YOSEMITE VALLEY.

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The name is Indian. Pronounce it in four syllables, accenting the second. It means "Big Grizzly Bear."

The valley lies very near the centre of the State, reckoning north and south, about one fifth the way across from east to west, and almost exactly in the middle of the high Sierras which inclose it. Its direction from San Francisco is a little south of east, and its distance about one hundred and forty miles in an air line. The valley itself lies nearly east and west. Its main axis runs a little north of east by a little south of west.

It consists of three parts:

1st. The surrounding wall of solid rock, nearly vertical, and varying in height from one thousand to four and even five thousand feet.

2d. The slope of rocky masses and fragments which have fallen from the face of the cliffs, forming a sort of talus or escarpment along the foot of this wall, from seventy-five to three hundred and fifty feet high, throughout the greater part of its extent.

3d. The nearly level bottom land, lying between these slopes, forming the valley proper, and divided into two unequal parts by the Merced River flowing through westerly, from end to end.

The main valley is seven miles long; though one may make it longer if he estimates the branches or divisions at the upper or eastern end. Its width varies from a few feet on either side of the stream, to a full mile and a quarter in its broadest part. It contains over a thousand acres; two thirds meadow, and the rest a few feet higher, somewhat sandy, gravelly, and, in places, covered with rocks and boulders from the surrounding cliffs. Over the latter portion, at irregular intervals, trees, shrubs and ferns are sparsely sprinkled or set in irregular groups. The richer bottom supports several fine clumps and groves of graceful trees.

The bottom of the valley is four thousand feet above the level of the sea, and has an average fall, towards the west, of about six feet to the mile. The river varies in width from fifty to seventy feet, and in depth from six to twelve feet. Its bottom is gravelly, its current remarkably swift, its waters clear as crystal. Trout, of delicious quality, abound, but seldom allow white men to catch them.

The rocky wall which shuts it in, averages over three quarters of a mile in perpendicular height. Nothing on wheels has ever gone up or down this tremendous precipice, and in only two places have the surest-footed horses or mules been able to find a safe trail.

Yosemite Valley is really a huge sink or cleft in a tangle of rock-mountains; a gigantic trough, not scooped or hollowed out from above, but sunk straight down, as if the bottom had dropped plumb toward the centre, leaving both walls so high that if either should fall, its top would reach clear across the valley and crash against the opposite cliff several hundred feet above its base.

In many places these cliffs rise into rock-mountains, or swell into huge mountainous domes, two or three of which have been split squarely in two, or cleft straight down from top to bottom, and the two halves, still standing straight up, have been heaved or thrown a half-mile asunder, whence each looks wistfully across at its old mate, or frowns sternly and gloomily down upon the beautiful valley which quietly keeps them apart.

Here and there they tower into lofty spires, shoot up in shattered or splintered needles, or solemnly stand in stately groups of massive turrets. High bastions surmount steep precipices, and both look down on awful chasms.

Back from the edge of the valley, behind these cliffs, the rock country stretches away in every direction through leagues of solid granite, rising irregularly into scattered hills, peaks and mountains, between which run the various snow-fed streams, whose final, sudden plunge over the valley's sharp and rocky brink makes the numerous falls of such wonderful height.

Coming in by either trail, one enters the western or lower end of the valley. We will suppose ourselves entering by the Mariposa trail. We have clambered, or allowed our animals to clamber, safely down the rocky, steep, and crooked trail, which lands us finally at the foot of the precipitous slope of two thousand seven hundred feet. As we follow the trail up the valley, that is, bearing away to the right, going eastward along the foot of the south wall, we encounter the falls, mountains, spires and domes in the following order:

One coming in by the Coulterville, Hardin's or Big Oak Flat trail, finds himself at the same end of the valley, directly opposite the foot of the Mariposa trail, having the river between; and as he bears away to the left, along the base of the north wall, he would, of course, meet all these wonders in exactly the reverse order. But to return to the foot of the Mariposa or Clark's trail:

First, the

Bridal Veil Fall,

Indian name Po-ho-no, meaning, "The Spirit of the Evil Wind." The fall is over nine hundred feet high, and of indescribable beauty. The stream which forms it has an average width of some sixty-five feet at the edge of the cliff where it breaks over the brink. It is narrower in summer and wider in winter. For six hundred and thirty feet the stream leaps clear of the cliff in one unbroken fall. Thence it rushes down the steep slope of broken rocks in a confusion of intermingled cascades nearly three hundred feet more.

