Features of the Proposed Yosemite National Park.

FEATURES OF THE PROPOSE NATIONAL PARK. OSEMITE HE upper Tuolumne Valley is the widest, smoothest, most serenely spacious, and in every way the most delightful summer pleasure park in all the high Sierra. And since it is connected with Yosemite by two good trails, and with the levels of civilization by a broad, well- graded carriage-road that passes between Yosemite and Mount Hoffman, it is also the most accessible. It lies in the heart of the high Sierra at a height of from 8500 to 9000 feet above the level of the sea, at a distance of less than ten miles from the northeastern boundary of the Yosemite reservation. It is bounded on the southwest by the gray, jagged, picturesque Cathedral range, which extends in a southeasterly direction from Cathedral Peak to Mount Lyell and Mount Ritter, the culminating peaks of the grand mass of icy mountains that form the crown of the Sierra ; on the northeast, by a similar range or spur, the highest peak of which is Mount Conness; on the east, by the smooth, majestic masses of Mount Dana, Mount Gibbs, Mount Ord, and others, nameless as yet, on the axis of the main range; and on the west by a heaving, billowy mass of glacier-polished rocks, over which the towering masses of Mount Hoffman are seen. Down through the open sunny levels of the valley flows the bright Tuolumne River, fresh from many a glacial fountain in the wild recesses of the peaks, the highest of which are the glaciers that lie on the north sides of Mount Lyell and Mount McClure. Along the river are a series of beautiful glacier meadows stretching, with but little interruption, from the lower end of the valley to its head, a distance of about twelve miles. These form charming sauntering grounds from which the glorious mountains may be enjoyed as they look down in divine serenity over the majestic swaths of forest that clothe their bases. Narrow strips of pine woods cross the meadow- carpet from side to side, and it is somewhat roughened here and there by groves, moraine boulders, and dead trees brought down from the heights by avalanches; but for miles and miles it is so smooth and level that a hundred horsemen may ride abreast over it. The main lower portion of the meadow is about four miles long and from a quarter to 656 half a mile wide; but the width of the valley is, on an average, about eight miles. Tracing the river we find that it forks a mile above the Soda Springs, which are situated on the north bank opposite the point where the Cathedral trail comes in — the main fork turning southward to Mount.Lyell, the other eastward to Mount Dana and Mount Gibbs. Along both forks strips of meadow extend almost to their heads. The most beautiful portions of the meadows are spread over lake basins, which have been filled up by deposits from the river. A few of these river-lakes still exist, but they are now shallow and are rapidly approaching extinction. The sod in most places is exceedingly fine and silky and free from rough weeds and bushes; while charming flowers abound, especially gentians, dwarf daisies, ivesias, and the pink bells of dwarf vaccinium. On the banks of the river and its tributaries Cassiope and Bryanthus may be found where the sod curls over in bosses, and about piles of boulders. The principal grass of these meadows is a delicate Calamagrostis with very slender leaves, and when it is in flower the ground seems to be covered with a faint purple mist, the stems of the spikelets being so.fine that they are almost invisible, and offer no appreciable resistance in walking through them. Along the edges of the meadows beneath the pines and throughout the greater part of the valley tall ribbon-leaved grasses grow in abundance, chiefly Bromus, Triticum, and Agrostis. In October, the nights\u27 are frosty, and then the meadows at sunrise, when every leaf is laden with crystals,\u27aire a1 fine sight. The days are warm and\u27calm; ~aricl bees and butterflies continue to waver and hum about the late- blooming flowers until the coming of the snow, usually late in November. Storm then follows storm in close succession, burying the meadows to a depth of from ten to twenty feet, while magnificent avalanches descend through the forests from the laden heights, depositing huge piles of snow mixed with uprooted trees and boulders. In the open