By cutting steps in the snow they gained a considerable elevation, but, on looking round a point of rocks, the height beyond was so much greater and worse than they expected, that they could not proceed. All along shore was the crack of open water about a yard wide, with young ice beyond, through which a stone or fragment of ice might be thrown. Dense water-clouds appeared in many directions. They returned to camp, and, after enjoying some tea, Lockwood gave Jewell the tidal rod to make observations, while with Brainard he started out again, this time to the south and up a stream-bed, at whose mouth they were encamped, hoping to find a route back of the cliffs overland. They soon found themselves in a ravine with high, rocky sides, and encountered a steep snow-drift. Beyond was a small hole in the snow, which seemed to be a cavern or grotto formed of snow and ice, and probably running down to the bed of the stream—if that may be called a stream which has no water. Beyond this were exposed rocks under foot, and they saw ptarmigan-tracks, where the birds had used their wings in getting down a snow-drift. Finally, they came to a branch ravine from the southeast, the main stream leading off toward the south. They turned up the branch, and kept on for a while, when the high rocky sides seemed to come to a formation of ice like a glacier, a hundred feet high, at least, and very steep. The crest was perpendicular. The route thus far was difficult yet practicable, but it was clearly impossible for a dog-team to haul an _empty_ sledge up this place, and yet it was the only place where there was anything else than an inclined plane of rocks. The glacier was covered with snow, but in many places the ice could be seen cropping out, the snow being only a thin covering. Some ice-grottoes were also seen. They clambered up the rocks to the left, and found themselves on a stony plateau. Off to the east was an elevated ridge or knoll, toward which they traveled about a mile and a half. On gaining it, the barometer showed an elevation of thirteen hundred feet. Toward the south was a chain of mountains running east and west, through the western extremity of which the main stream-bed they had ascended seemed to break, about six miles from the sea. The branch appeared to end at the glacier; but to the east of it the land sloped north and south, and formed a surface-drain which, running east, soon narrowed into a gorge, and, bending to the north, reached the sea just west of Rest Gorge, as well as they could make out. At the bend was a large formation of ice or snow.