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William & Dorothy Wordsworth Page 2
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I do not indeed know any tract of country in which, within so narrow a compass, may be found an equal variety in the influences of light and shadow upon the sublime or beautiful features of landscape; and it is owing to the combined circumstances to which the reader’s attention has been directed. From a point between Great Gavel and Scawfell, a shepherd would not require more than an hour to descend into any one of eight of the principal vales by which he would be surrounded; and all the others lie (with the exception of Hawswater) at but a small distance. Yet, though clustered together, every valley has its distinct and separate character: in some instances, as if they had been formed in studied contrast to each other, and in others with the united pleasing differences and resemblances of a sisterly rivalship. This concentration of interest gives to the country a decided superiority over the most attractive districts of Scotland and Wales, especially for the pedestrian traveller. In Scotland and Wales are found, undoubtedly, individual scenes, which, in their several kinds, cannot be excelled. But, in Scotland, particularly, what long tracts of desolate country intervene! so that the traveller, when he reaches a spot deservedly of great celebrity, would find it difficult to determine how much of his pleasure is owing to excellence inherent in the landscape itself; and how much to an instantaneous recovery from an oppression left upon his spirits by the barrenness and desolation through which he has passed.
But to proceed with our survey;—and, first, of the Mountains. Their forms are endlessly diversified, sweeping easily or boldly in simple majesty, abrupt and precipitous, or soft and elegant. In magnitude and grandeur they are individually inferior to the most celebrated of those in some other parts of this island; but, in the combinations which they make, towering above each other, or lifting themselves in ridges like the waves of a tumultuous sea, and in the beauty and variety of their surfaces and colours, they are surpassed by none.
The general surface of the mountains is turf, rendered rich and green by the moisture of the climate. Sometimes the turf, as in the neighbourhood of Newlands, is little broken, the whole covering being soft and downy pasturage. In other places rocks predominate; the soil is laid bare by torrents and burstings of water from the sides of the mountains in heavy rains; and not unfrequently their perpendicular sides are seamed by ravines (formed also by rains and torrents) which, meeting in angular points, entrench and scar the surface with numerous figures like the letters W. and Y.
In the ridge that divides Eskdale from Wasdale, granite is found; but the Mountains are for the most part composed of the stone by mineralogists termed schist, which, as you approach the plain country, gives place to limestone and free-stone; but schist being the substance of the mountains, the predominant color of their rockyparts is bluish, or hoary grey—the general tint of the lichens with which the bare stone is encrusted. With this blue or grey colour is frequently intermixed a red tinge, proceeding from the iron that interveins the stone, and impregnates the soil. The iron is the principle of decomposition in these rocks; and hence, when they become pulverized, the elementary particles crumbling down, overspread in many places the steep and almost precipitous sides of the mountains with an intermixture of colours, like the compound hues of a dove’s neck. When in the heat of advancing summer, the fresh green tint of the herbage has somewhat faded, it is again revived by the appearance of the fern profusely spread over the same ground: and, upon this plant, more than upon any thing else, do the changes which the seasons make in the colouring of the mountains depend. About the first week in October, the rich green, which prevailed through the whole summer, is usually passed away. The brilliant and various colours of the fern are then in harmony with the autumnal woods; bright yellow or lemon colour, at the base of the mountains, melting gradually, through orange, to a dark russet brown towards the summits, where the plant, being more exposed to the weather, is in a more advanced state of decay. Neither heath nor furze are generally found upon the sides of these mountains, though in many places they are adorned by those plants, so beautiful when in flower. We may add, that the mountains are of height sufficient to have the surface towards the summit softened by distance, and to imbibe the finest aerial hues. In common also with other mountains, their apparent forms and colours are perpetually changed by the clouds and vapours which float round them: the effect indeed of mist or haze, in a country of this character, is like that of magic. I have seen six or seven ridges rising above each other, all created in a moment by the vapours upon the side of a mountain, which, in its ordinary appearance, shewed not a projecting point to furnish even a hint for such an operation.