sunshine the snow lasts until June, but the new season\u27s vegetation is not generally in bloom until late in July. Perhaps the best time to visit this valley is in August. The snow is then melted from tht woods, and the meadows are dry and warm, while the weather is mostly sunshine, reviving 033. FEATURES OF THE PROPOSED YOSEMITE NATIONAL PARK. 657 BIG TUOLUMNE MEADOWS WITH MOUNT DANA AND MOUNT GIBBS, FROM NEAR THE SODA SPRINGS. and exhilarating in quality; and the few clouds that rise and the showers they yield are only enough for freshness, fragrance, and beauty. The groves about the Soda Springs are favorite camping-grounds on account of the- Spleasant-tasting, ie&colckwater of the springs,\u27 charged with carDorrkracid, and because of the fine views of the mountains across the meadow — the Glacier Monument, Cathedral Peak, Cathedral Spires, Unicorn Peak, and their many nameless .companions rising in. grand beauty 1 above a\u27noble swath of forest that-is growing on the left lateral moraine of the ancient Tuol umne Glacier, which, broad and deep and far- reaching, exerted vast influence on the scenery of this portion of the Sierra. But there are fine camping-grounds all along the meadows, and one may move from grove to grove every day y all summer enjoying-fresh home) and- fetch?-4-1 c (\u27,y\u27 ing enough to satisfy every roving desire for \u27 -s \u27 \u27\u27 change. vL-U tf iZ, There are four capital excursions to be iyt \u27 made from here — to the summits of Muts Dana and Lyell f to Mono Lake and the vol- jQtfHu\u27 * ). canoes, tnrougn Bloody Canon; and to the v great Tuolumne Canon as far as the foot of the / &-: • iJllll W\u27e\u27 SBPIltBiilllil I\u27L\u27OI.L\u27.MNIi MKADuWS, LUOICING SOUTH. UN ICC EAK AND CATHEDRAL PEAK. Vol.. XL. —87. 032.&3 658 FEATURES OF THE PROPOSED YOSEMITE NATIONAL PARK/ FEATURES OF THE PROPOSED YOSEMITE NATIONAL PARK. 659 LYELL GLACIER, FROM THE EDGE OF THE GREAT FISSURE. \\u27 foam. To the south of the lake there is a range of pale-gray volcanoes, now extinct, and though the highest of them rise;) nearly two thousand feet above the lake, you can look down into their well-defined circular, cup-like craters, from which, a comparatively short time ago, ashes and cinders were showered over the 66o FEATURES OF THE PROPOSED YOSEMITE NATIONAL PARK. THE SOUTH SIDE OF MOUNT LYELL. Dana, Warren, Conness, and -many others, unnumbered and unnamed; to the southeast the indescribably wild and jagged range of Mount Ritter and the Minarets; southwest- ward stretches the dividing ridge between the North Fork of the San Joaquin and the Merced, uniting with the Obelisk or Merced group of peaks that form the main fountains of the Illilouette branch of the Merced River; and to the northwestward extends the Cathedral spur. Alkjhese spurs, like distinct: ranges, meet at your feet,\u27 Therefore you look over-. them mostly in the direction of their extension, and their peaks seem to be massed and crowded together in bewildering combinations fVhile immense amphitheaters, canons, and subordi- I FEATURES OF THE PROPOSED YOSEMITE NATIONAL PARK. 661 f- f. TUOLUMNE RIVER NEAR THE HEAD OF THE GREAT CANON. nate masses, with their wealth of lakes, glaciers, and snow-fields, maze and cluster between them. In making the ascent in June or October the glacier is easily crossed, for then its snow mantle is smooth or mostly melted off. But in midsummer the climbing is exceedingly tedious, because the snow is then weathered into curious and beautiful blades, sharp and slender, and set on edge in aleaning position. They lean towards the head of the glacier, and extend across from side to side in regular order in a direction at right angles to the direction of greatest declivity, the distance between the crests be-* ing about two or three feet, and the depth of the troughs between them about three feet. . Ne more interesting problem\u27s ever presented to the mountaineer; than a walk over a glacier The Lyell Glacier is about a mile wide and less than a mile long, but presents, nevertheless, all the more characteristic features of large, river-like glaciers -— moraines, earth-bands, blue-veins, crevasses, etc., while the streams that issue from it are turbid with rock-mud, showing its grinding action on its bed. And it is all the more interesting since it is the highest and most enduring