Page:Whymper - Scrambles amongst the Alps.djvu/431

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chap. xx.
VIEW FROM THE RUINETTE.
371

(14,164), with its noble background of the whole range of Mont Blanc, never looks so big as it does from here. In the contrary direction, the Matterhorn overpowers all besides. The Dent d'Herens, although closer, looks a mere outlier of its great neighbour, and the snows of Monte Rosa, behind, seem intended for no other purpose than to give relief to the crags in front. To the south there is an endless array of Bec's and Becca's, backed by the great Italian peaks, whilst to the north Mont Pleureur (12,159) holds its own against the more distant Wildstrubel.

We gained the summit at 9.15,[1] and stayed there an hour and a half. My faithful guides then admonished me that Prerayen, whither we were bound, was still far away, and that we had yet to cross two lofty ridges. So we resumed our harness and departed; not, however, before a huge cairn had been built out of the blocks of gneiss with which the summit is bestrewn. Then we trotted down the slopes of the Buinette, over the glacier de Breney, and across a pass which (if it deserves a name) may be called the Col des Portons, after the neighbouring peaks. From thence we proceeded across the great Otemma glacier towards the Col d'Olen.

The part of the glacier that we traversed was overspread with snow which completely concealed its numerous pitfalls. We marched across it in single file, and, of course, roped together. All at once Almer dropped into a crevasse up to his shoulders. I pulled in the rope immediately, but the snow gave way as it was being done, and I had to spread out my arms to stop my descent. Biener held fast, but said afterwards, that his feet went through as well, so, for a moment, all three were in the jaws of the crevasse. We now altered our course, so as to take the fissures transversely, and after the centre of the glacier was passed changed it again and made directly for the summit of the Col d'Olen.

  1. After crossing the glacier de Breney, we ascended by some débris, and then by some cliffy ground, to the glacier which surrounds the peak upon the south; bore to the left (that is to the west) and went up the edge of the glacier; and lastly took to the arete of the ridge which descends towards the south-west, and followed it to the summit (12,727).