Time and Change Part 4

II

One warm, bright Sunday near the end of April, six of us walked up from the hotel to Vernal and Nevada Falls, or as near to them as we could get, and took our fill of the tumult of foaming waters struggling with the wreck of huge granite cliffs: so impa.s.sive and immobile the rocks, so impetuous and reckless and determined the onset of the waters, till the falls are reached, when the obstructed river seems to find the escape and the freedom it was so eagerly seeking. Better to be completely changed into foam and spray by one single leap of six hundred feet into empty s.p.a.ce, the river seems to say, than be forever baffled and tortured and torn on this rack of merciless boulders.

We followed the zigzagging trail up the steep side of the valley, touching melting snow-banks in its upper courses, pa.s.sing huge granite rocks also melting in the slow heat of the geologic ages, pausing to take in the rugged, s.h.a.ggy spruces and pines that sentineled the mountain-sides here and there, or resting our eyes upon Liberty Cap, which carries its suggestive form a thousand feet or more above the Nevada Fall. What beauty, what grandeur attended us that day! the wild tumult of waters, the snow-white falls, the motionless avalanches of granite rocks, and the naked granite shaft, Liberty Cap, dominating all!

And that night, too, when we sat around a big camp-fire near our tents in the valley, and saw the full moon come up and look down upon us from behind Sentinel Rock, and heard the intermittent booming of Yosemite Falls sifting through the spruce trees that towered around us, and felt the tender, brooding spirit of the great valley, itself touched to lyric intensity by the grandeurs on every hand, steal in upon us, and possess our souls--surely that was a night none of us can ever forget. As Yosemite can stand the broad, searching light of midday and not be cheapened, so its enchantments can stand the light of the moon and the stars and not be rendered too vague and impalpable.

III

Going from the Grand Canon to Yosemite is going from one sublimity to another of a different order. The canon is the more strange, unearthly, apocryphal, appeals more to the imagination, and is the more overwhelming in its size, its wealth of color, and its mult.i.tude of suggestive forms. But for quiet majesty and beauty, with a touch of the sylvan and pastoral, too, Yosemite stands alone.

One could live with Yosemite, camp in it, tramp in it, winter and summer in it, and find nature in her tender and human, almost domestic moods, as well as in her grand and austere. But I do not think one could ever feel at home in or near the Grand Canon; it is too unlike anything we have ever known upon the earth; it is like a vision of some strange colossal city uncovered from the depth of geologic time. You may have come to it, as we did, from the Petrified Forests, where you saw the silicified trunks of thousands of gigantic trees or tree ferns, that grew millions of years ago, most of them uncovered, but many of them protruding from banks of clay and gravel, and in their interiors rich in all the colors of the rainbow, and you wonder if you may not now be gazing upon some petrified antediluvian city of temples and holy places exhumed by mysterious hands and opened up to the vulgar gaze of to-day. You look into it from above and from another world and you descend into it at your peril. Yosemite you enter as into a gigantic hall and make your own; the canon you gaze down upon, and are an alien, whether you enter it or not. Yosemite is carved out of the most majestic and enduring of all rocks, granite; the Grand Canon is carved out of one of the most beautiful, but perishable, red Carboniferous sandstone and limestone. There is a maze of beautiful and intricate lines in the latter, a wilderness of temple-like forms and monumental remains, and n.o.ble architectural profiles that delight while they bewilder the eye. Yosemite has much greater simplicity, and is much nearer the cla.s.sic standard of beauty. Its grand and austere features predominate, of course, but underneath these and adorning them are many touches of the idyllic and the picturesque. Its many waterfalls fluttering like white lace against its vertical granite walls, its smooth, level floor, its n.o.ble pines and oaks, its open glades, its sheltering groves, its bright, clear, winding river, its soft voice of many waters, its flowers, its birds, its gra.s.s, its verdure, even its orchards of blooming apple trees, all inclosed in this tremendous granite frame--what an unforgettable picture it all makes, what a blending of the sublime and the homelike and familiar it all is! It is the waterfalls that make the granite alive, and bursting into bloom as it were. What a touch they give! how they enliven the scene! What music they evoke from these harps of stone!

