Page:Curiosities of Olden Times.djvu/236

Curiosities of Olden Times and may be discovered at a distance, because they overtop the mountains that are not themselves glacier-clad. We found that it was much farther to the Jökull than we had imagined, and at length we reached a pile of rocks which, without forming steps and gradation at the point where we ascended, were of considerable height and very steep: these rocks extend to a great distance, and appear to surround the glacier, for we perceived their continuance as far as the eye could reach. Between this pile of rocks and the glacier there is a small plain, about a quarter of a mile in width, the soil of which is clay without pebbles and flakes of ice, because the waters which continually flow from the glacier carry them off. On ascending farther, we discovered, to the right, a lake situated at one of the angles of the glacier, the banks of which were formed of ice, and the bed received a portion of the waters that flowed from the mountains. The water was perfectly green, a colour it acquired by the rays of light that broke against the ice.

"After many turnings and windings we found a path by which we could descend with our horses into the valley. On arriving there we met with another embarrassment, as well in crossing a rivulet discharged from the lake, as in passing the muddy soil, in which our horses often sank up to the chest. 224