In sharp contrast with these valley scenes is the view from Glacier Point down into the Merced and Tenaya Canyons, and out over the magical park landscape to the snow-capped mountains of the High Sierra. Two trails lead from the valley up to Glacier Point, and high upon the precipice, three thousand feet above the valley floor, is a picturesque hotel; it is also reached by road. Here one may sit at ease on shady porches and overlook one of the most extended, varied and romantic views in the world of scenery. One may take dinner on this porch and have sunset served with dessert and the afterglow with coffee.
Here again one is haunted by the suggestion of artistic intention, so happy is the composition of this extraordinary picture. The foreground is the dark, tremendous gulf of Merced Canyon, relieved by the silver shimmer of Vernal and Nevada Falls. From this in middle distance rises, in the centre of the canvas, the looming tremendous personality of Half Dome, here seen in profile strongly suggesting a monk with outstretched arms blessing the valley at close of day. Beyond stretches the horizon of famous, snowy, glacier-shrouded mountains, golden in sunset glow.
III
Every summer many thousands of visitors gather in Yosemite. Most of them, of course, come tourist-fashion, to glimpse it all in a day or two or three. A few thousands come for long enough to taste most of it, or really to see a little. Fewer, but still increasingly many, are those who come to live a little with Yosemite; among these we find the lovers of nature, the poets, the seers, the dreamers, and the students.
Living is very pleasant in the Yosemite. The freedom from storm during the long season, the dry warmth of the days and the coldness of the nights, the inspiration of the surroundings and the completeness of the equipment for the comfort of visitors make it extraordinary among mountain resorts. There is a hotel in the Valley, and another upon the rim at Glacier Point. There are three large hotel-camps in the Valley, where one may have hotel comforts under canvas at camp prices. Two of these hotel-camps possess swimming pools, dancing pavilions, tennis courts electrically lighted for night play, hot and cold-water tubs and showers, and excellent table service. One of the hotel-camps, the largest, provides evening lectures, song services, and a general atmosphere suggestive of Chatauqua. Still a third is for those who prefer quiet retirement and the tradition of old-fashioned camp life.
Above the valley rim, besides the excellent hotel upon Glacier Point, there are at this writing hotel-camps equipped with many hotel comforts, including baths, at such outlying points as Merced Lake and Tenaya Lake; the former centering the mountain climbing and trout fishing of the stupendous region on the southwest slope of the park, and the latter the key to the entire magnificent region of the Tuolumne. These camps are reached by mountain trail, Tenaya Lake Camp also by motor road. The hotel-camp system is planned for wide extension as growing demand warrants. There are also hotels outside park limits on the south and west which connect with the park roads and trails.
The roads, by the way, are fair. Three enter from the west, centering at Yosemite Village in the Valley; one from the south by way of the celebrated Mariposa Grove of giant sequoias; one from El Portal, terminus of the Yosemite Railway; and one from the north, by way of several smaller sequoia groves, connecting directly with the Tioga Road.
Above the valley rim and north of it, the Tioga Road crosses the national park and emerges at Mono Lake on the east, having crossed the Sierra over Tioga Pa.s.s on the park boundary. The Tioga Road, which was built in 1881, on the site of the Mono Trail, to connect a gold mine west of what has since become the national park with roads east of the Sierra, was purchased in 1915 by patriotic lovers of the Yosemite and given to the Government. The mine having soon failed, the road had been impa.s.sable for many years. Repaired with government money it has become the princ.i.p.al highway of the park and the key to its future development.
The increase in motor travel to the Yosemite from all parts of the country which began the summer following the Great War, has made this gift one of growing importance. It affords a new route across the Sierra.
But hotels and hotel-camps, while accommodating the great majority of visitors, by no means shelter all. Those who camp out under their own canvas are likely to be Yosemite"s most appreciative devotees. The camping-out colony lives in riverside groves in the upper reaches of the Valley, the Government a.s.signing locations without charge. Many families make permanent summer homes here, storing equipment between seasons in the village. Others hire equipment complete, from tents to salt-cellars, on the spot. Some who come to the hotels finish the season under hired canvas, and next season come with their own. An increasing number come in cars, which they keep in local garages or park near their canvas homes.