remnant of the great. Tuolumne Glacier, whose traces are still distinct fifty miles away, and whose influence on the landscape was so profound. The McClure Glacier, once a .tributary of the Lyell, is much smaller. •Eighteen years ago I set a series of stakes in it to determine its rate of motion, which towards the end of summer, in.the , middle of the glacier, I found to-Tiela little Vfc- thus sculptured and adorned. . over an inch in twenty-four hours. I The trip to Monfrom the Soda Springs \ *can be made in a/tfaybwt-Bloocly Canon.yttI be found rough foKanimals. The Scenery of vtlie canon, however, is wild, and rich; aii4 many Slays may profitably be spent around the shores of the lake and Out on its islands and about the volcanoes. \ ft i, \ y&t \u27V? 2-i.eaA-\u27--\u27 f #3.27.3 662 FEATURES OF THE PROPOSED YOSEMITE NATIONAL PARK. i_ JvV52 ENTRANCE TO HETCH HETCHY VALLEY FROM SMITH TRAIL. In making the trip clown the Big Tuolumne Canon animals may be led as far as a small, grassy, forested lake basin that lies below the crossing of the Virginia Creek trail. And from this point any one accustomed to walk on earthquake boulders, carpeted with canon chaparral, can easily go clown tlie.xaiioB\u27 as far as the big cascades and return to camp in one da}\u27. Many, however, are not able to do this, and it is far better to go leisurely, prepared to camp anywhere, and enjoy the marvelous grandeur of the place. The canon begins near the lower end of the meadows and extends to the Pletch Hetchy Valley, a distance of about eighteen miles, though it will seem much longer to any one who scrambles through it. It is from 1200 to about 5000 feet deep, and is comparatively narrow, but there are several fine, roomy, park-like openings in it, and throughout its LOOKING DOWN ON LAKE TENAYA. FEATURES OF THE PROPOSED YOSEMITE NATIONAL PARK. 663 VIEW OF A PART OF THE GRAND ,0- whole extent Yosemite features are displayed on a grand scale — domes, El Capitan rocks, gables, Sentinels, Royal Arches, glacier points, Cathedral Spires, etc. There is even a Half Dome among its wealth of rock forms, though less sublime and beautiful than the Yosemite Half Dome. It-jalso contains- falls and cas- (joi&. cades innumerable. The sheer falls, except when the snow is melting in early spring, are quite small in volume as compared with those of Yosemite and Hetch Hetchy; but many of them are. .very beautiful,-and\u27 in any other country would be regarded as great wonders. But it is the cascades or sloping falls on the main river that are the crowning glory of the canon, and these in volume, extent, and variety surpass those of any other cation in the Sierra. The most showy and interesting of the cascades are mostly in the upper part of the canon, above the point where Cathedral Creek and Hoffman Creek enter. CASCADES, BIG TUOLUMNE CANON. For miles the riveris one wild, exulting, on-rushing mass of snowy purple bloom, spreading over glacial; waves of granite without any definite channel, and through avalanche taluses-, gliding inLsilver plumes, clashing and foaming through huge boulder-dams, leaping high into the air in glorious wheel-like whirls, tossing from side to side, doubling, glinting, singing in glorious exuberance of mountain energy. Every one who is anything of a mountaineer should go on through the entire length of the canon, coming out by Hetch Hetchy. There is not a dull step all the way. With wide variations it is a Yosemite Valley from end to end. THE HETCH HETCHY VALLEY. Most people who visit Yosemite are apt to regard it as an exceptional creation, the only valley of its kind in\u27the world. But nothing in Nature stands alone.. She is not so poor as 030.53- 664 FEATURES OF THE PROPOSED YOSEMITE NATIONAL PARK. KOLANA ROCK, HETCH HETCHY VALLEY. to have only one of anything. The explorer in the Sierra and elsewhere finds many Yosem- ites, that differ not more than one tree differs from another of the same species. They occupy the same relative positions on the mountain flanks, were formed by the same forces in the same kind of granite, and have similar sculpture, waterfalls, and vegetation. The Hetch Hetchy Valley has long been known as the Tuolumne Yosemite. It is said to have been discovered by Joseph Screech, a hunter, in 1850, a year before the discovery of the great Merced Yosemite. It lies in a northwesterly