The varying pressure of the changeful wind causes a veil-like waving, swaying and fluttering, which readily suggests the obviously fitting and most appropriate name.

What could a bride be made of,

Who would wear a veil like this?

No sooner asked than answered,

She must be "Maid o' the Mist."

This fall presents its greatest beauty in May or June when the volume of water is not too great. The situation of Pohono, added to its intrinsic beauty, waving a welcome as the tourist enters and fluttering a farewell as he leaves, make it the universal favorite. Ladies especially love to linger at its foot, feasting their eyes with its marvelous and changeful beauty, and delighting their hearts with the delicious suggestiveness of its most appropriate name. The honeymoon can nowhere be more fittingly or happily spent than within sight of Pohono.

Half a mile further the cliff rounds outward and swells upward into an enormous double, rocky bastion, the

Cathedral Rocks.

Two thousand six hundred and sixty feet above the valley. Indian name, Po-see-nah Choock-kah, meaning a large store or hoard of acorns. From certain points of sight the form of these rocks readily suggests the outline of a dilapidated Gothic cathedral. Only the superior grandeur of Tu-toch-ah-nu-lah and the South Dome, prevent this rock from greater fame. Outside of Yosemite it would quickly attain a world-wide celebrity.

Just beyond these rocks the cliff bears away to the southeast and sends up two slender, graceful pinnacles of splintered granite, rising five hundred feet above the main wall, which supports them. These are the

Cathedral Spires.

Their summits are twenty-four hundred feet above the valley. Seen from the northeast, a mile distant, these spires appear symmetrical, of equal height, squarely hewn and rising above the edge of the cliff behind, exactly like two towers of a Gothic cathedral. One who doubts the appropriateness of their name, has only to view them from this point, whence a single glance will end his skepticism. Beyond the spires the wall runs southeasterly a quarter of a mile, then curves through an easterly and northerly sweep into a north and south line. The whole sweep forms a sort of precipitous coast with its rocky headlands, inclosing the valley between like an emerald bay. Beyond this bay the rocky wall gradually curves again, and resumes its easterly trend. An eighth of a mile further brings us to

The Fissure.

This is a cleft or split in the rock, running back southeasterly at nearly a right angle with the face of the cliff. It is one thousand feet deep, five feet wide at the top and front, and grows gradually narrower as it extends downward and backward into the mountain. Several boulders have fallen into it and lodged at different depths.

A third of a mile east of this fissure, and a mile and three quarters from the Cathedral Rocks, another rocky promontory projects northwesterly, like a huge buttress, a third of a mile into the valley, crowned with a lofty granite obelisk, three hundred feet thick, and standing straight up twelve hundred feet above the giant cliff which supports it. This is the famous

Sentinel Rock,

so named from its resemblance to a gigantic watchtower or signal station, for which, the legends say, the Indians formerly used it. The Indian name was Loya. Its top is three thousand and forty-three feet above the river at its foot. The sides show plainly-marked perpendicular cleavages in the granite.

Although so steep in front and at the sides, a strong grasp, a sure foot, a cool nerve and a calm head can safely climb it from the rear, that is, the southwest side. At least they have done so more than once, and planted a flag to wave in triumph from its summit. By the unanimous and unquestioned verdict of all tourists, this rock is one of the grandest and most beautiful even in Yosemite itself. Its striking prominence has made it a favorite subject with all artists who have visited the valley.

Three quarters of a mile southeast of the sentinel tower, half a mile back from the brink of the precipice, and partially or totally hidden by it, according as the spectator stands nearer to or farther from the foot of the cliff, the

Sentinel Dome

lifts its hemispherical bulk four thousand one hundred and fifty feet. This is one of the most regularly formed of all of the peculiar dome-like peaks about the valley. The Indian name was Loy-e-ma. A horseman can reach the very summit by a trail up the eastern slope, and enjoy a most extensive view as his reward. From this dome, the profile of the South Dome and strongly marked moraines of the Too-loo-le-wack CaÑon appear to better advantage than from any other point.

