Now, what becomes of these vast quantities of detritus12 furnished to the sea? That depends on the shore currents at the particular locality. If there is not much of a current, the larger grains of grit13 and sand are soon separated from the rest, and fall to the bottom, whilst the clays are taken farther out to sea before being laid down. But, in any case, the reader will readily perceive that marine deposits must of necessity be on a grander scale, and of a much more substantial character, as a rule, than river, lacustrine, or estuarine14 deposits. By their mode of origin, too, they must be more homogeneous, whilst they are frequently several hundreds of feet in thickness. In their process of deposition15 they were not influenced by every storm and freshet; nothing short of great earth-movements in process of time, or some other equally grand phenomena16, could disturb the even tenour of their existence. How different to the comparatively insignificant17 strata18 formed by the other methods alluded19 to!
Take samples of brick-earth of fluviatile origin at intervals and analyse them; no two analyses will be alike, except by a most remarkable20 coincidence—more by accident than otherwise. On the other hand, take a thick marine clay, and compare its chemical composition as ascertained21 at the present time with that of it made, say, 20 years ago in the same brickyard, and the analyses will, in most instances, be practically identical—at any rate, so far as they may be of use to the brickmaker.
24 A brickmaker using a marine clay possesses innumerable advantages over another employing brick-earths due to river action. It is no uncommon22 thing for a marine clay—say, 300 feet in thickness—to continue across country for hundreds of miles, stretching from the North of England to the South, and over into the Continent, save for the slight break occasioned by the scooping23 out of the English Channel. The composition of the Oxford24 Clay, from which the well-known bricks at Peterborough are made, does not differ in the slightest degree, so far as suitability for brickmaking is concerned, from the Oxford Clay of Bourges or Chateauroux, in the centre of France, or indeed at almost any other point en route. With marine beds it is possible to deal with the matter on broad lines, but it is not so with any other class of deposits.
If a marine clay in a specified25 locality is found to be unsuitable for bricks at one point, by reason of the presence of too much lime, it would be a phenomenon if clay along the same geological horizon did not present the same unfavourable features at every other point within the district. The homogeneous composition, both from mineralogical and chemical standpoints, of thick marine clays renders them of special use to the brickmaker. Having by sundry26 processes, after infinite labour, produced a certain class of brick from such an earth, he does not as a rule have to materially modify those processes as the earth is dug into to continue manufacturing the same brick. He is dealing27 with an earth which, comparatively speaking, is a constant quantity—when the clays are thick, and no lines of bedding are distinctly visible.
We find that a rooted conviction exists in many brickyards that clays of marine origin are no good for brickmaking, because (so the opinion runs) they always25 contain so much salt. It is wonderful that such ignorance prevails, when the slightest acquaintance with the subject would teach otherwise. It is perfectly28 true that such deposits might have contained salt during and for some time after deposition, but it is absurd to suppose that their marine origin has anything to do with the presence of common salt in the clay at the present time. Salt is soluble29 in water, and has been removed from such clays by the percolation30 of underground water in 99 cases out of a hundred. Indeed, as a matter of experience, we find that salt is most commonly found in beds of lacustrine origin, or those laid down in enclosed portions of the sea, for reasons we need not enter into at the present moment. Of course, when material is taken from the sea-shore to make into bricks, a considerable quantity of salt is manifest, but that is a totally different thing to the clays deposited—we should not like to say how many thousands of years ago. Clays of all kinds, however, may be impregnated with salt (as in parts of Cheshire), owing to the proximity31 of other beds containing that mineral; also by the percolation of underground water with much salt in solution.
To give some idea of the antiquity32 of the Oxford Clay alluded to—and that is quite a “young clay” geologically speaking—we may remark that at the time it was laid down not a single species of animal existed like those now living. The only mammals found, very small and very lowly organised, were like kangaroo rats; the birds were more like flying reptiles34 than anything else; it was the age of reptiles, and enormous, unwieldy brutes35 swam in the water or floundered about on land; huge sharks abounded36, and armour-clad fish of kinds very different to those now existing roamed the sea; even26 the “shell-fish” were not altogether like modern ones; whilst the plants find their nearest modern analogues37 in the wilds of Australasia. No elephants, tigers, lions, bears, or dogs lived then, and the face of Nature wore a totally different aspect to what obtains at the present time in any part of the globe.
And this seems a fitting opportunity to the writer to put on record the fact that many of the most wonderful remains38 found in the Oxford Clay and the neighbouring Kimeridge Clay are due to the discoveries of brickmakers. Without their valuable aid scientists would be quite unable to clearly depict39 the life of those remote epochs. We have mentioned Peterborough; some most interesting remains have been found in the clays near that town during the past few years. To appreciate this let the reader visit the fossil reptile33 gallery of the British Museum (Natural History), at South Kensington. One of the most recent acquisitions, set up a year or two ago, is the skeleton of a young Plesiosaurus—without doubt the most perfect specimen41 in the world of its kind—from Peterborough. The Plesiosaurus was a large swimming reptile, with paddles, and a long neck.
We mention these things not only to instil42 philosophical43 interest in such brick-earths, which may be reflected upon after business hours, but to impart some idea of the extreme remoteness of the epoch40 from the human point of view, and to insist on the immensity of the intervening time throughout which circulating underground waters—even in such an impervious44 material as stiff clay—may have exerted chemical action. The “mineralisation” of the fossils is an eloquent45 witness of the effect of such changes. The reader will perceive from this that there is scant46 possibility of soluble salts27 being present in such marine clays; and the geological circumstances are fully47 borne out by the results of hundreds of chemical analyses of thick marine clays.