Living is easy and not expensive in these camp homes. Midday temperatures are seasonable, and nights are always cool. As it does not rain, tents are concessions to habit; many prefer sleeping under the trees. Markets in the village supply meats, vegetables, milk, bread, and groceries at prices regulated by Government, and deliver them at your kitchen tent. Shops furnish all other reasonable needs. It is not camping out as commonly conceived; you are living at home on the banks of the Merced, under the morning shadow of Half Dome, and within sight of Yosemite Falls.
From these Valley homes one rides into the High Sierra on horses hired from the government concessioner, tours to the Tuolumne Meadows or the Mariposa Grove by automobile, wanders long summer afternoons in the Valley, climbs the great rocks and domes, picnics by moonlight under the shimmering falls or beneath the shining tower of El Capitan, explores famous fishing waters above the rim, and, on frivolous evenings, dances or looks at motion pictures at the greater hotel-camps.
No wonder that camp homes in the Yosemite are growing in popularity.
IV
The trail traveller finds the trails the best in the country, and as good as the best in the world; they are the models for the national system. Competent guides, horses, supplies, and equipment are easy to hire at regulated prices in the village.
As for the field, there is none n.o.bler or more varied in the world.
There are dozens of divides, scores of towering, snow-splashed peaks, hundreds of n.o.ble valleys and shining lakes, thousands of cascading streams, great and small, from whose depths fighting trout rise to the cast fly. There are pa.s.ses to be crossed which carry one through concentric cirques of toothed granite to ridges from which the High Sierra spreads before the eye a frothing sea of snowy peaks.
Such a trip is that through Tuolumne Meadows up Lyell Canyon to its headwaters, over the Sierra at Donohue Pa.s.s, and up into the birth chambers of rivers among the summit glaciers of Lyell and McClure--a never-to-be-forgotten journey, which may be continued, if one has time and equipment, down the John Muir Trail to Mount Whitney and the Sequoia National Park. Or one may return to the park by way of Banner Peak and Thousand Island Lake, a wonder spot, and thence north over Parker and Mono Pa.s.ses; trips like these produce views as magnificent as the land possesses.
s.p.a.ce does not permit even the suggestion of the possibilities to the trail traveller of this wonderland above the rim. It is the summer playground for a nation.
Second in magnificence among the park valleys is Hetch Hetchy, the Yosemite of the north. Both are broad, flowered and forested levels between lofty granite walls. Both are accented by gigantic rock personalities. Kolana Rock, which guards Hetch Hetchy at its western gateway as El Capitan guards Yosemite, must be ranked in the same cla.s.s.
Were there no Yosemite Valley, Hetch Hetchy, though it lacks the distinction which gives Yosemite Valley its world-wide fame, would be much better known than it now is--a statement also true about other features of the national park.
Hetch Hetchy is now being dammed below Kolana Rock to supply water for San Francisco. The dam will be hidden from common observation, and the timber lands to be flooded will be cut so as to avoid the unsightliness usual with artificial reservoirs in forested areas. The reservoir will cover one of the most beautiful bottoms in America. It will destroy forests of luxuriance. It will replace these with a long sinuous lake, from which sheer Yosemite-like granite walls will rise abruptly two or three thousand feet. There will be places where the edges are forested.
Down into this lake from the high rim will cascade many roaring streams.
The long fight in California, in the press of the whole country, and finally in Congress, between the advocates of the Hetch Hetchy reservoir and the defenders of the scenic wilderness is one of the stirring episodes in the history of our national parks. At this writing, time enough has not yet pa.s.sed to heal the wounds of battle, but at least we may look calmly at what remains. One consideration, at least, affords a little comfort. Hetch Hetchy was once, in late prehistoric times, a natural lake of great n.o.bility. The remains of Nature"s dam, not far from the site of man"s, are plain to the geologist"s eye. It is possible that, with care in building the dam and clearing out the trees to be submerged, this restoration of one of Nature"s n.o.ble features of the past may not work out so inappropriately as once we feared.