I will take this opportunity of observing, that they who have studied the appearances of nature feel that the superiority, in point of visual interest, of mountainous over other countries—is more strikingly displayed in winter than in summer. This, as must be obvious, is partly owing to the forms of the mountains, which, of course, are not affected by the seasons; but also, in no small degree, to the greater variety that exists in their winter than their summer colouring. This variety is such, and so harmoniously preserved, that it leaves little cause of regret when the splendour of autumn is passed away. The oak-coppices, upon the sides of the mountains, retain russet leaves; the birch stands conspicuous with its silver stem and puce-coloured twigs; the hollies, with green leaves and scarlet berries, have come forth to view from among the deciduous trees, whose summer foliage had concealed them: the ivy is now plentifully apparent upon the stems and boughs of the trees, and upon the steep rocks. In place of the deep summer-green of the herbage and fern, many rich colours play into each other over the surface of the mountains; turf (the tints of which are interchangeably tawny-green, olive, and brown,) beds of withered fern, and grey rocks, being harmoniously blended together. The mosses and lichens are never so fresh and flourishing as in winter, if it be not a season of frost; and their minute beauties prodigally adorn the foreground. Wherever we turn, we find these productions of nature, to which winter is rather favourable than unkindly, scattered over the walls, banks of earth, rocks, and stones, and upon the trunks of trees, with the intermixture of several species of small fern, now green and fresh; and, to the observing passenger, their forms and colours are a source of inexhaustable admiration. Add to this the hoar-frost and snow, with all the varieties they create, and which volumes would not be sufficient to describe. I will content myself with one instance of the colouring produced by snow, which may not be uninteresting to painters. It is extracted from the memorandum-book of a friend; and for its accuracy I can speak, having been an eye-witness of the appearance. “I observed,” says he, “the beautiful effect of the drifted snow upon the mountains, and the perfect tone of colour. From the top of the mountains downwards a rich olive was produced by the powdery snow and the grass, which olive was warmed with a little brown, and in this way harmoniously combined, by insensible gradations, with the white. The drifting took away the monotony of snow; and the whole vale of Grasmere, seen from the terrace walk in Easedale, was as varied, perhaps more so, than even in the pomp of autumn. In the distance was Loughrigg-Fell, the basin-wall of the lake: this, from the summit down- ward, was a rich orange-olive; then the lake of a bright olive-green, nearly the same tint as the snow-powdered mountain tops and high slopes in Easedale; and lastly, the church, with its firs, forming the centre of the view. Next to the church came nine distinguishable hills, six of them with woody sides turned towards us, all of them oak-copses with their bright red leaves and snow-powdered twigs; these hills—so variously situated in relation to each other, and to the view in general, so variously powdered, some only enough to give the herbage a rich brown tint, one intensely white and lighting up all the others—were yet so placed, as in the most inobtrusive manner to harmonise by contrast with a perfect naked, snowless bleak summit in the far distance.”
Having spoken of the forms, surface, and colour of the mountains, let us descend into the Vales. Though these have been represented under the general image of the spokes
of a wheel, they are, for the most part, winding; the windings of many being abrupt and intricate. And, it may be observed, that, in one circumstance, the general shape of them all has been determined by that primitive conformation through which so many became receptacles of lakes. For they are not formed, as are most of the celebrated Welsh vallies, by an approximation of the sloping bases of the opposite mountains towards each other, leaving little more between than a channel for the passage of a hasty river; but the bottom of these vallies is mostly a spacious and gently declining area, apparently level as the floor of a temple, or the surface of a lake, and broken in many cases, by rocks and hills, which rise up like islands from the plain. In such of the vallies as make many windings, these level areas open upon the traveller in succession, divided from each other sometimes by a mutual approximation of the hills, leaving only passage for a river, sometimes by correspondent windings, without such approximation; and sometimes by a bold advance, of one mountain towards that which is opposite it. It may here be observed with propriety that the several rocks and hills, which have been described as rising up like islands from the level area of the vale, have regulated the choice of the inhabitants in the situation of their dwellings. Where none of these are found, and the inclination of the ground is not sufficiently rapid easily to carry off the waters, (as in the higher part of Langdale, for instance,) the houses are not sprinkled over the middle of the vales, but confined to their sides, being placed merely so far up the mountain as to be protected from the floods. But where these rocks and hills have been scattered over the plain of the vale, (as in Grasmere, Donnerdale, Eskdale, &.) the beauty which they give to the scene is much heightened by a single cottage, or cluster of cottages, that will be almost always found under them, or upon their sides; dryness and shelter having tempted the Dalesmen to fix their habitations there.
I shall now speak of the Lakes of this country. The form of the lake is most perfect when, like Derwent-water, and some of the smaller lakes, it least resembles that of a river; —I mean, when being looked at from any given point where the whole may be seen at once, the width of it bears such proportion to the length, that, however the outline may be diversified by far-receding bays, it never assumes the shape of a river, and is contemplated with that placid and quiet feeling which belongs peculiarly to the lake—as a body of still water under the influence of no current; reflecting therefore the clouds, the light, and all the imagery of the sky and surrounding hills; expressing also and making visible the changes of the atmosphere, and motions of the lightest breeze, and subject to agitation only from the winds—
The visible scene
Would enter unawares into his mind
With all its solemn imagery, its rocks,
Its woods, and that uncertain heaven received
Into the bosom of the steady lake!
