CALIFORNIA by John Muir: My First Summer in the Sierra, Picturesque California, The Mountains of California, The Yosemite & Our National Parks (Illustrated Edition). John Muir. Читать онлайн. Newlib. NEWLIB.NET

Автор: John Muir
Издательство: Bookwire
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Жанр произведения: Путеводители
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isbn: 9788075838117
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of nature, amid the wildest displays of her power. In the bright spring mornings the black-walled recess at the foot of the Lower Yosemite Fall is lavishly filled with irised spray, which does not simply span the dashing foam, but the foam itself, the whole mass of it, seems to be colored, and drifts and wavers, mingling with the foliage of the adjacent trees, without suggesting any relationship to the ordinary rainbow. This is perhaps the largest and most reservoir-like accumulation of iris color to be found in the valley.

      The lunar rainbows, or spraybows, are grandly developed in the spray of the Upper Fall. Their colors are as distinct as those of the sun, and as regularly and obviously banded, though less vivid. They may be seen any night when there is plenty of moonlight and spray.

      Even the secondary bow is at times distinctly visible. The best point from which to observe them is on the upper ledge, 400 feet above the base of the fall on the east side. For some time after moonrise the arc is about 400 to 500 feet span, set upright, one end planted in the spray at the bottom, the other in the edge of the fall, creeping lower, of course, and becoming less upright as the moon rises higher. This grand arc of color, glowing with such invincible peacefulness and mild shapely beauty in so weird and dark a chamber of shadows, and amid the rush and roar and tumultuous dashing of this thunder-voiced fall, is one of the most impressive sights offered in all this wonder-filled valley.

      Smaller bows may be seen in the gorge on the plateau between the upper and lower falls. Once toward midnight, after spending a few hours with the wild beauty of the upper fall, I sauntered along the edge of the gorge, looking in here and there, wherever the footing felt safe, to see what I could learn of the night aspects of the smaller falls that dwell there. And down in an exceedingly black, pit-like portion of the gorge, at the foot of the highest of the intermediate falls, while the moonbeams were pouring into it through a narrow opening, I saw a well-defined spraybow, beautifully distinct in colors, spanning across from side to side of the pit.

      In the pool at the foot of the fall pure white foam waves were constantly springing up into the moonshine, beneath the beautiful bow, like a band of dancing ghosts.

      The leaping waves so foamy white, amid rocks and shadows so weird and black, and the mystic circle of colored light, made a scene in the general gloom of the night marvelously vivid and wild. Another marvelous night scene, but not a safe one, is a view of the full moon through the edge of the Upper Fall, from the narrow ledge that extends back of it, 400 feet above its base. But the ledge is less than a foot wide on the face of the wall at one place, and though considerably wider behind the fall, it is rounded on the edge by the action of the water, and the fall is liable to be swayed against it even in calm nights; therefore one is in danger of being washed off. My own experiences one night back of the fall, when it was booming in all its glory, were such that I shall never venture there again. But the effect was enchanting; wild music above, beneath, around. The moon appeared to be in the very midst of the rushing waters and struggling to keep her place, on account of the ever-varying density and forms of the masses through which she was seen; now darkened by a rush of opaque comets, now flashing out through openings of gaudy tissue, suffering a rushing succession of eclipses that lasted but a moment--a rare astronomical phenomenon, a transit of a thousand comets across the disc of the moon.

      A very telling excursion may be made to Glacier Point and Sentinel Dome, thence across the Illilouette and Little Yosemite Valley, and return to the valley past the Nevada and Vernal falls. On the trail leading up the craggy wall to Glacier Point, the main rocks and falls of the valley are seen in striking positions and combinations, developing marvelously grand and beautiful effects as you climb from point to point. At an elevation of about 500 feet, a wide sweeping view down the valley is obtained past the Sentinel, and between Cathedral Rock and El Capitan. At 1,500 feet the wide upper end of the valley comes in sight, bounded by the great Half Dome, that looms sublimely into the azure, overshadowing every other feature of the landscape.

