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If I were so time-poor as to have only one day to spend in Yosemite I should start at daybreak, say at three o’clock in midsummer, with a pocketful of any sort of dry breakfast stuff, for Glacier Point, Sentinel Dome, the head of Illilouette Fall, Nevada Fall, the top of Liberty Cap, Vernal Fall and the wild boulder-choked River Cañon. The trail leaves the Valley at the base of the Sentinel Rock, and as you slowly saunter from point to point along its many accommodating zigzags nearly all the Valley rocks and falls are seen in striking, ever-changing combinations. At an elevation of about five hundred feet a particularly fine, wide-sweeping view down the Valley is obtained, past the sheer face of the Sentinel and between the Cathedral Rocks and El Capitan. At a height of about 1500 feet the great Half Dome comes full in sight, overshadowing every other feature of the Valley to the eastward. From Glacier Point you look down 3000 feet over the edge of its sheer face to the meadows and groves and innumerable yellow pine spires, with the meandering river sparkling and spangling through the midst of them. Across the Valley a great telling view is presented of the Royal Arches, North Dome, Indian Cañon, Three Brothers and El Capitan, with the dome-paved basin of Yosemite Creek and Mount Hoffman in the background. To the eastward, the Half Dome close beside you looking higher and more wonderful than ever; southeastward the Starr King, girdled with silver firs, and the spacious garden-like basin of the Illilouette and its deeply sculptured fountain-peaks, called “The Merced Group”; and beyond all, marshaled along the eastern horizon, the icy summits on the axis of the Range and broad swaths of forests growing on ancient moraines, while the Nevada, Vernal and Yosemite Falls are not only full in sight but are distinctly heard as if one were standing beside them in their spray.
The views from the summit of Sentinel Dome are still more extensive and telling. Eastward the crowds of peaks at the head of the Merced, Tuolumne and San Joaquin Rivers are presented in bewildering array; westward, the vast forests, yellow foothills and the broad San Joaquin plains and the Coast Ranges, hazy and dim in the distance.
From Glacier Point go down the trail into the lower end of the Illilouette basin, cross Illilouette Creek and follow it to the Fall where from an outjutting rock at its head you will get a fine view of its rejoicing waters and wild cañon and the Half Dome. Thence returning to the trail, follow it to the head of the Nevada Fall. Linger here an hour or two, for not only have you glorious views of the wonderful fall, but of its wild, leaping, exulting rapids and, greater than all, the stupendous scenery into the heart of which the white passionate river goes wildly thundering, surpassing everything of its kind in the world. After an unmeasured hour or so of this glory, all your body aglow, nerve currents flashing through you never before felt, go to the top of the Liberty Cap, only a glad saunter now that your legs as well as head and heart are awake and rejoicing with everything. The Liberty Cap, a companion of the Half Dome, is sheer and inaccessible on three of its sides but on the east a gentle, ice-burnished, juniper-dotted slope extends to the summit where other wonderful views are displayed where all are wonderful: the south side and shoulders of Half Dome and Clouds’ Rest, the beautiful Little Yosemite Valley and its many domes, the Starr King cluster of domes, Sentinel Dome, Glacier Point, and, perhaps the most tremendously impressive of all, the views of the hopper-shaped cañon of the river from the head of the Nevada Fall to the head of the Valley.
Returning to the trail you descend between the Nevada Fall and the Liberty Cap with fine side views of both the fall and the rock, pass on through clouds of spray and along the rapids to the lead of the Vernal Fall, about a mile below the Nevada. Linger here if night is still distant, for views of this favorite fall and the stupendous rock scenery about it. Then descend a stairway by its side, follow a dim trail through its spray, and a plain one along the border of the boulder-dashed rapids and so back to the wide, tranquil Valley.
Another grand one-day excursion is to the Upper Yosemite Fall, the top of the highest of the Three Brothers, called Eagle Peak on the Geological Survey maps; the brow of El Capitan; the head of the Ribbon Fall; across the beautiful Ribbon Creek Basin; and back to the Valley by the Big Oak Flat wagon-road.
The trail leaves the Valley on the east side of the largest of the earthquake taluses immediately opposite the Sentinel Rock and as it passes within a few rods of the foot of the great fall, magnificent views are obtained as you approach it and pass through its spray, though when the snow is melting fast you will be well drenched. From the foot of the Fall the trail zigzags up a narrow cañon between the fall and a plain mural cliff that is burnished here and there by glacial action.