The first leap of Yosemite Falls is sixteen hundred feet--sixteen hundred feet of a compact ma.s.s of snowy rockets shooting downward and bursting into spray around which rainbows flit and hover. The next leap is four hundred feet, and the last six hundred. We tried to get near the foot and inspect the hidden recess in which this airy spirit again took on a more tangible form of still, running water, but the spray over a large area fell like a summer shower, drenching the trees and the rocks, and holding the inquisitive tourist off at a safe distance. We had to beat a retreat with dripping garments before we had got within fifty yards of the foot of the fall. At first I was surprised at the volume of water that came hurrying out of the hidden recess of dripping rocks and trees--a swiftly flowing stream, thirty or forty feet wide, and four or five feet deep. How could that comparatively narrow curtain of white spray up there give birth to such a full robust stream? But I saw that in making the tremendous leap from the top of the precipice, the stream was suddenly drawn out, as we stretch a rubber band in our hands, and that the solid and ma.s.sive current below was like the rubber again relaxed. The strain was over, and the united waters deepened and slowed up over their rocky bed.

Yosemite for a home or a camp, the Grand Canon for a spectacle. I have spoken of the robin I saw in Yosemite Valley. Think how forlorn and out of place a robin would seem in the Grand Canon! What would he do there? There is no turf for him to inspect, and there are no trees for him to perch on. I should as soon expect to find him amid the pyramids of Egypt, or amid the ruins of Karnak. The bluebird was in the Yosemite also, and the water-ouzel haunted the lucid waters.

I noticed a peculiarity of the oak in Yosemite that I never saw elsewhere [Footnote: I have since observed the same trait in the oaks in Georgia--probably a characteristic of this tree in southern lat.i.tudes.]--a fluid or outflowing condition of the growth aboveground, such as one usually sees in the roots of trees--so that it tended to envelop and swallow, as it were, any solid object with which it came in contact. If its trunk touched a point of rock, it would put out great oaken lips several inches in extent as if to draw the rock into its maw. If a dry limb was cut or broken off, a foot from the trunk, these thin oaken lips would slowly creep out and envelop it--a sort of Western omnivorous trait appearing in the trees.

Whitman refers to "the slumbering and liquid trees." These Yosemite oaks recall his expression more surely than any of our Eastern trees.

The reader may create for himself a good image of Yosemite by thinking of a section of seven or eight miles of the Hudson River, midway of its course, as emptied of its water and deepened three thousand feet or more, having the sides nearly vertical, with snow-white waterfalls fluttering against them here and there, the famous spires and domes planted along the rim, and the landscape of groves and glades, with its still, clear winding river, occupying the bottom.

IV

One cannot look upon Yosemite or walk beneath its towering walls without the question arising in his mind, How did all this happen?

What were the agents that brought it about? There has been a great geologic drama enacted here; who or what were the star actors? There are two other valleys in this part of the Sierra, Hetch-Hetchy and King's River, that are almost identical in their main features, though the Merced Yosemite is the widest of the three. Each of them is a tremendous chasm in the granite rock, with nearly vertical walls, domes, El Capitans, and Sentinel and Cathedral Rocks, and waterfalls--all modeled on the same general plan. I believe there is nothing just like this trio of Yosemites anywhere else on the globe.

Guided by one's ordinary sense or judgment alone, one's judgment as developed and disciplined by the everyday affairs of life and the everyday course of nature, one would say on beholding Yosemite that here is the work of exceptional and extraordinary agents or world-building forces. It is as surprising and exceptional as would be a cathedral in a village street, or a gigantic sequoia in a grove of our balsam firs. The approach to it up the Merced River does not prepare one for any such astonis.h.i.+ng spectacle as awaits one. The rus.h.i.+ng, foaming water amid the tumbled confusion of huge granite rocks and the open V-shaped valley, are nothing very remarkable or unusual. Then suddenly you are on the threshold of this hall of the elder G.o.ds. Demons and furies might lurk in the valley below, but here is the abode of the serene, beneficent Olympian deities. All is so calm, so hushed, so friendly, yet so towering, so stupendous, so unspeakably beautiful. You are in a mansion carved out of the granite foundations of the earth, with walls two or three thousand feet high, hung here and there with snow-white waterfalls, and supporting the blue sky on domes and pinnacles still higher. Oh, the calmness and majesty of the scene! the evidence of such tremendous activity of some force, some agent, and now so tranquil, so sheltering, so beneficent!