      From Glacier Point you look down over the edge of a sheer wall 3,000 feet high, upon soft green meadows and innumerable spires of the yellow pine, with the bright ribbon of the river curving through their midst. On the opposite side of the valley a fine general view is presented of the Royal Arches, North Dome, Indian Canyon, and Eagle Cliff, with Mt. Hoffman and the dome-paved basin of Yosemite Creek in the distance. To the eastward, Clouds Rest is seen beyond the Half Dome, and Mt. Starr King girdled with silver firs, the deeply sculptured peaks of the Merced Group, and about Mt. Lyell on the axis of the range, and broad swaths of forests growing on ancient moraines, while the Nevada, Vernal, and Yosemite falls, in full view, are as distinctly heard as if one were standing in their spray.

      Here the attentive observer will not fail to perceive that all this glorious landscape is new, lately brought to light from beneath the universal icesheet of the Glacial Period, and that the loftiest domes have been overswept by it as boulders are overswept by a flood. Hence the most resisting parts of the landscape are the highest. Every dome, ridge, and mountain in the fore and middle grounds are seen to have rounded outlines, while those of the summit peaks are sharp, the former having been overflowed by the heavy grinding folds of the ice-sheet while the latter were downflowed, thus grinding them into sharp peaks and crests. Here you see the tributary valleys or canyons of the main Yosemite Valley branching far and wide into the fountains of perpetual ice and snow. Adown these wide polished valleys once poured the ancient glaciers that united here to form the main Yosemite Glacier that eroded the valley out of the solid, wearing its channel gradually deeper, crawling on, unhalting, unresting, throughout the countless centuries of the Ice Period.

      The distant views from the summit of Sentinel Dome are still more extensive and telling, and many charming Alpine plants--phlox, telinum, eriogonae, rock-ferns, etc. are found there.

      On the way to Little Yosemite a view of the Illilouette Fall may be obtained from its head, though it is much inferior to the view obtained at the foot of the fall by scrambling up its rocky canyon from the valley. The fall in general appearance most resembles the Nevada. Before coming to the brink of the precipice its waters are severely dashed and tossed by steps and jutting angles on the bottom and sides of its channel, therefore it is a very white and finely textured fall. When in full play it is columnar and richly fluted from the partial division of its waters on the roughened lip of the precipice. It is not nearly so grand a fall as the Upper Yosemite, so symmetrical as the Vernal, or so nobly simple as the Bridal Veil; nor does it present so overwhelming an outgush of snowy magnificence as the Nevada, but in the richness and exquisite fineness of texture of its flowing folds it surpasses them all. After crossing the Illilouette Valley the trail descends into the Little Yosemite near the lower end, and thence down past the Nevada and Vernal falls to the main valley. But before returning, a visit should be made through the Little Yosemite. It is about four miles long, half a mile wide, and its walls are from 1,500 to 2,500 feet in height, bold and sheer and sculptured in true Yosemite style. And, since its rocks have not been so long exposed to post-glacial weathering, they are less blurred than those of the lower valley, large areas of the wall surfaces showing a beautiful glacial polishing that reflect the sunshine like glass.

      The bottom of the valley is flat and covered with showy gardens, meadows, rose and azalia thickets, and beautiful groves of silver-fir and pine; while the river, charmingly embowered, flows through the midst of them, softly gliding over smooth, shining sands in peaceful, restful beauty. At the head of the valley there is a showy cascade where the river flows over a bar of granite so moderately inclined that one may enjoy a climb close alongside the glad dancing flood, with but little danger of being washed away.

      This used to be a favorite hunting ground of the Indians, where they found abundance of game--mountain quail, grouse, deer, and the cinnamon bear--gathered together as if enclosed in a high-walled park with gates easily guarded. But the noisy, destructive methods of tourist sportsmen have driven most of the game away.

      As the river approaches the Nevada Fall after its tranquil flow through the valley levels, its channel is roughened with projecting rock-ribs and elbows, the object of which seems to be to fret the stream into foam and fit it for its grand display. And with what eager enthusiasm it accepts its fate, dashing on side angles, surging against round, bossy knobs, swirling in pot holes, upglancing in shallow, curved basins, then bounding out over the brink and down the grand descent, more air than water, glowing like a sun