You should stop a while on a flat iron-fenced rock a little below the head of the fall beside the enthusiastic throng of starry comet-like waters to learn something of their strength, their marvelous variety of forms, and above all, their glorious music, gathered and composed from the snow-storms, hail-, rain- and wind-storms that have fallen on their glacier-sculptured, domey, ridgy basin. Refreshed and exhilarated, you follow your trail-way through silver fir and pine woods to Eagle Peak, where the most comprehensive of all the views to be had on the north-wall heights are displayed. After an hour or two of gazing, dreaming, studying the tremendous topography, etc., trace the rim of the Valley to the grand El Capitan ridge and go down to its brow, where you will gain everlasting impressions of Nature’s steadfastness and power combined with ineffable fineness of beauty.
Dragging yourself away, go to the head of the Ribbon Fall, thence across the beautiful Ribbon Creek Basin to the Big Oak Flat stage-road, and down its fine grades to the Valley, enjoying glorious Yosemite scenery all the way to the foot of El Capitan and your camp.
For a two-day trip I would go straight to Mount Hoffman, spend the night on the summit, next morning go down by May Lake to Tenaya Lake and return to the Valley by Cloud’s Rest and the Nevada and Vernal Falls. As on the foregoing excursion, you leave the Valley by the Yosemite Falls trail and follow it to the Tioga wagon-road, a short distance east of Porcupine Flat. From that point push straight up to the summit. Mount Hoffman is a mass of gray granite that rises almost in the center of the Yosemite Park, about eight or ten miles in a straight line from the Valley. Its southern slopes are low and easily climbed, and adorned here and there with castle-like crumbling piles and long jagged crests that look like artificial masonry; but on the north side it is abruptly precipitous and banked with lasting snow. Most of the broad summit is comparatively level and thick sown with crystals, quartz, mica, hornblende, feldspar, granite, zircon, tourmaline, etc., weathered out and strewn closely and loosely as if they had been sown broadcast. Their radiance is fairly dazzling in sunlight, almost hiding the multitude of small flowers that grow among them. At first sight only these radiant crystals are likely to be noticed, but looking closely you discover a multitude of very small gilias, phloxes, mimulus, etc., many of them with more petals than leaves. On the borders of little streams larger plants flourish—lupines, daisies, asters, goldenrods, hairbell, mountain columbine, potentilla, astragalus and a few gentians; with charming heathworts—bryanthus, cassiope, kalmia, vaccinium in boulder-fringing rings or bank covers. You saunter among the crystals and flowers as if you were walking among stars. From the summit nearly all the Yosemite Park is displayed like a map: forests, lakes, meadows, and snowy peaks. Northward lies Yosemite’s wide basin with its domes and small lakes, shining like larger crystals; eastward the rocky, meadowy Tuolumne region, bounded by its snowy peaks in glorious array; southward Yosemite and westward the vast forest. On no other Yosemite Park mountain are you more likely to linger. You will find it a magnificent sky camp. Clumps of dwarf pine and mountain hemlock will furnish resin roots and branches for fuel and light, and the rills, sparkling water. Thousands of the little plant people will gaze at your camp-fire with the crystals and stars, companions and guardians as you lie at rest in the heart of the vast serene night.
The most telling of all the wide Hoffman views is the basin of the Tuolumne with its meadows, forests and hundreds of smooth rock-waves that appear to be coming rolling on towards you like high heaving waves ready to break, and beyond these the great mountains. But best of all are the dawn and the sunrise. No mountain top could be better placed for this most glorious of mountain views—to watch and see the deepening colors of the dawn and the sunbeams streaming through the snowy High Sierra passes, awakening the lakes and crystals, the chilled plant people and winged people, and making everything shine and sing in pure glory.
With your heart aglow, spangling Lake Tenaya and Lake May will beckon you away for walks on their ice-burnished shores. Leave Tenaya at the west end, cross to the south side of the outlet, find gradually work your way up in an almost straight south direction to the summit of the divide between Tenaya Creek and the main upper Merced River or Nevada Creek and follow the divide to Clouds Rest. After a glorious view from the crest of this lofty granite wave you will find a trail on its western end that will lead you down past Nevada and Vernal Falls to the Valley in good time, provided you left your Hoffman sky camp early.
