Post 03814
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With advance it grew steadily deeper from constantly acquired material and from the influence of converging water-channels which it followed. A quarter of a mile from its birthplace it was about fifty feet deep and twice as wide, with a length of three hundred feet. Composed of new snow and coasting as swiftly as a gale, it trailed a white streamer of snow-dust behind. A steeper or a rougher channel added to the volume of snow-dust or increased the agitation of the pace-keeping pennant. The morning was clear, and, by watching the wigwagging snow flag, I followed easily the fortunes of the slide to the bottom of the slope. After a swift mile of shooting and plunging, the slide, greatly compressed, sprawled and spread out over a level glacier meadow, where its last remnant lingered for the warmth of July.
Dismissing this slide, I watched along the range to the north and south, and from time to time saw the white scudding plumes of other slides, which, hidden in the cañons, were merrily coasting down from the steep-sloping crest.
These slides, unless they had run down an animal, did no damage. They were composed of freshly fallen snow and in their flight had moved in old channels that had been followed and perhaps formed by hundreds of slides in years gone by. Slides of this kind–those which accompany or follow each storm and which promptly make away with new-fallen snow by carrying it down through stream-channels–may be called Storm, or Flood, slides. These usually are formed in smooth gulches or on steep slopes.