That there should be two or three Yosemites in the Sierra not very far apart, all with the main features singularly alike, is very significant--as if this kind of valley was latent in the granite of that region--some peculiarity of rock structure that lends itself readily to these formations. The Sierra lies beyond the southern limit of the great continental ice-sheet of late Tertiary times, but it nursed and reared many local glaciers, and to the eroding power of these its Yosemites are partly due. But water was at work here long before the ice--eating down into the granite and laying open the mountain for the ice to begin its work. Ice may come, and ice may go, says the river, but I go on forever. Water tends to make a V-shaped valley, ice a U-shaped one, though in the Hawaiian Islands, where water erosion alone has taken place, the prevailing form of the valleys is that of the U-shaped. Yosemite approximates to this shape, and ice has certainly played a part in its formation. But the glacier seems to have stopped at the outlet of the great valley; it did not travel beyond the gigantic hall it had helped to excavate.

The valley of the Merced from the mouth of Yosemite downward is an open valley strewn with huge angular granite rocks and shows no signs of glaciation whatever. The reason of this abruptness is quite beyond my ken. It is to me a plausible theory that when the granite that forms the Sierra was lifted or squeezed up by the shrinking of the earth, large fissures and creva.s.ses may have occurred, and that Yosemite and kindred valleys may be the result of the action of water and ice in enlarging these original chasms. Little wonder that the earlier geologists, such as Whitney, were led to attribute the exceptional character of these valleys to exceptional and extraordinary agents--to sudden faulting or dislocation of the earth's crust. But geologists are becoming more and more loath to call in the cataclysmal to explain any feature of the topography of the land. Not to the thunder or the lightning, to earthquake or volcano, to the forces of upheaval or dislocation, but to the still, small voice of the rain and the winds, of the frost and the snow,--the gentle forces now and here active all about us, carving the valleys and reducing the mountains, and changing the courses of rivers,--to these, as Lyell taught us, we are to look in nine cases out of ten, yes, in ninety-nine out of a hundred, to account for the configuration of the continents.

The geologists of our day, while not agreeing as to the amount of work done respectively by ice and water, yet agree that to the latter the larger proportion of the excavation is to be ascribed. At any rate between them both they have turned out one of the most beautiful and stupendous pieces of mountain carving to be found upon the earth.

IV

THROUGH THE EYES OF THE GEOLOGIST

I

How habitually we go about over the surface of the earth, delving it or cultivating it or leveling it, without thinking that it has not always been as we now find it, that the mountains were not always mountains, nor the valleys always valleys, nor the plains always plains, nor the sand always sand, nor the clay always clay. Our experience goes but a little way in such matters. Such a thought takes us from human time to G.o.d's time, from the horizon of place and years to the horizon of geologic ages. We go about our little affairs in the world, sowing and reaping and building and journeying, like children playing through the halls of their ancestors, without pausing to ask how these things all came about.

We do not reflect upon the age of our fields any more than we do upon the size of the globe under our feet: when we become curious about such matters and look upon the mountains as either old or young, or as the subjects of birth, growth, and decay, then we are unconscious geologists. It is to our interest in such things that geology appeals and it is this interest that it stimulates and guides.

What an astonis.h.i.+ng revelation, for instance, that the soil was born of the rocks, and is still born of the rocks; that every particle of it was once locked up in the primitive granite and was unlocked by the slow action of the rain and the dews and the snows; that the rocky ribs of the earth were clothed with this fertile soil out of which we came and to which we return by their own decay; that the pulling-down of the inorganic meant the building-up of the organic; that the death of the crystal meant the birth of the cell, and indirectly of you and me and of all that lives upon the earth.

Had there been no soil, had the rocks not decayed, there had been no you and me. Such considerations have long made me feel a keen interest in geology, and especially of late years have stimulated my desire to try to see the earth as the geologist sees it. I have always had a good opinion of the ground underfoot, out of which we all come, and to which we all return; and the story the geologists tell us about it is calculated to enhance greatly that good opinion.