direction from Yosemite, at a. distance of about twenty miles, and is easily accessible to mounted travelers by a trail that leaves the Big Oak Flat road at Bronson\u27s Meadows, a few miles below Crane Flat. But by far the best way to it for those who have useful limbs is across the divide direct from Yosemite. Leaving the valley by Indian Cation or Fall Canon, you cross the dome-paved basin of Yosemite Creek, then bear to the left around the head fountains of the South Fork of the Tuolumne to the summit of the Big Tuolumne Canon, a few miles above the head of Hetch Hetchy. Here you will find a glorious view. Immediately beneath you, at a depth of more than 4000 feet, you see a beautiful ribbon of level ground, with a silver thread in the middle of it, and green or yellow according to the time of year. That ribbon is a strip of meadow, and the silver thread is the main Tuolumne River. The opposite wall of the canon rises in precipices, steep and angular, or with rounded brows like those of Yosemite, and from this wall as abase extends a fine wilderness of mountains, rising dome above dome, ridge above ridge, to a group of snowy peaks on the summit of the range. Of all this sublime congregation of mountains Castle Peak is king: robed with snow and light, clipping unnumbered points and spires into the thin blue sky, it maintains amid noble companions a perfect and commanding individuality. You will not encounter much difficulty in getting down into the canon, for bear trails may readily be found leading from the upper feeding-grounds to the berry gardens and acorn orchards of Hetch Hetchy, and when you reach the river you have only to saunter by its side a mile or two down the canon before FEATURES OF THE PROPOSED YOSEMITE NATIONAL PARK. 665 V you find yourself in the open valley. Looking about you, you cannot fail to discover that you are in a Yosemite valley. As the Merced flows through Yosemite, so does the Tuolumne through Hetch Hetchy. The bottom of Yosemite is about 4000 feet above sea level, the bottom of Hetch Hetchy is about 3800 feet, and in both the walls are of gray granite and rise abruptly in precipices from a level bottom, with but little debris along their bases. Furthermore it was a home and stronghold of the Tuolumne Indians, as Ahwahne was of the grizzlies. Standing boldly forward from the south wall near the lower end of the valley is the rock Kolana, the outermost of a picturesque group corresponding to the Cathedral Rocks of Yosemite, and about the same height. Facing Kolana on the north side of the valley- is a rock about 1800 feet in height, which presents a bare, sheer front like El Capitan, and over its massive brow flows a stream that makes the most graceful fall I have ever seen. Its Indian name is Tu-ee-u-la-la, and no other, so far as I have heard, has yet been given it. From the brow of the cliff it makes a free descent of a thousand feet and then breaks up into a ragged, foaming web of cascades among the boulders of an earthquake talus. Towards the end of summer it vanishes, because its head streams do not reach back to the lasting snows of the summits of the range, but in May and June it is indescribably lovely. The only fall that I know with which it may fairly be compared is the Bridal Veil, but it excels even that fall in peaceful, floating, swaying gracefulness. For when we attentively observe the Bridal Veil, even towards the middle of summer when its waters begin to fail, we may discover, when the winds blow aside the outer folds of spray, dense comet-shaped masses shooting through the air with terrible energy; but from the top of the cliff, where the Hetch Hetchy veil first floats free, all the way to the bottom it is in perfect repose. Again, the Bridal Veil is in a shadow-haunted nook inaccessible to the main wind currents of the valley, and has to depend for many of its gestures on irregular, teasing side currents and whirls, while Tu-ee-u-la-la, being fully exposed on the open cliff, is sun\u27 drenched all day, and is ever ready to yield graceful compliance to every wind that blows. Most people unacquainted with the behavior of mountain streams fancy that when they escape the bounds of their rocky channels and launch into the air they at once lose all self-control and tumble in confusion. On the contrary, m no part of their travels do they manifest more calm self-possession. Imagine yourself in Hetch Hetchy. It is a sunny day in June, the pines sway dreamily, and you are shoulder- deep in grass and flowers. Looking across the Vol. XL.