A mile east of Sentinel Rock the face of the cliff becomes less precipitous, bends sharply around to the south, and thence back towards the southwest, forming an angular and sloping rocky bluff known as

Glacier Rock,

called by the Indians, Oo-woo-yoo-wah, which means, the "Great Rock of the Elk." The story has it that during one of the expeditions of troops into the valley, a party of soldiers, searching for Indians, undertook to climb this rock, and while, slowly and with great labor, working their way up its smooth and steep slope, the hunted red men suddenly appeared upon its summit, and began to roll large stones down upon them. These came thundering down with terrific noise and frightful speed. The pale faces turned and fled with headlong haste, but the destructive missiles smote several of them with instant death.

From the point of Glacier Rock one has a fine view of the valley. All the domes, with the Yosemite, Vernal and Nevada Falls are plainly visible thence.

For nearly a mile southeast of Glacier Rock the cliff becomes steeper and more precipitous, forming the western wall of a wild, rough caÑon, stretching away southeasterly for nearly a mile. Over the cliff at the head of this caÑon the south fork of the Merced plunges six hundred feet in the

Illilouette Fall.

This is also called the Too-loo-le-wack, or Too-lool-we-ack Fall. The meaning of either of these Indian names is not certainly given. Cunningham, one of the oldest and best guides of the valley, calls the caÑon and the fall at the head of it, the El-lil-o-wit. The tourist who attempts this caÑon must leave all hoofs behind, and, falling back to first principles, depend entirely upon his own understanding.

Among the enormous masses of rock which obstruct it, several extensive fissures and romantic caverns furnish additional stimulus to the wonder-loving pedestrian. As General Coulter says: "rough is no name for it." It is one of the wildest places imaginable. Few tourists accomplish it, but those who do are amply repaid.

From the foot of the Il-lil-ou-ette CaÑon make your way directly east, clamber along half a mile, or let your horse do it for you, then bear away to the right, slightly south of east, and you find yourself entering the caÑon of the main Merced itself. Now pick your way carefully along, and, as soon as you feel sufficiently sure of your foothold, look about you, and look ahead. Did you ever see finer boulder-scenery in your life? Stop under the sheltering lee of this huge, church-like boulder, and don the oiled or rubber suit which awaits your hire. You can get on without it, but the spray will quickly wet you into a

"Dem'd damp, moist and disagreeable body,"

if you try it.

Now take a stout stick, a deep breath, hold firmly on to both and plunge sturdily along the ascending trail. The deepest, richest and greenest of moss lines the narrow foot-path on either hand. Look quickly; enjoy it while you may, for presently you find breath and sight nearly taken away together by heavy spray-gusts, rushing, wind-driven, down the caÑon. Catching the intervals between, and catching your breath at the same time, you lift your nearly blinded eyes to the

Vernal Fall,

four hundred and fifty feet high, one hundred feet wide, and from three to five feet deep where it breaks over the square-cut edge of the solid granite beneath. The name Vernal was given it on account of the greenness of its water as it plunges over the brink, as well as to distinguish it from the very white fall a mile above. The Indian name was Pi-wy-ack, which is differently translated to mean "a shower of crystals," or "the cataract of diamonds."

This fall pours in one solid unbroken sheet of emerald green, flecked and fringed with creamy foam, and filling the whole caÑon below with a thick, and fine and ceaseless spray, which keeps its moss, and grass and foliage of a rich, deep green nowhere surpassed in nature. This spray also combines with the sunshine to develop another and a marvelous beauty. At almost any point along the trail for several rods below the fall, the visitor who is climbing in the morning has only to turn square about to find himself glorified by an exquisitely beautiful circular rainbow surrounding his head like a halo. This rainbow forms a complete circle of so small a diameter that the tourist who views it for the first time involuntarily stretches out his hands to grasp it.