I think that if I could be persuaded, as my fathers were, that the world was made in six days, by the fiat of a supernatural power, I should soon lose my interest in it. Such an account of it takes it out of the realm of human interest, because it takes it out of the realm of natural causation, and places it in the realm of the arbitrary, and non-natural. But to know that it was not made at all, in the mechanical sense, but that it grew--that it is an evolution as much as the life upon the surface, that it has an almost infinite past, that it has been developing and ripening for millions upon millions of years, a veritable apple upon the great sidereal tree, ameliorating from cycle to cycle, mellowing, coloring, sweetening--why, such a revelation adds immensely to our interest in it.

As with nearly everything else, the wonder of the world grows the more we grasp its history. The wonder of life grows the more we consider the chaos of fire and death out of which it came; the wonder of man grows the more we peer into the abyss of geologic time and of low b.e.s.t.i.a.l life out of which he came.

Not a tree, not a shrub, not a flower, not a green thing growing, not an insect of an hour, but has a background of a vast aeon of geologic and astronomic time, out of which the forces that shaped it have emerged, and over which the powers of chaos and darkness have failed to prevail.

The modern geologist affords us one of the best ill.u.s.trations of the uses of the scientific imagination that we can turn to. The scientific imagination seems to be about the latest phase of the evolution of the human mind. This power of interpretation of concrete facts, this Miltonic flight into time and s.p.a.ce, into the heavens above, and into the bowels of the earth beneath, and bodying forth a veritable history, a warring of the powers of light and darkness, with the triumph of the angels of light and life, makes Milton's picture seem hollow and unreal. The creative and poetic imagination has undoubtedly already reached its high-water mark. We shall probably never see the great imaginative works of the past surpa.s.sed or even equaled. But in the world of scientific discovery and interpretation, we see the imagination working in new fields and under new conditions, and achieving triumphs that mark a new epoch in the history of the race. Nature, which once terrified man and made a coward of him, now inspires him and fills him with love and enthusiasm.

The geologist is the interpreter of the records of the rocks. From a bit of strata here, and a bit there, he re-creates the earth as it was in successive geologic periods, as Cuvier reconstructed his extinct animals from fragments of their bones; and the same interpretative power of the imagination is called into play in both cases, only the palaeontologist has a much narrower field to work in, and the background of his re-creations must be supplied by the geologist.

Everything connected with the history of the earth is on such a vast scale--such a scale of time, such a scale of power, such a scale of movement--that in trying to measure it by our human standards and experience we are like the proverbial child with his cup on the seash.o.r.e. Looked at from our point of view, the great geological processes often seem engaged in world-destruction rather than in world-building. Those oft-repeated invasions of the continents by the ocean, which have gone on from Archaean times, and during which vast areas which had been dry land for ages were engulfed, seem like world-wide catastrophes. And no doubt they were such to myriads of plants and animals of those times. But this is the way the continents grew. All the forces of the invading waters were engaged in making more land.

The geologist is bold; he is made so by the facts and processes with which he deals; his daring affirmations are inspired by a study of the features of the earth about him; his time is not our time, his horizons are not our horizons; he escapes from our human experiences and standards into the vast out-of-doors of the geologic forces and geologic ages. The text he deciphers is written large, written across the face of the continent, written in mountain-chains and ocean depths, and in the piled strata of the globe. We untrained observers cannot spell out these texts, because they are written large; our vision is adjusted to smaller print; we are like the school-boy who finds on the map the name of a town or a river, but does not see the name of the state or the continent printed across it. If the geologist did not tell us, how should we ever suspect that probably where we now stand two or more miles of strata have been worn away by the winds and rains; that the soil of our garden, our farm, represents the ashes of mountains burned up in the slow fires of the geologic ages.

Geology first gives us an adequate conception of time. The limitations which shut our fathers into the narrow close of six thousand years are taken down by this great science and we are turned out into the open of unnumbered millions of years. Upon the background of geologic time our chronological time shows no more than a speck upon the sky. The whole of human history is but a mere fraction of a degree of this mighty arc. The Christian era would make but a few seconds of the vast cycle of the earth's history.

Geologic time! The words seem to ring down through the rocky strata of the earth's crust; they reverberate under the mountains, and make them rise and fall like the waves of the sea; they open up vistas through which we behold the continents and the oceans changing places, and the climates of the globe s.h.i.+fting like clouds in the sky; whole races and tribes of animal forms disappear and new ones come upon the scene. Such a past! the imagination can barely skirt the edge of it. As the pool in the field is to the sea that wraps the earth, so is the time of our histories to the cycle of ages in which the geologist reckons the events of the earth's history.

