Wordsworth's Guide 1810, edn 1835

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	page 19 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 contrasts 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 us 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 the lighter
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