The path is wet and slippery, and the ladder-stairs which carry one up the right-hand face of the cliff, just at the south edge of the fall, are steep and tiresome. But good oil or rubber suits keep out the wet, a good restful pause now and then keeps in the breath, while careful stepping and firm holding on rob the steepness and slipperiness of all their real danger. Scores of ladies go up and come down every season without accident or harmful fatigue.

Arrived at the top of the singularly square-cut granite cliff, we turn to the left, walk to the very edge of the stream and the brink of the fall, and gaze into the misty chasm in which the foot of the fall disappears. One need not fear to do so, for nature, as if with special forethought for the gratification of future guests, has provided a remarkable parapet of solid granite running along the very edge of the brink for several yards south of the fall, just breast high, and looking as if made on purpose for timid tourists to lean over, and gaze with fearless safety into the seething chasm in whose foaming depths the foot of the cataract shrouds itself in impenetrable mist.

This ceaseless mistiness makes it almost impossible to estimate or calculate the exact height of the fall with any satisfactory accuracy. Another variable element which enters into all conjectures of its height is the fact that the rock on which it strikes slopes sharply down for upwards of a hundred and sixty feet. Hence in late spring or early summer, when the volume and velocity of the river are greatest, the water, shooting further out, falls at the very base of this slope, and gives the fall a height of four hundred and seventy-five or even five hundred feet in May or June. In October, on the other hand, when the stream is at its lowest, the water, falling straight down, strikes upon the top of this slope, a hundred and sixty or seventy-five feet above its base, and thus diminishes the height of the fall by just that amount.

In its volume, this fall resembles Niagara more than any other in the valley. In width, of course, it falls far below, but its height is more than three times as great. It also resembles Niagara in its greatening on the gaze with each successive visit. In its approaches, in its surroundings, and in itself, the Vernal fall surpasses expectation and fully satisfies desire.

Half a mile above the Vernal is a small but beautiful gem of a little fall, called the

Kachoomah,

or Wild Cat Fall. The reason of the name is obvious to one standing a hundred feet below, and noting how the impetuous stream, breaking over the sharp edge of a huge transverse boulder, dashes against the sloping side of another; lying angularly across; and is thrown, or seems to spring, diagonally across towards the northern bank, readily, though roughly, suggesting the sudden side-spring of the animal for whom the observing red man named it.

Another half mile, and the rocky walls close together, shut us in and bar our further progress. The caÑon narrows to a point, over whose right hand wall, close to the very angle of meeting, the same river, the main Merced, plunges its whole volume in the famous

Nevada Fall,

seven hundred feet high, seventy-five feet wide at the brink, and one hundred and thirty below. This fall is, in all respects, one of the grandest in the world. In height, in width, in purity and volume of water during the early summer, in graceful peculiarities and in grandeur of surrounding scenery, it is simply stupendous. Other falls, though few, surpass it in the single element of height, but in surrounding grandeur, in the harmony of beauty and magnificence, none equal this. None brings the visitor oftener to its foot, detains him with greater delight, or sends him away with more profound satisfaction.

The exact statement of the height of this fall is hindered by causes similar to those at the Vernal, viz: the constant and blinding spray around the bottom, and the consequent uncertainty as to the exact spot where the water strikes.

The rock beneath this fall is not vertical, but rather steeply inclined, having a slope of about eighty-five degrees through its upper half and not far from seventy-five degrees through its lower. Hence in summer, when tourists usually see it, the diminished force of the current causes the water rather to slide down the slope, than to shoot out over and fall clear of it, as in the spring. Thus, from June to November the Nevada is more properly a chute or slide than a fall. During this season the friction of the rock breaks the stream into a white froth; hence the name, Nevada, or Snowy Fall.

When the water is very low, the fittest thing to which one could liken it would be to myriads of white lace or gauze veils hung over the face of the cliff, waving and fluttering in the wind. A party of ladies originated this figure, and it occurred also to Mr. Bowles in his fine descriptions of Yosemite wonders.

As one stands in the caÑon below gazing at the Nevada, the Snowy Fall, away upon his left, about a third of a mile back from the brink of the northeast wall of the caÑon, rises

Mt. Broderick,

or the Cap of Liberty, whose general outline suggests its name. Its rounded summit lifts its smooth, weather-polished granite two thousand feet above the fall and nearly five thousand above the main valley. It bears upon its crown a single juniper of enormous diameter.