Another grand two-day excursion is the same as the first of the one-day trips, as far as the head of Illilouette Fall. From there trace the beautiful stream up through the heart of its magnificent forests and gardens to the cañons between the Red and Merced Peaks, and pass the night where I camped forty-one years ago. Early next morning visit the small glacier on the north side of Merced Peak, the first of the sixty-five that I discovered in the Sierra.
Glacial phenomena in the Illilouette Basin are on the grandest scale, and in the course of my explorations I found that the cañon and moraines between the Merced and Red Mountains were the most interesting of them all. The path of the vanished glacier shone in many places as if washed with silver, and pushing up the cañon on this bright road I passed lake after lake in solid basins of granite and many a meadow along the cañon stream that links them together. The main lateral moraines that bound the view below the cañon are from a hundred to nearly two hundred feet high and wonderfully regular, like artificial embankments covered with a magnificent growth of silver fir and pine. But this garden and forest luxuriance is speedily left behind, and patches of bryanthus, cassiope and arctic willows begin to appear. The small lakes which a few miles down the Valley are so richly bordered with flowery meadows have at an elevation of 10,000 feet only small brown mats of carex, leaving bare rocks around more than half their shores. Yet, strange to say, amid all this arctic repression the mountain pine on ledges and buttresses of Red Mountain seems to find the climate best suited to it. Some specimens that I measured were over a hundred feet high and twenty-four feet in circumference, showing hardly a trace of severe storms, looking as fresh and vigorous as the giants of the lower zones. Evening came on just as I got fairly into the main cañon. It is about a mile wide and a little less than two miles long. The crumbling spurs of Red Mountain bound it on the north, the somber cliffs of Merced Mountain on the south and a deeply-serrated, splintered ridge curving around from mountain to mountain shuts it in on the east. My camp was on the brink of one of the lakes in a thicket of mountain hemlock, partly sheltered from the wind. Early next morning I set out to trace the ancient glacier to its head. Passing around the north shore of my camp lake I followed the main stream from one lakelet to another. The dwarf pines and hemlocks disappeared and the stream was bordered with icicles. The main lateral moraines that extend from the mouth of the cañon are continued in straggling masses along the walls. Tracing the streams back to the highest of its little lakes, I noticed a deposit of fine gray mud, something like the mud corn from a grindstone. This suggested its glacial origin, for the stream that was carrying it issued from a raw-looking moraine that seemed to be in process of formation. It is from sixty to over a hundred feet high in front, with a slope of about thirty-eight degrees. Climbing to the top of it, I discovered a very small but well-characterized glacier swooping down from the shadowy cliffs of the mountain to its terminal moraine. The ice appeared on all the lower portion of the glacier; farther up it was covered with snow. The uppermost crevasse or “bergeschrund” was from twelve to fourteen feet wide. The melting snow and ice formed a network of rills that ran gracefully down the surface of the glacier, merrily singing in their shining channels. After this discovery I made excursions over all the High Sierra and discovered that what at first sight looked like snowfields were in great part glaciers which were completing the sculpture of the summit peaks.
Rising early,—which will be easy, as your bed will be rather cold and you will not be able to sleep much anyhow,—after visiting the glacier, climb the Red Mountain and enjoy the magnificent views from the summit. I counted forty lakes from one standpoint an this mountain, and the views to the westward over the Illilouette Basin, the most superbly forested of all the basins whose waters rain into Yosemite, and those of the Yosemite rocks, especially the Half Dome and the upper part of the north wall, are very fine. But, of course, far the most imposing view is the vast array of snowy peaks along the axis of the Range. Then from the top of this peak, light and free and exhilarated with mountain air and mountain beauty, you should run lightly down the northern slope of the mountain, descend the cañon between Red and Gray Mountains, thence northward along the bases of Gray Mountain and Mount Clark and go down into the head of Little Yosemite, and thence down past the Nevada and Vernal Falls to the Valley, a truly glorious two-day trip!
The best three-day excursion, as far as I can see, is the same as the first of the two-day trips until you reach Lake Tenaya. There instead of returning to the Valley, follow the Tioga road around the northwest side of the lake, over to the Tuolumne Meadows and up to the west base of Mount Dana. Leave the road there and make straight for the highest point on the timber line between Mounts Dana and Gibbs and camp there.
