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t of ice-covered rock towering six thousand or seven thousand feet above the glacier floor, the first of the very impressive features of the mountain. The other wall of the glacier, through a breach in which we reached its surface--the right-hand wall as we journeyed up it--consists of a series of inaccessible cliffs deeply seamed with snow gullies and crusted here and there with hanging glaciers, the rock formation changing several times as one proceeds but maintaining an unbroken rampart. Now, it is important to remember that these two ridges which make the walls of the Muldrow Glacier rise ultimately to the two summits of the mountain, the right-hand wall culminating in the North Peak and the left-hand wall in the South Peak. And the glacier lies between the walls all the way up and separates the summits, with this qualification--that midway in its course it is interrupted by a perpendicular ice-fall of about four thousand feet by which its upper portion discharges into its lower. It will help the reader to a comprehension of the ascent if this rough sketch be borne in mind. [Illustration: The Muldrow Glacier. Karstens in the foreground.] The course of the glacier at the point at which we reached it is nearly northeast and southwest (magnetic); its surface is almost level and it is free of crevasses save at its sides. For three or four miles above the pass it pursues its course without change of direction or much increase in grade; then it takes a broad sweep toward the south and grows steep and much crevassed. Three miles farther up it takes another and more decided southerly bend, receiving two steep but short tributaries from the northwest at an elevation of about ten thousand feet, and finishing its lower course in another mile and a half, at an elevation of about eleven thousand five hundred feet, with an almost due north and south direction (magnetic). A week after our first sight of the glacier, or on the 18th April, we were camped at about the farthest point we had been able to see on that occasion--just round the first bend. Our stuff had been freighted to the pass and cached there; then, in the usual method of our advance, the camp had been moved forward beyond the cache on to the glacier, a full day's march. Then the team worked backward, bringing up the stuff to the new camp. Thus three could go ahead, prospecting and staking out a trail for further advance, while two worked with the dog team at th
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