The photograph of the base camp shows a mountainous ridge stretching across much of the background. That ridge belongs to the outer wall of the Muldrow Glacier and indicates its general direction. Just beyond the picture, to the right, the ridge breaks down, and the little valley in the middle distance sweeps around, becomes a steep, narrow gulch, and ends at the breach in the glacier wall. This breach, thus reached, is the pass which the Kantishna miners of the “pioneer” expedition discovered and named “McPhee Pass,” after a Fairbanks saloon-keeper. The name should stand. There is no other pass by which the glacier can be reached; certainly none at all above, and probably no convenient one below. Unless this pass were used, it would be necessary to make the long and difficult journey to the snout of the glacier, some twenty miles farther to the east, cross its rough terminal moraine, and traverse all its lower stretch.

On the 11th April Karstens and I wound our way up the narrow, steep defile for about three miles from the base camp and came to our first sight of the Muldrow Glacier, some two thousand five hundred feet above camp and six thousand, three hundred feet above the sea. That day stands out in recollection as one of the notable days of the whole ascent. There the glacier stretched away, broad and level—the road to the heart of the mountain, and as our eyes traced its course our spirits leaped up that at last we were entered upon our real task. One of us, at least, knew something of the dangers and difficulties its apparently smooth surface concealed, yet to both of us it had an infinite attractiveness, for it was the highway of desire.


CHAPTER II

THE MULDROW GLACIER

Right opposite McPhee Pass, across the glacier, perhaps at this point half a mile wide, rises a bold pyramidal peak, twelve thousand or thirteen thousand feet high, which we would like to name Mount Farthing, in honor of the memory of a very noble gentlewoman who died at the mission at Nenana three years ago, unless, unknown to us, it already bear some other name. [1] Walter and our two Indian boys had been under her instruction.

At the base of this peak two branches of the glacier unite, coming down in the same general direction and together draining the snows of the whole eastern face of the mountain. The dividing wall between them, almost up to their head and termination, is one stupendous, well-nigh vertical escarpment 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.