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The universal geography : earth and its inhabitants

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CHAPTER VIII.<br />

THE BASIN OF THE WASH.<br />

(Bedfordshire, Cambhidgeshike, Huntingdonshire, Northamptonshire, Ri'Tl<strong>and</strong>, Lincolnshire.)<br />

General Features.<br />

HESE are the English Netherl<strong>and</strong>s, <strong>and</strong> one of the districts even<br />

bears the name of Holl<strong>and</strong>—<strong>and</strong> that with perfect justice. <strong>The</strong><br />

aspect of the two countries is precisely the same. As in Holl<strong>and</strong>,<br />

so in the district of the Fens, the country forms a perfect level,<br />

<strong>and</strong> a traveller sees trees, houses, windmills, <strong>and</strong> other elevated<br />

objects rise gradually above the horizon, like ships on the ocean. <strong>The</strong> country of<br />

the Fens occu|)ies an area of nearly 1,200 square miles, <strong>and</strong> it is intersected by<br />

innumerable artificial water channels—some of them broad like rivers, <strong>and</strong> capable<br />

of bearing large vessels, others mere drains, whose direction is indicated from afar<br />

by a fringe of reeds. <strong>The</strong> waters would flood nearly the whole of this region if<br />

artificial means were not employed to get rid of the excess. <strong>The</strong> coast, the rivers,<br />

<strong>and</strong> the canals are lined by embankments, which prevent the water from invading<br />

the adjoining fields <strong>and</strong> meadows. Trees are scarce ; only willows are reflected in<br />

the sluggish waters, <strong>and</strong> here <strong>and</strong> there clumps of verdure surround the isolated<br />

homesteads. <strong>The</strong> soil of English Holl<strong>and</strong> is also the same as that of the Nether-<br />

l<strong>and</strong>s. In a few localities clayey soil of exceeding fertility slightly rises above<br />

the surrounding plain, <strong>and</strong> here the most ancient villages of the country are<br />

found. As a rule, the soil consists of peat, which has gradually been trans-<br />

formed by cultivation. <strong>The</strong> district of the Fens lies, moreover, at a higher<br />

level than the greater part of veritable Holl<strong>and</strong>. It has been raised by warp-<br />

ing, <strong>and</strong> as there are no " polders " whose level is inferior to that of the sea,<br />

the danger from inundation is very much less. In 1613, however, several villages<br />

were overwhelmed by a flood, <strong>and</strong> an extensive tract of productive l<strong>and</strong> converted<br />

temporarily into a marsh, but since that time the sea has not again broken through<br />

the embankments which form <strong>its</strong> bounds. <strong>The</strong> rainfall is less considerable than in<br />

the Netherl<strong>and</strong>s,* <strong>and</strong> the floods of the small rivers which Intersect the lowl<strong>and</strong>s<br />

Average rainfall in the basin of the Wash<br />

Holl<strong>and</strong> .<br />

22 inches.<br />

27 „

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