John Muir: Wilderness Essays, Environmental Studies, Memoirs & Letters (Illustrated Edition). John Muir
the Little Yosemite Valley. It resembles the main Yosemite, though formed on a smaller scale. Then you find a long train of booming, dancing cascades, alternating with rapids and lakes and short, tranquil reaches, and a grand variety of smaller Yosemite valleys, garden patches and forests in hollows, here and there, where soil has been accumulated, until at length the icy fountains of the river are reached among the alpine peaks of the summit.
The Yosemite Valley was discovered in 1851, by Captain Boling, who then, with two Indians as guides, led a company of soldiers into it from Mariposa to punish a band of marauding Indians who occupied the valley as their home and stronghold.
The regular Yosemite pleasure travel began in 1856, and has gradually increased until the present time. Considering the remoteness of many of the fountains of this current of travel, its flow has been remarkably constant. The regular tourist, ever in motion, is one of the most characteristic productions of the present century; and however frivolous and inappreciative the poorer specimens may appear, viewed comprehensively they are a hopeful and significant sign of the times, indicating at least a beginning of our return to nature; for going to the mountains is going home. Perhaps nowhere else along the channels of pleasure travel may so striking and interesting a variety of people be found together as in this comparatively wild and remote Yosemite. Men, women, and children of every creed and color come here from every country under the sun; farmers, men of business, lawyers, doctors, and divines; scientists seeking causes, wealthy and elegant loafers trying to escape from themselves, the titled and obscure, all in some measure seeing and loving wild beauty, and traveling to better purpose than they know, bome onward by currents that they cannot understand, like ships at sea.
Arriving in the valley most parties keep together and fall into the hands of the local guides by whom they are led hastily from point to point along the beaten trails. Others separate more or less and follow their own ways. These are mostly members of Alpine Clubs, sturdy Englishmen and Germans, with now and then a cannie Scotchman, all anxious to improve their opportunities to the utmost. Besides rambling at will into odd comers of the valley, they climb about the canyons, and around the tops of the walls; or push out bravely over the adjacent mountains, radiating far into the High Sierra among the ice and snow. They thread the mazes of the glorious forests, and trace the wild young streams in their courses down from the glaciers through grandly sculptured canyons, past garden hollows and lake basins, and down glossy inclines, sharing in all their exhilarating rush and roar.
Gentle, contemplative grandmothers, and a few fine-grained specimens of fewer years, spend most of their time sauntering along the banks of the river, and sitting in the shade of the trees; admiring sky and cliff, and falling water, in a quiet way, enriching their lives far more than their neighbors who keep themselves in perpetual motion, following each other along dusty trails, painfully "doing" the valley by rule.
Little children are, of course, the most delightfully natural of all the visitors, flashing around the hotel verandahs, or out beneath the trees, glowing in rainbow-hued ruffles and ribbons like butterflies and scarlet tanagers. They consider the lilies and birds and bees, nor are they altogether unconscious of the glorious sublimities about them; for one may see them at times gazing silently with upturned faces at the mighty cliffs, and at the white water pouring out of the sky, their pure, natural wonderment offering a refreshing contrast to the mean complacency and blindness of the finished tourist, who has seen all, knows all, and is engulfed in eternal apathetic tranquillity.
The Yosemite Fall is partially separated into an upper and lower fall, with a series of smaller falls and cascades between them, but when viewed in front they appear as one, only slightly interrupted by striking on what seems to be a narrow ledge. First there is a sheer descent of about 1,600 feet; then a succession of cascades and smaller falls nearly a third of a mile long, and making altogether a descent of 600 feet; then a final sheer fall of about 400 feet is made to the bottom of the valley. So grandly does this magnificent fall display itself from the floor of the valley few visitors take the trouble to climb the wall to gain nearer views, unable to realize how vastly more impressive it becomes when closely approached, instead of being seen at a distance of from one to two miles.
