If the velocity of the river always remained the same, we should be presented with thick accumulations of the same character in sharply defined areas. But it is always changing. With every storm and every steady18 rain the motion of the river becomes greatly accelerated, with the result that the deposits for the time being are deposited farther out in the lake than in more quiescent11 periods. In this way we may have a gravel thrown down on sand, sand on clay, and so on.
From the foregoing observations it will be gleaned12 that, in general, deposits in large lakes are more persistent13 in character than are river deposits; indeed, in very large sheets of water, as Lake Superior, Lake Erie, &c., they are in this sense more comparable with sediment of marine14 origin.
The practical value of this knowledge hinges on the correct determination of the origin of the deposits, and it is not always easy to identify a brick-earth of lacustrine origin. In all probability the tyro15, on meeting one, would be disposed to regard it as a river deposit pure and simple. The valuation of a brick-earth property under such circumstances would thus be greatly in favour of the prospective16 purchaser; but it would be disastrous17 for the seller. A random18 section, except in the case of a very large lake, would show gravels19, sands and clays in much the same manner as the river deposits described in the last article of this series. But, as previously20 remarked, on the whole they would be more continuous and persistent, and what is quite as important, the mineral composition of each stratum21 would be equally homogeneous when traced over wide areas. The geologist22 distinguishes a lacustrine deposit from one of fluviatile origin more from its mineral constitution and the general disposition23 of the beds, as ascertained24 by mapping, than from evidence afforded by fossils—these latter for the most part being similar to those found in the deposits left by rivers.
The well-known brick-earth called “Reading mottled19 clay,” so extensively developed on the outskirts25 of the London basin, and in the Isle26 of Wight and Hampshire generally, furnishes a good example of a lacustrine deposit. Many millions of bricks are made from this bed every year, and in some parts of the districts mentioned the stratum is thick and extensively developed. It is pure enough to be suitable for terra-cotta manufacture here and there. No one who had seen this remarkable27 deposit could possibly fail to recognise it again. The natural colour of the clay when damp is brilliant red, scarlet28 or crimson29, in large blotches30 and patches mottled tea-green and yellow, and locally white.
We have been intensely amused to note the efforts in recent years to obtain possession of a few acres of this coveted31 deposit for brickmaking in divers32 localities. Not long since we visited a large brickmaking establishment where these Reading plastic clays are actively33 raised and used, the works being situated34 four miles from the nearest railway. There were no other brickworks between it and the railway line, and there was no water accommodation. Enquiry revealed the fact that the greater part of the intervening land belonged to the same landowner as the ground where the brickyard stands, and that no difficulty was apprehended35 of the owner letting out such intervening land for the same uses and on the same terms if other brickyards were contemplated36. The proprietor37 of the brickyard in question volunteered the information that the reason he started so far from the railway was because the earth at the point selected was the only kind suitable for brickmaking in the neighbourhood. We then questioned him as to his knowledge of the brick-earths in the district, and eventually elicited38 the fact that he chanced upon the spot selected, without any reasoning therefor,20 and commenced operations. As a matter of fact, precisely39 the same clay extended from his works all the way to the railway line, and had he known anything whatever of the geology of the district (even the merest boy’s knowledge of the subject), he would have seen how to save that four miles of road carriage. What prevented him from knowing the fact was a thin mantle40 of gravel and soil about four feet in thickness, which covered the plastic clay in the area generally, except in the immediate4 vicinity of his brickyard. That was in reference to a lacustrine deposit—the Reading plastic clay—and shows the value of knowing something of its persistent character; if it had been a river deposit there would not have been so much room for wonderment.
To give some idea of the extent of that particular horizon, we may say that not only is the plastic clay alluded to found so extensively in the London and Hampshire basins, it is even more expanded in the north-eastern parts of France, and is there as much utilised as on this side of the Channel for brickmaking.
Lacustrine deposits are sometimes of enormous value to the clayworker, on account of the general purity of the clays. This is more particularly the case when the material deposited is in part or wholly derived41 from chemical disintegration42 of granitic43 rocks, as in the celebrated44 Bovey Heathfield clays near Newton Abbot, so well described in a small pamphlet by Mr. S. Smith Harvey. Here an experimental boring proved the clays to a depth of 130 feet with no signs of exhaustion45. In the divers clay-pits but a small proportion of waste is found, the different levels vary in composition, and, like almost all thick clays, improve in quality as the depth increases. The strata46 are very irregular towards the surface, due perhaps to the action of local21 freshets in the final periods of the history of the lake. These clays are extensively employed for the manufacture of stoneware pipes, facing and other bricks, fire-bricks, etc. They constitute a somewhat remarkable exception to the class of clays laid down in lakes, as a rule, and, as will have been observed, are of enormous thickness.
