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in descriptive notes. It is that very fact, I believe, upon which hinges the curative value of the sight: you are so completely absorbed by the moment, and all other things fall away. Many and many a day have I lain in my deck chair on board a liner and watched the play of the waves; but the pleasure, which was very great indeed, was momentary; and sometimes, when in an unsympathetic mood, I have since impatiently wondered in what that fascination may have consisted. It was different here. Snow is very nearly as yielding as water and, once it fully responds in its surface to the carving forces of the wind, it stays--as if frozen into the glittering marble image of its motion. I know few things that are as truly fascinating as the sculptures of the wind in snow; for here you have time and opportunity a-plenty to probe not only into the what, but also into the why. Maybe that one day I shall write down a fuller account of my observations. In this report I shall have to restrict myself to a few indications, for this is not the record of the whims of the wind, but merely the narrative of my drives. In places, for instance, the rounded, "bomb-proof" aspect of the expanses would be changed into the distinct contour of gigantic waves with a very fine, very sharp crest-line. The upsweep from the northwest would be ever so slightly convex, and the downward sweep into the trough was always very distinctly concave. This was not the ripple which we find in beach sand. That ripple was there, too, and in places it covered the wide backs of these huge waves all over; but never was it found on the concave side. Occasionally, but rarely, one of these great waves would resemble a large breaker with a curly crest. Here the onward sweep from the northwest had built the snow out, beyond the supporting base, into a thick overhanging ledge which here and there had sagged; but by virtue of that tensile strength and cohesion in snow which I have mentioned already, it still held together and now looked convoluted and ruffled in the most deceiving way. I believe I actually listened for the muffled roar which the breaker makes when its subaqueous part begins to sweep the upward sloping beach. To make this illusion complete, or to break it by the very absurdity and exaggeration of a comparison drawn out too far--I do not know which--there would, every now and then, from the crest of one of these waves, jut out something which closely resembled the
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