Away to the right of the caÑon, just peeping above the edge of the cliff, and nearly two miles south-southeast of the Nevada Fall, rises the steep, conical summit of the South Dome, or

Mt. Starr King,

reaching an estimated height of one mile above the valley. Next to the wonderful half-dome, this is the steepest and smoothest cone in the region. Indian name, See-wah-lam, meaning not known. Its exact height, like that of its great namesake, has never been satisfactorily settled.

Clambering back down this caÑon, depositing our oiled or rubber suits, and experiencing an immediate sense of relief and lightness, we retrace the trail up which we came, bear away to the right, that is, going nearly northwest, proceed nearly or quite a mile round the base of a lofty buttress, and open the

Tenaya CaÑon,

stretching away northeast nearly in a continuous line with the main valley itself.

About one mile up this caÑon towers Yosemite's sheerest and loftiest isolated cliff, the

Half-Dome

itself. It is a bare crest of naked granite, four thousand seven hundred and forty feet high, cleft straight down in one vast vertical front on the Tenaya, or northwest side, while on the back, that is, toward the southeast, it swells off and rounds away with a dome-like sweep that utterly dwarfs the grandeur of a thousand St. Peters in one.

Following still on up the Tenaya CaÑon, nearly two miles beyond the dome, and a thousand feet higher, rises the

Clouds' Rest,

a granite ridge, long, bare and steep, having its axis parallel with that of the valley, and falling away along its southeastern slope into the rocky mountain wilderness of the High Sierras. This is one of the few points about the valley which the Geological Survey has not yet measured. They estimated its height one thousand feet above that of the Half Dome, which would make its summit ten thousand feet, or nearly two miles above the sea level.

Beyond this, little of note invites the traveler's delay, so we make our way northwesterly straight across this caÑon from the base of its southeasterly wall toward that of the opposite cliff. On the way, however,

Mirror Lake

arrests and enchants us. Surely water reflections were never more perfect. The Indian name Ke-ko-too-yem, Sleeping Water, was never more happily bestowed. Imagine a perfect water mirror nearly eight acres in extent, and of a temperament so calm and deep and philosophic that it devotes its whole life to the profoundest reflection. A mile of solid cliff above, a mile of seeming solid cliff beneath; for though the mind knows the lower to be only an image, the eye cannot, by simple sight alone, determine which is the solid original and which the shadowy reflection.

Twin mountains, base to base, here meet the astonished eye;

One towers toward heaven in substance vast,

One looms below in shadow cast,

As grand, as perfect as its peer on high.

In early morning, when no breeze ripples the lake, its reflections are, indeed, marvelously life-like. So exactly is every line and point repeated that the photographic view has puzzled hundreds to tell which mountain is in the air and which is in the water. The spectator who takes the photogram in his hand for the first time often hesitates for several minutes before he can determine which side up the picture should be held. The depth of the lake is from eight to twenty feet.

One sufficiently vigorous and persevering may push on up the Tenaya creek till he finds the

Tenaya Lake,

over a mile long, snugly nestled in among the mountains. This lies beyond the usual limit of tourists' excursions, but well repays a visit.

Nearly a mile northwest of the lake, and about a third of a mile back from the edge of the cliff, the

North Dome

lifts its rounded granite bulk three thousand five hundred and seventy feet above the valley. It looks as if built of huge, concentric, overlapping, hemispherical domes, piled one upon another, and having their overlapping edges irregularly broken away. On the valley side, that is, toward the south and southeast, it is so steep that no human foot has ever climbed it. In the rear, however, that is, toward the north and west, it falls away in a vast ridge or spine, along which one can easily gain the very summit of the dome itself. The Indian name was To-coy-ah, meaning the shade of an Indian baby basket.

Passing three quarters of a mile still down, we reach the angle or turn between the Tenaya caÑon and the valley proper. In this turn, in fact forming the angle, stands the

Washington Column,

a rounded, columnar rock tower, partially standing forth from the abutting cliff behind. This reaches the height of two thousand five hundred feet.

