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Curiosities of Olden Times sands. East of the glacier were two brown fells; that which was most to the south was not large, and it had a castellated appearance, whilst the other was oblong, stretching from north to south, and full of snowdrifts. From the same height they saw a great valley, long and narrow, running in a semicircle. At the end were heaps of shingle, precipices, and ravines. The valley began about the middle of the glacier, and ran north-east; then bent towards the east, and finally turned south. Towards the east the glacier became lower, and in the same proportion as the mountain ranges fell, did the valley become shallower; but it seemed nowhere to dive to the very bottom of the mountains. Towards the higher end of the valley, the glacier hemmed it in with steep sides. Where the valley was deepest, the mountain slopes were bare and weather-beaten, consisting of swarthy or brown terraces and hollows, having a colour like that of the fell close to the southern extremity of Geitland.

"In some places there were dry watercourses. It was so far to the bottom of the valley that the explorers could not discover exactly whether there was not grass on one of the slopes; but possibly the hue was the peculiar colour of the sandstone. Anyhow, they could not discover green pasturage. At the bottom of the valley were sandy flats, and in 232