sooner or later spin down the snow which fills the trough; and, as their course and pace are more clearly apparent when falling over snow than when jumping from ledge to ledge, persons with lively imaginations are readily impressed by them. The grooves which are usually seen wandering down the length of snow couloirs are deepened (and, perhaps, occasionally originated) by falling stones, and they are sometimes pointed out by cautious men as reasons why couloirs should not be followed. I think they are very frequently only gutters, caused by water trickling off the rocks. Whether this is so or not, one should always consider the possibility of being struck by falling stones, and, in order to lessen the risk as far as possible, should mount upon the sides of the snow, and not up its centre. Stones that come off the rocks then fly over one's head, or bound down the middle of the trough at a safe distance.
At 9.30 a.m. we commenced the ascent of the couloir leading from the nameless glacier to a point in the ridge, just to the east of Mont Bans.[1] So far the route had been nothing more than a steep grind in an angle where little could be seen, but now views opened out in several directions, and the way began to be interesting. It was more so, perhaps, to us than to our companion M. Reynaud, who had no rest in the last night. He was, moreover, heavily laden. Science was to be regarded—his pockets were stuffed with books; heights and angles were to be observed—his knapsack was filled with instruments; hunger was to be guarded against—his shoulders were ornamented with a huge nimbus of bread, and a leg of mutton swung behind from his knapsack, looking like an overgrown tail. Like a good-hearted fellow, he had brought this food, thinking we might be in need of it. As it happened, we were well provided for, and having our own packs to carry, could not relieve him of his superfluous burdens, which, naturally, he did not like to throw away. As the angles steepened,
- ↑ The upper part of the southern side of the Col de Pilatte, and the small glaciers spoken of on p. 224, can be seen from the high road leading from Briançon to Mont Dauphin, between the 12th and 13th kilomètre stones (from Briançon).