—88. valley through beautiful open groves you see a bare granite wall 1800 feet high rising abruptly out of the green and yellow vegetation and glowing with sunshine, and in front of it the fall, waving like a downy scarf, silver bright, burning with white sun-fire in every fiber. In coming forward to the edge of the tremendous precipice and taking flight a little hasty eagerness appears, but this is speedily hushed in divine repose. Now observe the marvelous distinctness and delicacy of the various kinds of sun-filled tissue into which the waters are woven. They fly and float and drowse down the face of that grand gray rock in so leisurely and unconfused a manner that you may examine their texture and patterns as you would a piece of embroidery held in the hand. It is a flood of singing air, water, and sunlight woven into cloth that spirits might wear. The great Hetch Hetchy Fall, called Wa- pama by the Tuolumnes, is on the same side of the valley as the Veil, and so near it that both may be seen in one view. It is about 1800 feet in height, and seems to be nearly vertical when one is standing in front of it, though it is considerably inclined. Its location is similar to that of -the Yosemite Fall, but the volume of water is much greater. No two falls could be more unlike than Wa-pama and Tu-ee-u-la-la, the one thundering and beating in a shadowy gorge, the other chanting in deep, low tones, and with no other shadows about it than those of its own waters, pale- gray mostly, and violet and pink delicately graded. One whispers, He dwells in peace the other is the thunder of his chariot wheels in power. This noble pair are the main falls of the valley, though there are many small ones essential to the perfection of the general harmony. The wall above Wa-pama corresponds, both in outlines and in details of sculpture, with the same relative portion of the Yosemite wall. Near the Yosemite Fall the cliff has two conspicuous benches extending in a horizontal direction 500 and 1500 feet above the valley. Two benches similarly situated, and timbered in the same way, occur on the same relative position on the Hetch Hetchy wall, and on no other portion. The upper end of Yosemite is closed by the great Half Dome, and the upper end of Hetch Hetchy is closed in the same way by a mountain rock. Both occupy angles formed by the confluence of two large glaciers that have long since vanished. In front of this head rock the river forks like the Merced in Yosemite. The right fork as you ascend is the main Tuolumne, which takes its rise in a glacier on the north side of Mount Lyell and flows through the Big 666 FEATURES OF THE PROPOSED YOSEMITE NATIONAL PARK. BOUNDARY 3° OF _ Y OS EM J T E NIX tToNA L _ PA ff K %±jL,. tTjll t// *ou J7wv- ,0\u27~/ \u27. / ~ \u27 y P nOPOSEO\u27 BOUNDARY \u27o\u27f V YOSEMITE \ ?0 j/AJVgVj. PARK 10/!„,„f MAP OF THE YOSEMITE REGION, SHOWING PRESENT RESERVATION, WATER-SHED OF THE VALLEY, AND APPROXIMATE LIMITS OF THE PROPOSED NATIONAL PARK.1 Canon. I have not traced the left fork to its highest source, but, judging from the general trend of the ridges, it must be near Castle Peak. Upon this left or North Fork there is a remarkably interesting series of cascades, five in number, ranged along a picturesque gorge, on the edges of which we may saunter safely and gain fine views of the dancing spray below. The first is a wide-spreading fan of white, crystal-covered water, half leaping half sliding over a steep polished pavement, at the foot of which it rests and sets forth clear and shining on its final flow to the main river. A short distance above the head of this cascade you discover the second, which is as impressively wild and beautiful as the first, and makes you sing with it as though you were a part of it. It is framed in deep rock walls that are colored yellow and red with lichens, and fringed on the jagged edges by live-oaks and sabine pines, and at the bottom in damp nooks you may see ferns, lilies, and azaleas. Three or four hundred yards higher you come to the third of the choir, the largest of the five. It is formed of three smaller ones inseparably combined, which sing divinely, and make s