On the morning of the third day go to the top of Mount Dana in time for the glory of the dawn and the sunrise over the gray Mono Desert and the sublime forest of High Sierra peaks. When you leave the mountain go far enough down the north side for a view of the Dana Glacier, then make your way back to the Tioga road, follow it along the Tuolumne Meadows to the crossing of Budd Creek where you will find the Sunrise trail branching off up the mountain-side through the forest in a southwesterly direction past the west side of Cathedral Peak, which will lead you down to the Valley by the Vernal and Nevada Falls. If you are a good walker you can leave the trail where it begins to descend a steep slope in the silver fir woods, and bear off to the right and make straight for the top of Clouds’ Rest. The walking is good and almost level and from the west end of Clouds’ Rest take the Clouds’ Rest Trail which will lead direct to the Valley by the Nevada and Vernal Falls. To any one not desperately time-poor this trip should have four days instead of three; camping the second night at the Soda Springs; thence to Mount Dana and return to the Soda Springs, camping the third night there; thence by the Sunrise trail to Cathedral Peak, visiting the beautiful Cathedral lake which lies about a mile to the rest of Cathedral Peak, eating your luncheon, and thence to Clouds’ Rest and the Valley as above. This is one of the most interesting of all the comparatively short trips that can be made in the whole Yosemite region. Not only do you see all the grandest of the Yosemite rocks and waterfalls and the High Sierra with their glaciers, glacier lakes and glacier meadows, etc., but sections of the magnificent silver fir, two-leaved pine, and dwarf pine zones; with the principal alpine flowers and shrubs, especially sods of dwarf vaccinium covered with flowers and fruit though less than an inch high, broad mats of dwarf willow scarce an inch high with catkins that rise straight from the ground, and glorious beds of blue gentians,—grandeur enough and beauty enough for a lifetime.
We come now to the grandest of all the Yosemite excursions, one that requires at least two or three weeks. The best time to make it is from about the middle of July. The visitor entering the Yosemite in July has the advantage of seeing the falls not, perhaps, in their very flood prime but next thing to it; while the glacier-meadows will be in their glory and the snow on the mountains will be firm enough to make climbing safe. Long ago I made these Sierra trips, carrying only a sackful of bread with a little tea and sugar and was thus independent and free, but now that trails or carriage roads lead out of the Valley in almost every direction it is easy to take a pack animal, so that the luxury of a blanket and a supply of food can easily be had.
The best way to leave the Valley will be by the Yosemite Fall trail, camping the first night on the Tioga road opposite the east end of the Hoffman Range. Next morning climb Mount Hoffman; thence push on past Tenaya Lake into the Tuolumne Meadows and establish a central camp near the Soda Springs, from which glorious excursions can be made at your leisure. For here in this 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 a fairly good carriage road that passes between Yosemite and Mount Hoffman, it is also the most accessible. It is in the heart of the High Sierra east of Yosemite, 8500 to 9000 feet above the level of the sea. The gray, picturesque Cathedral Range bounds it on the south; a similar range or spur, the highest peak of which is Mount Conness, on the north; the noble Mounts Dana, Gibbs, Mammoth, Lyell, McClure and others on the axis of the Range on the east; a heaving, billowing crowd of glacier-polished rocks and Mount Hoffman on the west. Down through the open sunny meadow-levels of the Valley flows the Tuolumne River, fresh and cool from its many glacial fountains, the highest of which are the glaciers that lie on the north sides of Mount Lyell and Mount McClure.
Along the river a series of beautiful glacier-meadows extend with but little interruption, from the lower end of the Valley to its head, a distance of about twelve miles, forming charming sauntering-grounds from which the glorious mountains may be enjoyed as they look down in divine serenity over the dark forests 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 moraine boulders and dead trees brought down from the heights by snow 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 meadows is about four miles long and from a quarter to 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, 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 weeds and bushes; while charming flowers abound, especially gentians, dwarf daisies, potentillas, 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 stream banks and around boulders. The principal grass of these meadows is a delicate calamagrostis with very slender filiform leaves, and when it is in flower the ground seems to be covered with a faint purple mist, the stems of the panicles 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 are frosty, and then the meadows at sunrise, when every leaf is laden with crystals, are a fine sight. The days are still warm and calm, and bees and butterflies continue to waver and hum about the late-blooming flowers until the coming of the snow, usually in November. Storm then follows storm in quick 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 usually lasts until the end of June but the new season’s vegetation is not generally in bloom until late in July. Perhaps the best all round excursion-time after winters of average snowfall is from the middle of July to the middle or end of August. The snow is then melted from the woods and southern slopes of the mountains and the meadows and gardens are in their glory, while the weather is mostly all-reviving, exhilarating sunshine. The few clouds that rise now and then and the showers they yield are only enough to keep everything fresh and fragrant.