[Ill.u.s.tration: _From a photograph by J.T. Boysen_
THE CLIMAX OF YOSEMITE NATIONAL PARK
Mount Lyell and its glacier from Lyell Fork]
[Ill.u.s.tration: THE GREATEST WATERWHEEL OF THE TUOLUMNE
It is fifty feet in height and seventy-five feet long; Yosemite National Park]
The Grand Canyon of the Tuolumne, through which the river descends from the level of the Tuolumne Meadows almost five thousand feet to the Hetch Hetchy Valley, possesses real Yosemite grandeur. Much of this enormous drop occurs within a couple of amazing miles west of the California Falls. Here the river slips down sharply tilted granite slopes at breathless speed, breaking into cascades and plunging over waterfalls at frequent intervals. It is a stupendous spectacle which few but the hardiest mountaineers saw previous to 1918, so steep and difficult was the going. During that season a trail was opened which makes accessible to all one of the most extraordinary examples of plunging water in the world.
The climax of this spectacle is the Waterwheels. Granite obstructions in the bed of the steeply tilted river throw solid arcs of frothing water fifty feet in air. They occur near together, singly and in groups.
V
The fine camping country south of the Yosemite Valley also offers its sensation. At its most southern point, the park accomplishes its forest climax in the Mariposa Grove. This group of giant sequoias (Sequoia washingtoniana) ranks next, in the number and magnificence of its trees, to the Giant Forest of the Sequoia National Park and the General Grant grove.
The largest tree of the Mariposa Grove is the Grizzly Giant, which has a diameter of twenty-nine feet, a circ.u.mference of sixty-four feet, and a height of two hundred and four feet. One may guess its age from three thousand to thirty-two hundred years. It is the third in size and age of living sequoias; General Sherman, the largest and oldest, has a diameter of thirty-six and a half feet, and General Grant a diameter of thirty-five feet, and neither of these, in all probability, has attained the age of four thousand years. General Sherman grows in the Sequoia National Park, seventy miles or more south of Yosemite; General Grant has a little national park of its own a few miles west of Sequoia.
The interested explorer of the Yosemite has so far enjoyed a wonderfully varied sequence of surprises. The incomparable valley with its towering monoliths and extraordinary waterfalls, the High Sierra with its glaciers, serrated cirques and sea of snowy peaks, the Grand Canyon of the Tuolumne with its cascades, rushing river and frothing Waterwheels, are but the headliners of a long catalogue of the unexpected and extraordinary. It only remains, to complete this new tale of the Arabian Nights, to make one"s first visit to the sequoias of Mariposa Grove. The first sight of the calm tremendous columns which support the lofty roof of this forest temple provokes a new sensation. Unconsciously the visitor removes his hat and speaks his praise in whispers.
The sequoias are considered at greater length in the chapter describing the Sequoia National Park, which was created especially to conserve and exhibit more than a million of these most interesting of trees. It will suffice here to say that their enormous stems are purplish red, that their fine, lace-like foliage hangs in splendid heavy plumes, that their enormous limbs crook at right angles, the lowest from a hundred to a hundred and fifty feet above the ground, and that all other trees, even the gigantic sugar pine and Douglas fir, are dwarfed in their presence.
Several of the sequoias of the Mariposa grove approach three hundred feet in height. The road pa.s.ses through the trunk of one.
VI
The human history of the Yosemite is quickly told. The country north of the Valley was known from early times by explorers and trappers who used the old Mono Indian Trail, now the Tioga Road, which crossed the divide over Mono Pa.s.s. But, though the trail approached within a very few miles of the north rim of the Yosemite Valley, the valley was not discovered till 1851, when Captain Boling of the Mariposa Battalion, a volunteer organization for the protection of settlers, entered it from the west in pursuit of Indians who had raided mining settlements in the foothills.
