!DOCTYPE html PUBLIC "-//W3C//DTD XHTML 1.0 Strict//EN" "http://www.w3.org/TR/xhtml1/DTD/xhtml1-strict.dtd"> Streamline Training & Documentation: John Muir Festival IV: Mount Rainier

Thursday, June 25, 2009

John Muir Festival IV: Mount Rainier

Mount Rainier,
by Albert Bierstadt (1830 - 1902)


By night of the third day we reached the Soda Springs on the right bank of the Nisqually, which goes roaring by, gray with mud, gravel, and boulders from the caves of the glaciers of Rainier, now close at hand. The distance from the Soda Springs to the Camp of the Clouds is about ten miles. The first part of the way lies up the Nisqually Canyon, the bottom of which is flat in some places and the walls very high and precipitous, like those of the Yosemite Valley. The upper part of the canyon is still occupied by one of the Nisqually glaciers, from which this branch of the river draws its source, issuing from a cave in the gray, rock-strewn snout. About a mile below the glacier we had to ford the river, which caused some anxiety, for the current is very rapid and carried forward large boulders as well as lighter material, while its savage roar is bewildering.

At this point we left the canyon, climbing out of it by a steep zigzag up the old lateral moraine of the glacier, which was deposited when the present glacier flowed past at this height, and is about eight hundred feet high. It is now covered with a superb growth of Picea amabilis [30]; so also is the corresponding portion of the right lateral. From the top of the moraine, still ascending, we passed for a mile or two through a forest of mixed growth, mainly silver fir, Patton spruce, and mountain pine, and then came to the charming park region, at an elevation of about five thousand feet above sea level. Here the vast continuous woods at length begin to give way under the dominion of climate, though still at this height retaining their beauty and giving no sign of stress of storm, sweeping upward in belts of varying width, composed mainly of one species of fir, sharp and spiry in form, leaving smooth, spacious parks, with here and there separate groups of trees standing out in the midst of the openings like islands in a lake. Every one of these parks, great and small, is a garden filled knee-deep with fresh, lovely flowers of every hue, the most luxuriant and the most extravagantly beautiful of all the alpine gardens I ever beheld in all my mountain-top wanderings.

[. . .]

At noon next day we left camp and began our long climb. We were in light marching order, save one who pluckily determined to carry his camera to the summit. At night, after a long easy climb over wide and smooth fields of ice, we reached a narrow ridge, at an elevation of about ten thousand feet above the sea, on the divide between the glaciers of the Nisqually and the Cowlitz. Here we lay as best we could, waiting for another day, without fire of course, as we were now many miles beyond the timberline and without much to cover us. After eating a little hardtack, each of us leveled a spot to lie on among lava-blocks and cinders. The night was cold, and the wind coming down upon us in stormy surges drove gritty ashes and fragments of pumice about our ears while chilling to the bone. Very short and shallow was our sleep that night; but day dawned at last, early rising was easy, and there was nothing about breakfast to cause any delay. About four o'clock we were off, and climbing began in earnest. We followed up the ridge on which we had spent the night, now along its crest, now on either side, or on the ice leaning against it, until we came to where it becomes massive and precipitous. Then we were compelled to crawl along a seam or narrow shelf, on its face, which we traced to its termination in the base of the great ice cap. From this point all the climbing was over ice, which was here desperately steep but fortunately was at the same time carved into innumerable spikes and pillars which afforded good footholds, and we crawled cautiously on, warm with ambition and exercise.

At length, after gaining the upper extreme of our guiding ridge, we found a good place to rest and prepare ourselves to scale the dangerous upper curves of the dome. The surface almost everywhere was bare, hard, snowless ice, extremely slippery; and, though smooth in general, it was interrupted by a network of yawning crevasses, outspread like lines of defense against any attempt to win the summit. Here every one of the party took off his shoes and drove stout steel caulks about half an inch long into them, having brought tools along for the purpose, and not having made use of them until now so that the points might not get dulled on the rocks ere the smooth, dangerous ice was reached. Besides being well shod each carried an alpenstock, and for special difficulties we had a hundred feet of rope and an axe.

Thus prepared, we stepped forth afresh, slowly groping our way through tangled lines of crevasses, crossing on snow bridges here and there after cautiously testing them, jumping at narrow places, or crawling around the ends of the largest, bracing well at every point with our alpenstocks and setting our spiked shoes squarely down on the dangerous slopes. It was nerve-trying work, most of it, but we made good speed nevertheless, and by noon all stood together on the utmost summit, save one who, his strength failing for a time, came up later.

We remained on the summit nearly two hours, looking about us at the vast maplike views, comprehending hundreds of miles of the Cascade Range, with their black interminable forests and white volcanic cones in glorious array reaching far into Oregon; the Sound region also, and the great plains of eastern Washington, hazy and vague in the distance. Clouds began to gather. Soon of all the land only the summits of the mountains, St. Helen's, Adams, and Hood, were left in sight, forming islands in the sky. We found two well-formed and well-preserved craters on the summit, lying close together like two plates on a table with their rims touching. The highest point of the mountain is located between the craters, where their edges come in contact. Sulphurous fumes and steam issue from several vents, giving out a sickening smell that can be detected at a considerable distance. The unwasted condition of these craters, and, indeed, to a great extent, of the entire mountain, would tend to show that Rainier is still a comparatively young mountain. With the exception of the projecting lips of the craters and the top of a subordinate summit a short distance to the northward, the mountains is solidly capped with ice all around; and it is this ice cap which forms the grand central fountain whence all the twenty glaciers of Rainier flow, radiating in every direction.

[. . .]

Source: Excerpt from "An Ascent of Mount Rainer," Chapter 20 of John Muir's 1918 book, Steep Trails. You can read the full text of the book here.


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