Immediately beyond this, large masses of the huge concentric, overlapping plates, have cracked off, slipped away and fallen, leaving rough bas-relief arches several hundred yards long, and projecting some scores of feet, like rudely-drawn gigantic eyebrows. These are commonly called the

Royal Arches,

or the Arched Rocks, but the Indian name, Hun-to, "The Watching Eye," will better satisfy the poetical visitor, unless, indeed, his Masonic proclivities quite overpower his poetic appreciation, in which case he will undoubtedly prefer the former title.

For the next mile and a half northwest nothing of special wonder for Yosemite detains us.

The relief is fitting and needful, not only that we may recover in some degree from the continued effect of the marvels already past, but, more especially, that we may rally in preparation for the most stupendous wonder of them all, the great

Yosemite Fall

itself. Here language ceases and art quite fails. No words nor paintings, not even the photogram itself, can reproduce one tithe of the grandeur here enthroned. A cataract from heaven to earth, plunging from the clouds of the sky to bury itself among the trees of the forest. The loftiest waterfall yet known upon the face of the globe.

Don't mention figures yet, please. When a man is overwhelmed with the sublime, don't plunge him into statistics. By and by, when we have cooled down to a safe pitch, we may condescend to hear the calm calculator project his inexorable mathematics into the very face of nature's sublimity and triumphantly tell us just how great this surpassing wonder is. But after all his exactest calculations, his absolute measurements and his positive assurances, one feels how small the fraction of real greatness which figures can express or the intellect apprehend. A cataract half a mile high, setting its forehead against the stars and planting its feet at the base of the eternal hills. Gracefully swaying from side to side in rhythmical vibration, swelling into grandeur in earlier spring, and shrinking into beauty under the ardency of summer heat; towering far above all other cataracts, it calmly abides, the undisputed monarch of them all.

A half mile is no exaggeration, for the official measurement of the State Survey makes the height two thousand six hundred and forty-one (2,641) feet—a full half mile, and one foot more.

The fall is not in one unbroken, perpendicular sheet, but in three successive leaps. In the upper fall, the stream slides over a huge rounded lip or edge of polished granite, and falls one thousand five hundred and eighty-seven feet in one tremendous plunge. Here its whole volume thunders upon a broad shelf or recess, whence it rushes in a series of roughly-broken cascades down a broken slope of over seven hundred feet in linear measurement, but whose base is six hundred and twenty-six feet perpendicularly below its top. From the bottom of this broken slope it makes a final plunge of four hundred and twenty-eight feet in one clear fall, and then slides off contentedly into the restful shadows of the welcoming forests below.

Its width, like that of all snow-fed streams, varies greatly with the season. In March or April, when the tributary snows are melting most rapidly, and myriads of streamlets swell its volume, the stream is from seventy-five to a hundred feet wide, where it suddenly slips over the smoothly-rounded granite at its upper brink. During the same season it scatters or spreads to a width of from three to four hundred feet, when it breaks upon the rocky masses below.

In later spring, or earlier summer, it dwindles to less than a third of its greatest bulk; and its most intimate friend, the veteran Yosemite pioneer, Hutchings, tells us that he has seen it when it hardly seemed more than a silver thread winding down the face of the cliff. Under a full moon, the element of weirdness mingles with its graceful grandeur, shrouds it with mystery, and transports one into a soft and dreamy wonder-land, from which he cares not to return.

A mile further on our way back toward the western end, brings us under, or in front of, the triple rocky group, or three-peaked stone-mountain, whose name, the

Three Brothers,

readily suggests itself to one standing in the proper place below. They are three huge, bluntly conical, rocky peaks, fronting nearly south, slightly inclined toward the valley and descending in height as they approach it. To the rude Indian fancy they might well suggest the name Porn-porn-pa-sue—"Mountains playing leap-frog,"—with which they christened them.

The highest, which is the northernmost, the one furthest back from the valley, is three thousand eight hundred and thirty feet high. The summit of this rock is readily reached by a trail from the rear, and affords a superb view of the valley and its surroundings. Nearly all who have enjoyed it consider it the very best to be had.

