 | |
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39 lengthened | |
(时间或空间)延长,伸长( lengthen的过去式和过去分词 ) | |
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40 incandescence | |
n.白热,炽热;白炽 | |
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41 absurdity | |
n.荒谬,愚蠢;谬论 | |
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42 arduous | |
adj.艰苦的,费力的,陡峭的 | |
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43 ascent | |
n.(声望或地位)提高;上升,升高;登高 | |
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44 shrill | |
adj.尖声的;刺耳的;v尖叫 | |
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45 landmarks | |
n.陆标( landmark的名词复数 );目标;(标志重要阶段的)里程碑 ~ (in sth);有历史意义的建筑物(或遗址) | |
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46 fatiguing | |
a.使人劳累的 | |
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47 spoke | |
n.(车轮的)辐条;轮辐;破坏某人的计划;阻挠某人的行动 v.讲,谈(speak的过去式);说;演说;从某种观点来说 | |
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48 precipice | |
n.悬崖,危急的处境 | |
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49 avalanche | |
n.雪崩,大量涌来 | |
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50 stony | |
adj.石头的,多石头的,冷酷的,无情的 | |
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51 tacked | |
用平头钉钉( tack的过去式和过去分词 ); 附加,增补; 帆船抢风行驶,用粗线脚缝 | |
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52 equilibrium | |
n.平衡,均衡,相称,均势,平静 | |
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53 agility | |
n.敏捷,活泼 | |
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54 fatigue | |
n.疲劳,劳累 | |
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55 athletic | |
adj.擅长运动的,强健的;活跃的,体格健壮的 | |
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56 torrent | |
n.激流,洪流;爆发,(话语等的)连发 | |
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57 torrents | |
n.倾注;奔流( torrent的名词复数 );急流;爆发;连续不断 | |
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58 eruptions | |
n.喷发,爆发( eruption的名词复数 ) | |
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59 microscopic | |
adj.微小的,细微的,极小的,显微的 | |
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60 attained | |
(通常经过努力)实现( attain的过去式和过去分词 ); 达到; 获得; 达到(某年龄、水平、状况) | |
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61 bulge | |
n.突出,膨胀,激增;vt.突出,膨胀 | |
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62 latitude | |
n.纬度,行动或言论的自由(范围),(pl.)地区 | |
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63 exhausted | |
adj.极其疲惫的,精疲力尽的 | |
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64 impatience | |
n.不耐烦,急躁 | |
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65 decided | |
adj.决定了的,坚决的;明显的,明确的 | |
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66 pulverized | |
adj.[医]雾化的,粉末状的v.将…弄碎( pulverize的过去式和过去分词 );将…弄成粉末或尘埃;摧毁;粉碎 | |
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67 lashing | |
n.鞭打;痛斥;大量;许多v.鞭打( lash的现在分词 );煽动;紧系;怒斥 | |
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68 revolving | |
adj.旋转的,轮转式的;循环的v.(使)旋转( revolve的现在分词 );细想 | |
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69 eddies | |
(水、烟等的)漩涡,涡流( eddy的名词复数 ) | |
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70 glaciers | |
冰河,冰川( glacier的名词复数 ) | |
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71 irresistible | |
adj.非常诱人的,无法拒绝的,无法抗拒的 | |
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72 mangled | |
vt.乱砍(mangle的过去式与过去分词形式) | |
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73 hurled | |
v.猛投,用力掷( hurl的过去式和过去分词 );大声叫骂 | |
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74 prudent | |
adj.谨慎的,有远见的,精打细算的 | |
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75 zigzag | |
n.曲折,之字形;adj.曲折的,锯齿形的;adv.曲折地,成锯齿形地;vt.使曲折;vi.曲折前行 | |
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76 circuitous | |
adj.迂回的路的,迂曲的,绕行的 | |
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77 gilding | |
n.贴金箔,镀金 | |
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