Through the eyes of the geologist one may look upon his native hills and see them as they were incalculable ages ago, and as they probably will be incalculable ages ahead; those hills, so unchanging during his lifetime, and during a thousand lifetimes, he may see as flitting as the cloud shadows upon the landscape. Out of the dark abyss of geologic time there come stalking the ghosts of lost mountains and lost hills and valleys and plains, or lost rivers and lakes, yea, of lost continents; we see a procession of the phantoms of strange and monstrous beasts, many of them colossal in size and fearful in form, and among the minor forms of this fearful troop of spectres we see the ones that carried safely forward, through the vicissitudes of those ages, the precious impulse that was to eventuate in the human race.

Only the geologist knows the part played by erosion in shaping the earth's surface as we see it. He sees, I repeat, the phantoms of vanished hills and mountains all about us. He sees their shadow forms wherever he looks. He follows out the lines of the flexed or folded strata where they come to the surface, and thus sketches in the air the elevation that has disappeared. In some places he finds that the valleys have become hills and the hills have become valleys, or that the anticlines and synclines, as he calls them, have changed places--as a result of the unequal hardness of the rocks. Over all the older parts of the country the original features have been so changed by erosion that, could they be suddenly restored, one would be lost on his home farm. The rocks have melted into soil, as the snow-banks in spring melt into water. The rocks that remain are like fragments of snow or ice that have so far withstood the weather. Geologists tell us that the great Appalachian chain has been in the course of the ages reduced almost to a base level or peneplain, and then reelevated and its hills and mountains carved out anew.

We change the surface of the earth a little with our engineering, drain a marsh, level a hill, sweep away a forest, or bore a mountain, but what are these compared with the changes that have gone on there before our race was heard of? In my native mountains, the Catskills, all those peaceful pastoral valleys, with their farms and homesteads, lie two or three thousand feet below the original surface of the land. Could the land be restored again to its first condition in Devonian times, probably the fields where I hoed corn and potatoes as a boy would be buried one or two miles beneath the rocks.

The Catskills are residual mountains, or what Aga.s.siz calls "denudation mountains." When we look at them with the eye of the geologist we see the great plateau of tableland of Devonian times out of which they were carved by the slow action of the sub-aerial forces. They are like the little ridges and mounds of soil that remain of your garden-patch after the waters of a cloudburst have swept over it. They are immeasurably old, but they do not look it, except to the eye of the geologist. There is nothing decrepit in their appearance, nothing broken, or angular, or gaunt, or rawboned.

Their long, easy, flowing lines, their broad, smooth backs, their deep, wide, gently sloping valleys, all help to give them a look of repose and serenity, as if the fret and fever of life were long since pa.s.sed with them. Compared with the newer mountains of uplift in the West, they are like cattle lying down and ruminating in the field beside alert wild steers with rigid limbs and tossing horns.

They sleep and dream with bowed heads upon the landscape. Their great flanks and backs are covered with a deep soil that nourishes a very even growth of beech, birch, and maple forests. Though so old, their tranquillity never seems to have been disturbed; no storm-and-stress period has left its mark upon them. Their strata all lie horizontal just as they were laid down in the old seas, and nothing but the slow gentle pa.s.sage of the hand of time shows in their contours. Mountains of peace and repose, hills and valleys with the flowing lines of youth, coming down to us from the fore- world of Palaeozoic time, yet only rounded and mellowed by the aeons they have pa.s.sed through. Old, oh, so old, but young with verdure and limpid streams, and the pastoral spirit of to-day!

To the geologist most mountains are short-lived. When he finds great st.u.r.dy ranges, like the Alps, the Andes, the Himalayas, he knows they are young,--mere boys. When they get old, they will be cut down, and their pride and glory gone. A few more of these geologic years and they will be reduced to a peneplain,--only their stumps left. This seems to hold truer of mountains that are wrinkles in the earth's crust--squeezed up and crumpled stratified rock, such as most of the great mountain-systems are--than of mountains of erosion like the Catskills, or of upheaval like the Adirondacks. The crushed and folded and dislocated strata are laid open to the weather as the horizontal strata, and as the upheaved ma.s.ses of Archaean rock are not. Moreover, strata of unequal hardness are exposed, and this condition favors rapid erosion.