The groves about the Soda Springs are favorite camping-grounds on account of the cold, pleasant-tasting water charged with carbonic acid, and because of the views of the mountains across the meadow—the Glacier Monument, Cathedral Peak, Cathedral Spires, Unicorn Peak and a series of ornamental nameless companions, rising in striking forms and nearness above a dense forest growing on the left lateral moraine of the ancient Tuolumne glacier, which, broad, 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 all summer, enjoying new homes and new beauty to satisfy every roving desire for change.
There are five main capital excursions to be made from here—to the summits of Mounts Dana, Lyell and Conness, and through the Bloody Cañon Pass to Mono Lake and the volcanoes, and down the Tuolumne Cañon, at least as far as the foot of the wonderful series of river cataracts. All of these excursions are sure to be made memorable with joyful health-giving experiences; but perhaps none of them will be remembered with keener delight than the days spent in sauntering on the broad velvet lawns by the river, sharing the sky with the mountains and trees, gaining something of their strength and peace.
The excursion to the top of Mount Dana is a very easy one; for though the mountain is 13,000 feet high, the ascent from the west side is so gentle and smooth that one may ride a mule to the very summit. Across many a busy stream, from meadow to meadow, lies your flowery way; mountains all about you, few of them hidden by irregular foregrounds. Gradually ascending, other mountains come in sight, peak rising above peak with their snow and ice in endless variety of grouping and sculpture. Now your attention is turned to the moraines, sweeping in beautiful curves from the hollows and cañons, now to the granite waves and pavements rising here and there above the heathy sod, polished a thousand years ago and still shining. Towards the base of the mountain you note the dwarfing of the trees, until at a height of about 11,000 feet you find patches of the tough, white-barked pine, pressed so flat by the ten or twenty feet of snow piled upon them every winter for centuries that you may walk over them as if walking on a shaggy rug. And, if curious about such things, you may discover specimens of this hardy tree-mountaineer not more than four feet high and about as many inches in diameter at the ground, that are from two hundred to four hundred years old, still holding bravely to life, making the most of their slender summers, shaking their tasseled needles in the breeze right cheerily, drinking the thin sunshine and maturing their fine purple cones as if they meant to live forever. The general view from the summit is one of the most extensive and sublime to be found in all the Range. To the eastward you gaze far out over the desert plains and mountains of the “Great Basin,” range beyond range extending with soft outlines, blue and purple in the distance. More than six thousand feet below you lies Lake Mono, ten miles in diameter from north to south, and fourteen from west to east, lying bare in the treeless desert like a disk of burnished metal, though at times it is swept by mountain storm winds and streaked with foam. To the southward there is a well defined range of pale-gray extinct volcanoes, and though the highest of them rises nearly two thousand feet above the lake, you can look down from here into their circular, cup-like craters, from which a comparatively short time ago ashes and cinders were showered over the surrounding sage plains and glacier-laden mountains.
To the westward the landscape is made up of exceedingly strong, gray, glaciated domes and ridge waves, most of them comparatively low, but the largest high enough to be called mountains; separated by cañons and darkened with lines and fields of forest, Cathedral Peak and Mount Hoffman in the distance; small lakes and innumerable meadows in the foreground. Northward and southward the great snowy mountains, marshaled along the axis of the Range, are seen in all their glory, crowded together in some places like trees in groves, making landscapes of wild, extravagant, bewildering magnificence, yet calm and silent as the sky.
Some eight glaciers are in sight. One of these is the Dana Glacier on the north side of the mountain, lying at the foot of a precipice about a thousand feet high, with a lovely pale-green lake a little below it. This is one of the many, small, shrunken remnants of the vast glacial system of the Sierra that once filled the hollows and valleys of the mountains and covered all the lower ridges below the immediate summit-fountains, flowing to right and left away from the axis of the Range, lavishly fed by the snows of the glacial period.