It must be noticed, as a favourable characteristic of the lakes of this country, that, though several of the largest, such as Winandermere, Ulswater, Haweswater, do, when the whole length of them is commanded from an elevated point, lose somewhat of the peculiar form of the lake, and assume the resemblance of a magnificent river; yet, as their shape is winding, (particularly that of Ulswater and Hawswater) when the view of the whole is obstructed by those barriers which determine the windings, and the spectator is confined to one reach, the appropriate feeling is revived; and one lake may thus in succession present to the eye the essential characteristic of many. But, though the forms of the large lakes have this advantage, it is never- theless favourable to the beauty of the country that the largest of them are comparatively small; and that the same vale generally furnishes a succession of lakes, instead of being filled with one. The vales in North Wales, as hath been observed, are not formed for the reception of lakes; those of Switzerland, Scotland, and this part of the North of England, are so formed; but, in Switzerland and Scotland, the proportion of diffused water is often too great, as at the lake of Geneva for instance, and in most of the Scotch lakes. No doubt it sounds magnificent and flatters the imagination, to hear at a distance of expanses of water so many leagues in length and miles in width; and such ample room may be delightful to the fresh-water sailor, scudding with a lively breeze amid the rapidly- shifting scenery. But, who ever travelled along the banks of Loch-Lomond, variegated as the lower part is by islands, without feeling that a speedier termination of the long vista of blank water would be acceptable; and without wishing for an interposition of green meadows, trees, and cottages, and a sparkling stream to run by his side? In fact, a notion, of grandeur, as connected with magnitude, has seduced persons of taste into a general mistake upon this subject. It is much more desirable, for the purposes of pleasure, that lakes should be numerous, and small or middlesized, than large, not only for communication by walks and rides, but for variety, and for recurrence of similar appearances. To illustrate this by one instance:—how pleasing is it to have a ready and frequent opportunity of watching, at the outlet of a lake, the stream pushing its way among the rocks in lively contrast with the stillness from which it has escaped; and how amusing to compare its noisy and turbulent motions with the gentle playfulness of the breezes, that may be starting up or wandering here and there over the faintly-rippled surface of the broad water! I may add, as a general remark, that, in lakes of great width, the shores cannot be distinctly seen at the same time, and therefore contribute little to mutual illustration and ornament; and, if the opposite shores are out of sight of each other, like those of the American and Asiatic lakes, then unfortunately the traveller is reminded of a nobler object; he has the blankness of a sea-prospect without the grandeur and accompanying sense of power.
As the comparatively small size of the lakes in the North of England is favourable to the production of variegated landscape, their boundary-line also is for the most part gracefully or boldly indented. That uniformity which prevails in the primitive frame of the lower grounds among all chains or clusters of mountains where large bodies of still water are bedded, is broken by the secondary agents of nature, ever at work to supply the deficiences of the mould in which things were originally cast. Using the word deficiences, I do not speak with reference to those stronger emotions which a region of mountains is peculiarly fitted to excite. The bases of those huge barriers may run for a long space in straight lines, and these parallel to each other; the opposite sides of a profound vale may ascend as exact counterparts, or in mutual reflection, like the billows of a troubled sea; and the impression be, from its very simplicity, more awful and sublime. Sublimity is the result of Nature’s first great dealings with the superficies of the earth; but the general tendency of her subsequent operations is towards the production of beauty; by a multiplicity of symmetrical parts uniting in a consistent whole. This is every where exemplified along the margins of these lakes. Masses of rock, that have been precipitated from the heights into the area of waters, lie in some places like stranded ships; or have acquired the compact structure of jutting piers; or project in little peninsulas crested with native wood. The smallest rivulet—one whose silent influx is scarcely noticeable in a season of dry weather—so faint is the dimple made by it on the surface of the smooth lake—will be found to have been not useless in shaping, by its deposits of gravel and soil in time of flood, a curve that would not otherwise have existed. But the more powerful brooks, encroaching upon the level of the lake, have, in course of time, given birth to ample promontories of sweeping outline that contrast boldly with the longitudinal base of the steeps on the opposite shore; while their flat or gently sloping surfaces never fail to introduce, into the midst of desolation and barrenness, the elements of fertility, even where the habitations of men may not have been raised. These alluvial promontories, however, threaten, in some places, to bisect the waters which they have long adorned; and, in course of ages, they will cause some of the lakes to dwindle into numerous and insignificant pools; which, in their turn, will finally be filled up. But, checking these intrusive calculations, let u
s rather be content with appearances as they are, and pursue in imagination the meandering shores, whether rugged steeps, admitting of no cultivation, descend into the water; or gently-sloping lawns and woods, or flat and fertile meadows stretch between the margin of the lake and the mountains. Among minuter recommendations will be noticed, especially along bays exposed to the setting-in of strong-winds, the curved rim of fine blue gravel, thrown up in course of time by the waves, half of it perhaps gleaming from under the water, and the corresponding half of a lighter hue; and in other parts bordering the lake, groves, if I may so call them, of reeds and bulrushes; or plots of water-lilies lifting up their large target-shaped leaves to the breeze, while the white flower is heaving upon the wave.