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on of details, which influences like these, acting on an enormous scale, must inevitably produce in all mountain groups; because each individual part and promontory, being compelled to assume the same symmetrical curves as its neighbors, and to descend at precisely the same slope to the valley, falls in with their prevailing lines, and becomes a part of a great and harmonious whole, instead of an unconnected and discordant individual. It is true that each of these members has its own touches of specific character, its own projecting crags and peculiar hollows; but by far the greater portion of its lines will be such as unite with, though they do not repeat, those of its neighbors, and carry out the evidence of one great influence and spirit to the limits of the scene. This effort is farther aided by the original unity and connection of the rocks themselves, which though it often may be violently interrupted, is never without evidence of existence; for the very interruption itself forces the eye to feel that there is something to be interrupted, a sympathy and similarity of lines and fractures, which, however full of variety and change of direction, never lose the appearance of symmetry of one kind or another. But, on the other hand, it is to be remembered that these great sympathizing masses are not one mountain, but a thousand mountains; that they are originally composed of a multitude of separate eminences, hewn and chiselled indeed into associating form, but each retaining still its marked points and features of character,--that each of these individual members has, by the very process which assimilated it to the rest, been divided and subdivided into equally multitudinous groups of minor mountains; finally, that the whole complicated system is interrupted forever and ever by daring manifestations of the inward mountain will--by the precipice which has submitted to no modulation of the torrent, and the peak which has bowed itself to no terror of the storm. Hence we see that the same imperative laws which require perfect simplicity of mass, require infinite and termless complication of detail,--that there will not be an inch nor a hairbreadth of the gigantic heap which has not its touch of separate character, its own peculiar curve, stealing out for an instant and then melting into the common line; felt for a moment by the blue mist of the hollow beyond, then lost when it crosses the enlightened slope,--that all this m
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