In the excursion to Mount Lyell the immediate base of the mountain is easily reached on meadow walks along the river. Turning to the southward above the forks of the river, you enter the narrow Lyell branch of the Valley, narrow enough and deep enough to be called a cañon. It is about eight miles long and from 2000 to 3000 feet deep. The flat meadow bottom is from about three hundred to two hundred yards wide, with gently curved margins about fifty yards wide from which rise the simple massive walls of gray granite at an angle of about thirty-three degrees, mostly timbered with a light growth of pine and streaked in many places with avalanche channels. Towards the upper end of the cañon the Sierra crown comes in sight, forming a finely balanced picture framed by the massive cañon walls. In the foreground, when the grass is in flower, you have the purple meadow willow-thickets on the river banks; in the middle distance huge swelling bosses of granite that form the base of the general mass of the mountain, with fringing lines of dark woods marking the lower curves, smoothly snow-clad except in the autumn.
If you wish to spend two days on the Lyell trip you will find a good camp-ground on the east side of the river, about a mile above a fine cascade that comes down over the cañon wall in telling style and makes good camp music. From here to the top of the mountains is usually an easy day’s work. At one place near the summit careful climbing is necessary, but it is not so dangerous or difficult as to deter any one of ordinary skill, while the views are glorious. To the northward are Mammoth Mountain, Mounts Gibbs, Dana, Warren, Conness and others, unnumbered and unnamed; to the southeast the indescribably wild and jagged range of Mount Ritter and the Minarets; southwestward 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; and to the north-westward extends the Cathedral spur. These spurs like distinct ranges meet at your feet; therefore you look at them mostly in the direction of their extension, and their peaks seem to be massed and crowded against one another, while immense amphitheaters, cañons and subordinate ridges 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 a leaning 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 being about two or three feet, and the depth of the troughs between them about three feet. A more interesting problem than a walk over a glacier thus sculptured and adorned is seldom presented to the mountaineer.
The Lyell Glacier is about a mile wide and less than a mile long, but presents, nevertheless, all the essential characters of large, river-like glaciers—moraines, earth-bands, blue veins, crevasses, etc., while the streams that issue from it are, of course, 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 smaller. Thirty-eight years ago I set a series of stakes in it to determine its rate of motion. Towards the end of summer in the middle of the glacier it was only a little over an inch in twenty-four hours.
The trip to Mono from the Soda Springs can be made in a day, but many days may profitably be spent near the shores of the lake, out on its islands and about the volcanoes.
In making the trip down the Big Tuolumne Cañon, 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 walking on earthquake boulders, carpeted with cañon chaparral, can easily go down as far as the big cascades and return to camp in one day. Many, however, are not able to do his, and it is better to go leisurely, prepared to camp anywhere, and enjoy the marvelous grandeur of the place.
The cañon begins near the lower end of the meadows and extends to the Hetch Hetchy Valley, a distance of about eighteen miles, though it will seem much longer to any one who scrambles through it. It is from twelve hundred to about five thousand feet deep, and is comparatively narrow, but there are several roomy, park-like openings in it, and throughout its whole extent Yosemite natures 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 far less sublime than the Yosemite Half Dome. Its falls and cascades are 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; though in any other country many of them would be regarded as wonders. But it is the cascades or sloping falls on the main river that are the crowning glory of the cañon, and these in volume, extent and variety surpass those of any other cañon in the Sierra. The most showy and interesting of them are mostly in the upper part of the cañon, above the point of entrance of Cathedral Creek and Hoffman Creek. For miles the river is one wild, exulting, on-rushing mass of snowy purple bloom, spreading over glacial waves of granite without any definite channel, gliding in magnificent silver plumes, dashing and foaming through huge boulder-dams, leaping high into the air in wheel-like whirls, displaying glorious enthusiasm, tossing from side to side, doubling, glinting, singing in exuberance of mountain energy.
Every one who is anything of a mountaineer should go on through the entire length of the cañon, 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.
Besides these main, far-reaching, much-seeing excursions from the main central camp, there are numberless, lovely little saunters and scrambles and a dozen or so not so very little. Among the best of these are to Lambert and Fair View Domes; to the topmost spires of Cathedral Peak, and to those of the North Church, around the base of which you pass on your way to Mount Conness; to one of the very loveliest of the glacier-meadows imbedded in the pine woods about three miles north of the Soda Springs, where forty-two years ago I spent six weeks. It trends east and west, and you can find it easily by going past the base of Lambert’s Dome to Dog Lake and thence up northward through the woods about a mile or so; to the shining rock-waves full of ice-burnished, feldspar crystals at the foot of the meadows; to Lake Tenaya; and, last but not least, a rather long and very hearty scramble down by the end of the meadow along the Tioga road toward Lake Tenaya to the crossing of Cathedral Creek, where you turn off and trace the creek down to its confluence with the Tuolumne. This is a genuine scramble much of the way but one of the most wonderfully telling in its glacial rock-forms and inscriptions.