These savages were known as the Yosemite or Grizzly Bear Indians.
Tenaya, their chief, met their pursuers on the uplands and besought them to come no further. But Captain Boling pushed on through the heavy snows, and on March 21, entered the valley, which proved to be the Indians" final stronghold. Their villages, however, were deserted.
The original inhabitants of the Valley were called the Ahwahneechees, the Indian name for the Valley being Ahwahnee, meaning a deep gra.s.sy canyon. The Ahwahneechees, previous to Captain Boling"s expedition, had been decimated by war and disease. The new tribe, the Yosemites, or Grizzly Bears, was made up of their remainder, with Monos and Piutes added.
Captain Boling"s report of the beauty of the valley having been questioned, he returned during the summer to prove his a.s.sertions to a few doubters. Nevertheless, there were no further visitors until 1853, when Robert B. Stinson of Mariposa led in a hunting-party. Two years later J.M. Hutchings, who was engaged in writing up the beauties of California for the _California Magazine_, brought the first tourists; the second, a party of sixteen, followed later the same year.
Pleasure travel to the Yosemite Valley may be said to have commenced with 1856, the year the first house was built. This house was enlarged in 1858 by Hite and Beardsley and used for a hotel. Sullivan and Cushman secured it for a debt the following year, and it was operated in turn by Peck, Longhurst, and Hutchings until 1871. Meantime J.C. Lamon settled in 1860, the first actual resident of the valley, an honor which he did not share with others for four years.
The fame of the valley spread over the country and in 1864 Congress granted to the State of California "the Cleft or Gorge of the Granite Peak of the Sierra Nevada Mountains" known as the Yosemite Valley, with the understanding that all income derived from it should be spent for improving the reservation or building a road to it. The Mariposa Big Tree Grove was also granted at the same time. California carefully fulfilled her charge. The Yosemite Valley became world-famous, and in 1890 the Yosemite National Park was created.
VII
The Yosemite"s geological history is much more thrilling. Everyone who sees it asks, How did Nature make the Yosemite Valley? Was it split by earth convulsions or scooped by glacier? Few ask what part was played by the gentle Merced.
The question of Yosemite"s making has busied geologists from Professor Whitney of the University of California, who first studied the problem, down to F.E. Matthes, of the United States Geological Survey, whose recent exhaustive studies have furnished the final solution. Professor Whitney maintained that glaciers never had entered the valley; he did not even consider water erosion. At one time he held that the valley was simply a cleft or rent in the earth"s crust. At another time he imagined it formed by the sudden dropping back of a large block in the course of the convulsions that resulted in the uplift of the Sierra Nevada. Galen Clark, following him, carried on his idea of an origin by force. Instead of the walls being cleft apart, however, he imagined the explosion of close-set domes of molten rock the riving power, but conceived that ice and water erosion finished the job. With Clarence King the theory of glacial origin began its long career. John Muir carried this theory to its extreme.
Since the period of Muir"s speculations, the tremendous facts concerning the part played by erosion in the modification of the earth"s surface strata have been developed. Beginning with W.H. Turner, a group of Yosemite students under the modern influence worked upon the theory of the stream-cut valley modified by glaciers. The United States Geological Survey then entered the field, and Matthes"s minute investigations followed; the ma.n.u.script of his monograph has helped me reconstruct the dramatic past.
The fact is that the Yosemite Valley was cut from the solid granite nearly to its present depth by the Merced River; before the glaciers arrived, the river-cut valley was twenty-four hundred feet deep opposite El Capitan, and three thousand feet deep opposite Eagle Peak. The valley was then V-shaped, and the present waterfalls were cascades; those which are now the Yosemite Falls were eighteen hundred feet deep, and those of Sentinel Creek were two thousand feet deep. All this in pre-glacial times.
Later on the glaciers of several successive epochs greatly widened the valley, and measurably deepened it, making it U-shaped. The cascades then became waterfalls.