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Updated: May 9, 2025
It was as though, as soon as the Parker-Browne party reached the foot of the mountain, the ladder by which they had ascended and descended was broken up. The earthquake cleavage is plainly shown half-way down the ridge in the background. The Browne Tower is the uppermost point in the picture. What a wonderful providential escape these three men, Parker, Browne, and La Voy had!
Having gratified this desire, as he supposed, there had meantime arisen another desire, upon reading the narrative of the Parker-Browne expedition of the previous year, a copy of which we were fortunate enough to procure just as we were starting for the mountain. It was the feeling of our whole company that the names of Professor Parker and Mr.
As is well known, the Parker-Browne party pushed up the Northeast Ridge and the upper glacier and made a first attack upon the summit itself, from a camp at seventeen thousand feet, on the 29th June. When within three or four hundred feet of the top they were overwhelmed and driven down, half frozen, by a blizzard that suddenly arose.
The Parker-Browne expedition left Seward, on Resurrection Bay, late in January, 1912, and after nearly three months' travel, relaying their stuff forward, they crossed the range under extreme difficulties, being seventeen days above any vegetation, and reached the northern face of the mountain on 25th March.
But if, attempting the mountain when they did, the Parker-Browne party had remained two or three days longer in the Grand Basin, which they would assuredly have done had their food been eatable, their bodies would be lying up there yet or would be crushed beneath the débris of the earthquake on the ridge.
This ridge, that the pioneer climbers of 1910 went up at one march with climbing-irons strapped beneath their moccasins, carrying nothing but their flagpole, that the Parker-Browne party surmounted in a few days, relaying their camping stuff and supplies, was to occupy us for three weeks while we hewed a staircase three miles long in the shattered ice.
Now just before leaving Fairbanks we had received a copy of a magazine containing the account of the Parker-Browne climb, and in that narrative Mr. Browne speaks of this Northeast Ridge as "a steep but practicable snow slope," and prints a photograph which shows it as such.
The designation "Northeast," which the Parker-Browne party put upon the ridge that affords passage from the lower glacier to the upper, is open to question. Mr. Charles Sheldon, who spent a year around the base of the mountain studying the fauna of the region, refers to the outer wall of the Muldrow Glacier as the Northeast Ridge, that is, the wall that rises to the North Peak.
Our course was almost precisely the same as that of the Parker-Browne party up to seventeen thousand feet, and the course of that party was precisely the same as that of the Lloyd party up to fifteen thousand feet. There is only one way up the mountain, and Lloyd and his companions discovered it. The earthquake had enormously increased the labor of the ascent; it had not altered the route.
All at once the explanation came to us "the earthquake"! The Parker-Browne party had reported an earthquake which shook the whole base of the mountain on 6th July, 1912, two days after they had come down, and, as was learned later, the seismographic instruments at Washington recorded it as the most severe shock since the San Francisco disturbance of 1906.
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