The views developed in a walk up the zigzags of the trail leading to the upper fall are as varied and impressive and almost as extensive, as those on the well-known Glacier Point Trail. One rises as if on wings. The groves, meadows, fern-flats, and reaches of the river at once gain new interest, as if never seen before, and all become new over and over again as we go higher from point to point; the foreground also changes every few rods in the most surprising manner, although the bench on the face of the wall over which the trail passes is very monotonous and commonplace in appearance as seen from the bottom of the valley. Up we climb with glad exhilaration, through shaggy fringes of laurel and ceanothus, and glossy-leaved manzanita and live oak from shadow to shadow across bars of sunshine, the leafy openings making charming frames for the valley pictures beheld through them, and for the glimpses of the high alps that appear in the distance. The higher we go, the farther we seem to be from the summit of the vast carved wall up which we are creeping. Here we pass a huge projecting buttress whose grooved and rounded surface tells a wonderful story of the time when the valley now filled with sunshine was filled with ice, when a grand old glacier, flowing river-like from its many fountains on the snow-laden summits of the range, swept through the valley with its crushing, grinding floods, wearing its way ever deeper, and fashioning these sublime cliffs to the varied forms of beauty they now possess. Here a white, battered gully marks the pathway of an avalanche of rocks, now we cross the channel of an avalanche of snow. Farther on we come to a small stream clinging to the face of the cliff in lace-like strips, or leaping from ledge to ledge, too small and feeble to be called a fall, trickling, dripping, slipping, oozing, a pathless wanderer from the upland meadows, seeking a way century after century to the depths of the valley without having worn any appreciable channel. Constant dropping has not worn away these stones. Every morning, after a cool night, evaporation being checked, it gathers strength and sings like a bird, but as the day advances, and the sun strikes its thin currents outspread on the heated precipices, most of its waters vanish long ere the bottom of the valley is reached. Many a fine, hanging garden aloft on these breezy inaccessible heights owe to it their freshness and fullness of beauty; ferneries in shady nooks, filled with adiantum, woodwardia, woodsia, aspidium, pellaea, and cheilanthes; rosetted and tufted and ranged in lines, daintily overlapping, thatching the stupendous cliffs with softest beauty, the delicate fronds seeming to float on the warm, moist air, without any connection with rock or stream. And colored plants, too, in abundance, wherever they can find a place to cling to; the showy cardinal mimulus, lilies and mints, and glowing cushions of the golden bahia, together with sedges and grasses growing in tufts, and the butterflies and bees and all the small, happy creatures that belong to them.
After the highest point on the lower division of the trail is gained it conducts along a level terrace on the face of the wall, around a shoulder, and into the deep recess occupied by the great Upper Yosemite Fall, the noblest display of falling water to be found in the valley, or, perhaps, in the world. When it first comes in sight, it seems almost within reach of one's hand, so great is its volume and velocity, yet it is still nearly a third of a mile away, and appears to recede as we advance. The sculpture of the walls about it is on a scale of grandeur, according nobly with the fall, plain and massive, though elaborately finished, like all the other cliffs about the valley.
In the afternoon an immense shadow is cast athwart the plateau in front of the fall, and far over the fields of chaparral that clothe the slopes and benches of the wall to the eastward, creeping upward upon the fall until it is wholly overcast, the contrast between the shaded and illuminated sections being very striking in near views.
Under this shadow, during the cool centuries immediately following the breaking up of the Glacial Period, dwelt a small residual glacier, one of the few that lingered on this sun-beaten side of the valley after the main trunk glacier had vanished. It sent down a long winding current through the narrow canyon on the west side of the fall, and must have formed a striking feature of the ancient scenery of the valley; the lofty fall of ice and fall of water side by side, yet separate and distinct.
The coolness of the afternoon shadow and the abundant dewy moisture from the spray of the fall make a fine climate for ferns and grasses on the plateau, and for the beautiful azalia, which grows