If you stop and fish at every tempting lake and stream you come to, a whole month, or even two months, will not be too long for this grand High Sierra excursion. My own Sierra trip was ten years long.
Short carriage trips are usually made in the early morning to Mirror Lake to see its wonderful reflections of the Half Dome and Mount Watkins; and in the afternoon many ride down the Valley to see the Bridal Veil rainbows or up the river cañon to see those of the Vernal Fall; where, standing in the spray, not minding getting drenched, you may see what are called round rainbows, when the two ends of the ordinary bow are lengthened and meet at your feet, forming a complete circle which is broken and united again and again as determined by the varying wafts of spray. A few ambitious scramblers climb to the top of the Sentinel Rock, others walk or ride down the Valley and up to the once-famous Inspiration Point for a last grand view; while a good many appreciative tourists, who slave only day or two, do no climbing or riding but spend their time sauntering on the meadows by the river, watching the falls, and the relay of light and shade among the rocks from morning to night, perhaps gaining more than those who make haste up the trails in large noisy parties. Those who have unlimited time find something worth while all the year round on every accessible part of the vast deeply sculptured walls. At least so I have found it after making the Valley my home for years.
Here are a few specimens selected from my own short trips which walkers may find useful.
One, up the river cañon, across the bridge between the Vernal and Nevada Falls, through chaparral beds and boulders to the shoulder of Half Dome, along the top of the shoulder to the dome itself, down by a crumbling slot gully and close along the base of the tremendous split front (the most awfully impressive, sheer, precipice view I ever found in all my cañon wanderings), thence up the east shoulder and along the ridge to Clouds’ Rest—a glorious sunset—then a grand starry run back home to my cabin; down through the junipers, down through the firs, now in black shadows, now in white light, past roaring Nevada and Vernal, flowering ghost-like beneath their huge frowning cliffs; down the dark, gloomy cañon, through the pines of the Valley, dreamily murmuring in their calm, breezy sleep—a fine wild little excursion for good legs and good eyes—so much sun-, moon- and star-shine in it, and sublime, up-and-down rhythmical, glacial topography.
Another, to the head of Yosemite Fall by Indian Cañon; thence up the Yosemite Creek, tracing it all the way to its highest sources back of Mount Hoffman, then a wide sweep around the head of its dome-paved basin, passing its many little lakes and bogs, gardens and groves, trilling, warbling rills, and back by the Fall Cañon. This was one of my Sabbath walk, run-and-slide excursions long ago before any trail had been made on the north side of the Valley.
Another fine trip was up, bright and early, by Avalanche Cañon to Glacier Point, along the rugged south wall, tracing all its far outs and ins to the head of the Bridal Veil Fall, thence back home, bright and late, by a brushy, bouldery slope between Cathedral rocks and Cathedral spires and along the level Valley floor. This was one of my long, bright-day and bright-night walks thirty or forty years ago when, like river and ocean currents, time flowed undivided, uncounted—a fine free, sauntery, scrambly, botanical, beauty-filled ramble. The walk up the Valley was made glorious by the marvelous brightness of the morning star. So great was her light, she made every tree cast a well-defined shadow on the smooth sandy ground.
Everybody who visits Yosemite wants to see the famous Big Trees. Before the railroad was constructed, all three of the stage-roads that entered the Valley passed through a grove of these trees by the way; namely, the Tuolumne, Merced and Mariposa groves. The Tuolumne grove was passed on the Big Oak Flat road, the Merced grove by the Coulterville road and the Mariposa grove by the Raymond and Wawona road. Now, to see any one of these groves, a special trip has to be made. Most visitors go to the Mariposa grove, the largest of the three. On this Sequoia trip you see not only the giant Big Trees but magnificent forests of silver fir, sugar pine, yellow pine, libocedrus and Douglas spruce. The trip need not require more than two days, spending a night in a good hotel at Wawona, a beautiful place on the south fork of the Merced River, and returning to the Valley or to El Portal, the terminus of the railroad. This extra trip by stage costs fifteen dollars. All the High Sierra excursions that I have sketched cost from a dollar a week to anything you like. None of mine when I was exploring the Sierra cost over a dollar a week, most of them less.
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