While I gave them their time, I looked around, and here a lesson came home to me. In the hollow where we stood, the snow did not lie smoothly. A huge obstacle to the northwest, probably a buried clump of brush, had made the wind turn back upon itself, first downward, then, at the bottom of the pit, in a direction opposite to that of the main current above, and finally slantways upward again to the summit of the obstacle, where it rejoined the parent blow. The floor of the hollow was cleanly scooped out and chiselled in low ridges; and these ridges came from the southeast, running their points to the northwest. I learned to look out for this sign, and I verily believe that, had I not learned that lesson right now, I should never have reached the creek which was still four or five miles distant.
The huge mound in the lee of which I was stopping was a matter of two hundred yards away; nearer to it the snow was considerably deeper; and since it presented an appearance very characteristic of Prairie bush-drifts, I shall describe it in some detail. Apparently the winds had first bent over all the stems of the clump; for whenever I saw one of them from the north, it showed a smooth, clean upward sweep. On the south side the snow first fell in a sheer cliff; then there was a hollow which was partly filled by a talus-shaped drift thrown in by the counter currents from the southern pit in which we were stopping; the sides of this talus again showed the marks that reminded of those left by the spoon when butter is roughly stroked into the shape of a pyramid. The interesting parts of the structure consisted in the beetling brow of the cliff and the roof of the cavity underneath. The brow had a honeycombed appearance; the snow had been laid down in layers of varying density (I shall discuss this more fully in the next chapter when we are going to look in on the snow while it is actually at work); and the counter currents that here swept upward in a slanting direction had bitten out the softer layers, leaving a fine network of little ridges which reminded strangely of the delicate fretwork-tracery in wind-sculptured rock—as I had seen it in the Black Hills in South Dakota. This piece of work of the wind is exceedingly short-lived in snow, and it must not be confounded with the honeycombed appearance of those faces of snow cliffs which are “rotting” by reason of their exposure to the heat of the noonday sun. These latter are coarse, often dirty, and nearly always have something bristling about them which is entirely absent in the sculptures of the wind. The under side of the roof in the cavity looked very much as a very stiff or viscid treacle would look when spread over a meshy surface, as, for instance, over a closely woven netting of wire. The stems and the branches of the brush took the place of the wire, and in their meshes the snow had been pressed through by its own weight, but held together by its curious ductility or tensile strength of which I was to find further evidence soon enough. It thus formed innumerable, blunted little stalactites, but without the corresponding stalagmites which you find in limestone caves or on the north side of buildings when the snow from the roof thaws and forms icicles and slender cones of ice growing up to meet them from the ground where the trickling drops fall and freeze again.
By the help of these various tokens I had picked my next resting place before we started up again. It was on this second dash that I understood why those Homeric words had come to my lips a while ago. This was indeed like nothing so much as like being out on rough waters and in a troubled sea, with nothing to brace the storm with but a wind-tossed nutshell of a one-man sailing craft. I knew that experience for having outridden many a gale in the mouth of the mighty St. Lawrence River. When the snow reached its extreme in depth, it gave you the feeling which a drowning man may have when fighting his desperate fight with the salty waves. But more impressive than that was the frequent outer resemblance. The waves of the ocean rise up and reach out and batter against the rocks and battlements of the shore, retreating again and ever returning to the assault, covering the obstacles thrown in the way of their progress with thin sheets of licking tongues at least. And if such a high crest wave had suddenly been frozen into solidity, its outline would have mimicked to perfection many a one of the snow shapes that I saw around.
Once the horses had really learned to pull exactly together—and they learned it thoroughly here—our progress was not too bad. Of course, it was not like going on a grade, be it ever so badly drifted in. Here the ground underneath, too, was uneven and overgrown with a veritable entanglement of brush in which often the horses’ feet would get caught. As for the road, there was none left, nothing that even by the boldest stretch of imagination could have been considered even as the slightest indication of one. And worst of all, I knew positively that there would be no trail at any time during the winter. I was well aware of the fact that, after it once snowed up, nobody ever crossed this waste between the “half way farms” and the “White Range Line House.” This morning it took me two and a half solid hours to make four miles.
But the ordeal had its reward. Here where the fact that there was snow on the ground, and plenty of it, did no longer need to be sunk into my brain—as soon as it had lost its value as a piece of news and a lesson, I began to enjoy it just as the hunter in India will enjoy the battle of wits when he is pitted against a yellow-black tiger. I began to catch on to the ways of this snow; I began, as it were, to study the mentality of my enemy. Though I never kill, I am after all something of a sportsman. And still another thing gave me back that mental equilibrium which you need in order to see things and to reason calmly about them. Every dash of two hundred yards or so brought me that much nearer to my goal. Up to the “half way farms” I had, as it were, been working uphill: there was more ahead than behind. This was now reversed: there was more behind than ahead, and as yet I did not worry about the return trip.
Now I have already said that snow is the only really plastic element in which the wind can carve the vagaries of its mood and leave a record of at least some permanency. The surface of the sea is a wonderful book to be read with a lightning-quick eye; I do not know anything better to do as a cure for ragged nerves—provided you are a good sailor. But the forms are too fleeting, they change too quickly—so quickly, indeed, that I have never succeeded in so fixing their record upon my memory as to be able to develop one form from the other 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 wide back of a large fish diving down into the concave side towards the trough. This looked very much like porpoises or dolphins jumping in a heaving sea; only that in my memory picture the real dolphins always jump in the opposite direction, against the run of the waves, bridging the trough.
In other places a fine, exceedingly delicate crest-line would spring up from the high point of some buried obstacle and sweep along in the most graceful curve as far as the eye would carry I particularly remember one of them, and I could discover no earthly reason for the curvature in it.
Again there would be a triangular—or should I say “tetrahedral”?—up-sweep from the direction of the wind, ending in a sharp, perfectly plane down-sweep on the south side; and the point of this three-sided but oblique pyramid would hang over like the flap of a tam. There was something of the consistency of very thick cloth about this overhanging flap.
Or an up-slope from the north would end in a long, nearly perpendicular cliff-line facing south. And the talus formation which I have mentioned would be perfectly smooth; but it did not reach quite to the top of the cliff, maybe to within a foot of it. The upsloping layer from the north would hang out again, with an even brow; but between this smooth cornice and the upper edge of the talus the snow looked as if it had been squeezed out by tremendous pressure from above, like an exceedingly viscid liquid—cooling glue, for instance, which is being squeezed out from between the core and the veneer in a veneering press.