Another mile-and-a-half and the rocky wonders of Yosemite fitly culminate and terminate in

Tu-toch-ah-nu-lah,

"The Great Chief of the Valley" more commonly, though very weakly, called "El Capitan," an ordinary Spanish word, meaning simply, "the Captain;" good enough for a ferry-boat or river steamer, but entirely beneath the dignity of this most magnificent rock on the face of the earth.

Tu-toch-ah-nulah is an immense granite cliff, projecting angularly into the valley, toward the southwest. It has two fronts, one facing nearly west, the other southeasterly, meeting in a sub-acute angle. These two fronts are over a mile long, and three thousand three hundred feet high, smooth, bare and vertical, and bounded above by a sharp edge, standing pressed against the sky, which its Atlas-like shoulder seems made to uphold.

The State Survey, with all its scientific coolness, could not help saying, "El Capitan imposes upon us by its stupendous bulk, which seems as if hewed from the mountains on purpose to stand as the type of eternal massiveness. It is doubtful, if anywhere in the world, there is presented so squarely cut, so lofty and so imposing a face of rock." Starr King declared, "A more majestic object than this rock, I never expect to see on this planet." Horace Greeley, who enjoyed the rare experience of entering the valley by night, and in moonlight too, thus pays tribute to the Great Chief:

"That first, full, deliberate gaze, up the opposite height! Can I ever forget it? The valley here, is scarcely half a mile wide, while its northern wall of mainly naked, perpendicular granite, is at least four thousand feet high, probably more. But the modicum of moonlight that fell into this awful gorge, gave to that precipice a vagueness of outline, an indefinite vastness, a ghostly and weird spirituality. Had the mountain spoken to me in an audible voice, or begun to lean over with the purpose of burying me, I should hardly have been surprised."

After Tutochahnulah, nothing on earth can seem very grand or overpowering, and with this the wonders of the valley fitly close.

We have, by no means, seen all the falls, nor even mentioned all the peaks, but the others are of little note in Yosemite, though, elsewhere, tourists might go a thousand miles to see the least of them. This valley is, beyond comparison, the most wonderful and beautiful of all earthly sights. No matter how incredulous one may be before entering, the Great Chief and his tremendous allies, soon crush him into the most humble and complete subjection. Do not expect, however, that your first view will stagger your skepticism. On the contrary, it may even confirm it. Upon our first view of Tutochahnulah, as we were walking into the valley, one bright July forenoon, we stopped a mile and a half from its foot, collected ourselves for a calm, cool, mathematical judgment and said with all confidence, "That rock isn't over fifteen hundred feet high. It can't be. Why, just look at that tree near its base. That tree, certainly, can't be more than a hundred and twenty-five feet high, and certainly, the cliff doesn't rise more than ten times its height above it." But, unfortunately, we had forgotten that never before had we seen the works of nature on as grand a scale. One's judgment has to change its base. He has to reconstruct it; to adopt a new unit. Comparison serves him little, for he has no adequate standard by which to measure, or with which to compare the rock-mountains before him. They are like nothing else. They are a law unto themselves, and one must learn the law, the new law, before he can begin to enter the secret of their greatness. Look at that tree. Elsewhere you would call it lofty. It measures a hundred and fifty feet, and yet, that wall of solid rock behind rises straight up to twenty times its height above it. Look again; now, turn away; shut eyes and think. Forget all former standards and adopt the new. Slowly you begin to "even" yourself to the stupendous scale of the gigantic shapes around.

Even Niagara requires two or three days before one begins to fully realize or truly appreciate its greatness. How much more, then, Yosemite, compared with which Niagara is but a very little thing! Then, on the other hand, one must remember that after he has adjusted himself to the new and grander scale of Yosemite, upon coming out into the midst of ordinary hills and mountains, for several days they seem low and flat and small.

A single visit to Yosemite dwarfs all other natural wonders and spoils one for all places else. He who has seen it listens quietly to the most enthusiastic rhapsodies of the most widely traveled tourists, and simply answers, with a calm, superior smile, "Ah, that's all very well, but you should see Yosemite."

The Traveler's University—should such an institution ever exist—can never righteously graduate the most widely traveled tourist, until he can truthfully add to his name, "Y.S.T."—Yosemite Tourist.

                                                                                                                                                                                                                                                                                                           

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