The invertebrate48 fossils more particularly testify to the marine origin of the clays, and are thus invested with considerable practical interest. The man whose duty it is to determine the persistence49, or otherwise, of valuable marine brick-earths has thus a much easier task than when called upon to decide the value of a large tract50 of land for brickmaking purposes, of fluviatile origin. Finally, brick-earths do not, except in extremely rare instances, vary materially in character when dug into horizontally, thus every opportunity is afforded to the manufacturer for making an unvariable quality brick, tile, or drain pipe. It should be borne in mind, however, that these clays often weather a brown colour, which on being dug into changes to a bluish-black tint51, the latter being the unaltered and best portion as a rule. The only practical advantage the worker of a superficial river deposit possesses over his neighbour using thick marine clay is in the great range of variation in materials disclosed in the former kind of pit. By judiciously52 mixing the different beds he may be able to live well where the worker of marine clays, especially where the clay is too stiff, or contains too much lime, “comes to grief.” A good marine clay is a great boon53, a bad one cannot be remedied other than by the sacrifice of much money.
点击收听单词发音
1 marine | |
adj.海的;海生的;航海的;海事的;n.水兵 | |
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2 attentively | |
adv.聚精会神地;周到地;谛;凝神 | |
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3 friable | |
adj.易碎的 | |
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4 intervals | |
n.[军事]间隔( interval的名词复数 );间隔时间;[数学]区间;(戏剧、电影或音乐会的)幕间休息 | |
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5 denudation | |
n.剥下;裸露;滥伐;剥蚀 | |
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6 succumb | |
v.屈服,屈从;死 | |
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7 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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8 gravel | |
n.砂跞;砂砾层;结石 | |
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9 projections | |
预测( projection的名词复数 ); 投影; 投掷; 突起物 | |
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10 incessant | |
adj.不停的,连续的 | |
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11 limestone | |
n.石灰石 | |
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12 detritus | |
n.碎石 | |
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13 grit | |
n.沙粒,决心,勇气;v.下定决心,咬紧牙关 | |
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14 estuarine | |
河口的,江口的 | |
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15 deposition | |
n.免职,罢官;作证;沉淀;沉淀物 | |
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16 phenomena | |
n.现象 | |
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17 insignificant | |
adj.无关紧要的,可忽略的,无意义的 | |
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18 strata | |
n.地层(复数);社会阶层 | |
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19 alluded | |
提及,暗指( allude的过去式和过去分词 ) | |
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20 remarkable | |
adj.显著的,异常的,非凡的,值得注意的 | |
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21 ascertained | |
v.弄清,确定,查明( ascertain的过去式和过去分词 ) | |
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22 uncommon | |
adj.罕见的,非凡的,不平常的 | |
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23 scooping | |
n.捞球v.抢先报道( scoop的现在分词 );(敏捷地)抱起;抢先获得;用铲[勺]等挖(洞等) | |
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24 Oxford | |
n.牛津(英国城市) | |
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25 specified | |
adj.特定的 | |
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26 sundry | |
adj.各式各样的,种种的 | |
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27 dealing | |
n.经商方法,待人态度 | |
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28 perfectly | |
adv.完美地,无可非议地,彻底地 | |
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29 soluble | |
adj.可溶的;可以解决的 | |
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30 percolation | |
n.过滤,浸透;渗滤;渗漏 | |
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31 proximity | |
n.接近,邻近 | |
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32 antiquity | |
n.古老;高龄;古物,古迹 | |
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33 reptile | |
n.爬行动物;两栖动物 | |
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34 reptiles | |
n.爬行动物,爬虫( reptile的名词复数 ) | |
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35 brutes | |
兽( brute的名词复数 ); 畜生; 残酷无情的人; 兽性 | |
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36 abounded | |
v.大量存在,充满,富于( abound的过去式和过去分词 ) | |
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37 analogues | |
相似物( analogue的名词复数 ); 类似物; 类比; 同源词 | |
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38 remains | |
n.剩余物,残留物;遗体,遗迹 | |
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39 depict | |
vt.描画,描绘;描写,描述 | |
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40 epoch | |
n.(新)时代;历元 | |
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41 specimen | |
n.样本,标本 | |
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42 instil | |
v.逐渐灌输 | |
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43 philosophical | |
adj.哲学家的,哲学上的,达观的 | |
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44 impervious | |
adj.不能渗透的,不能穿过的,不易伤害的 | |
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45 eloquent | |
adj.雄辩的,口才流利的;明白显示出的 | |
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46 scant | |
adj.不充分的,不足的;v.减缩,限制,忽略 | |
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47 fully | |
adv.完全地,全部地,彻底地;充分地 | |
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48 invertebrate | |
n.无脊椎动物 | |
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49 persistence | |
n.坚持,持续,存留 | |
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50 tract | |
n.传单,小册子,大片(土地或森林) | |
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51 tint | |
n.淡色,浅色;染发剂;vt.着以淡淡的颜色 | |
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52 judiciously | |
adv.明断地,明智而审慎地 | |
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53 boon | |
n.恩赐,恩物,恩惠 | |
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