We have very little to say in regard to estuarine47 brick-earths; as might readily be anticipated, they are intermediate in character between fluviatile and marine deposits, and approach the one or the other according to position in the estuary48. On the whole, they are variable in character, individual beds being thin. The strata frequently contain abundant plant remains49 (pieces of wood, etc.), and, except in the case of large rivers, are not noted50 for yielding very good brick-earths. Sometimes, however, the quality of the clays is not bad, as instance the bricks made in Lincolnshire and Northamptonshire from Jurassic Estuarine clays.
点击收听单词发音
1 sediment | |
n.沉淀,沉渣,沉积(物) | |
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2 deposition | |
n.免职,罢官;作证;沉淀;沉淀物 | |
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3 velocity | |
n.速度,速率 | |
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4 immediate | |
adj.立即的;直接的,最接近的;紧靠的 | |
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5 detritus | |
n.碎石 | |
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6 alluded | |
提及,暗指( allude的过去式和过去分词 ) | |
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7 subside | |
vi.平静,平息;下沉,塌陷,沉降 | |
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8 curbed | |
v.限制,克制,抑制( curb的过去式和过去分词 ) | |
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9 gravel | |
n.砂跞;砂砾层;结石 | |
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10 grit | |
n.沙粒,决心,勇气;v.下定决心,咬紧牙关 | |
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11 quiescent | |
adj.静止的,不活动的,寂静的 | |
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12 gleaned | |
v.一点点地收集(资料、事实)( glean的过去式和过去分词 );(收割后)拾穗 | |
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13 persistent | |
adj.坚持不懈的,执意的;持续的 | |
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14 marine | |
adj.海的;海生的;航海的;海事的;n.水兵 | |
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15 tyro | |
n.初学者;生手 | |
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16 prospective | |
adj.预期的,未来的,前瞻性的 | |
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17 disastrous | |
adj.灾难性的,造成灾害的;极坏的,很糟的 | |
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18 random | |
adj.随机的;任意的;n.偶然的(或随便的)行动 | |
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19 gravels | |
沙砾( gravel的名词复数 ); 砾石; 石子; 结石 | |
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20 previously | |
adv.以前,先前(地) | |
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21 stratum | |
n.地层,社会阶层 | |
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22 geologist | |
n.地质学家 | |
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23 disposition | |
n.性情,性格;意向,倾向;排列,部署 | |
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24 ascertained | |
v.弄清,确定,查明( ascertain的过去式和过去分词 ) | |
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25 outskirts | |
n.郊外,郊区 | |
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26 isle | |
n.小岛,岛 | |
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27 remarkable | |
adj.显著的,异常的,非凡的,值得注意的 | |
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28 scarlet | |
n.深红色,绯红色,红衣;adj.绯红色的 | |
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29 crimson | |
n./adj.深(绯)红色(的);vi.脸变绯红色 | |
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30 blotches | |
n.(皮肤上的)红斑,疹块( blotch的名词复数 );大滴 [大片](墨水或颜色的)污渍 | |
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31 coveted | |
adj.令人垂涎的;垂涎的,梦寐以求的v.贪求,觊觎(covet的过去分词);垂涎;贪图 | |
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32 divers | |
adj.不同的;种种的 | |
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33 actively | |
adv.积极地,勤奋地 | |
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34 situated | |
adj.坐落在...的,处于某种境地的 | |
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35 apprehended | |
逮捕,拘押( apprehend的过去式和过去分词 ); 理解 | |
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36 contemplated | |
adj. 预期的 动词contemplate的过去分词形式 | |
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37 proprietor | |
n.所有人;业主;经营者 | |
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38 elicited | |
引出,探出( elicit的过去式和过去分词 ) | |
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39 precisely | |
adv.恰好,正好,精确地,细致地 | |
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40 mantle | |
n.斗篷,覆罩之物,罩子;v.罩住,覆盖,脸红 | |
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41 derived | |
vi.起源;由来;衍生;导出v.得到( derive的过去式和过去分词 );(从…中)得到获得;源于;(从…中)提取 | |
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42 disintegration | |
n.分散,解体 | |
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43 granitic | |
花岗石的,由花岗岩形成的 | |
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44 celebrated | |
adj.有名的,声誉卓著的 | |
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45 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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46 strata | |
n.地层(复数);社会阶层 | |
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47 estuarine | |
河口的,江口的 | |
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48 estuary | |
n.河口,江口 | |
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49 remains | |
n.剩余物,残留物;遗体,遗迹 | |
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50 noted | |
adj.著名的,知名的 | |
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