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Preface
Forty years ago John Muir wrote to a friend; “I am hopelessly and forever a mountaineer. . . . Civilization and fever, and all the morbidness that has been hooted at me, have not dimmed my glacial eyes, and I care to live only to entice people to look at Nature's loveliness.” How gloriously he fulfilled the promise of his early manhood! Fame, all unbidden, wore a path to his door, but he always remained a modest, unspoiled mountaineer. Kindred spirits, the greatest of his time, sought him out, even in his mountain cabin, and felt honored by his friendship. Ralph Waldo Emerson urged him to visit Concord and rest awhile from the strain of his solitary studies in the Sierra Nevada. But nothing could dislodge him from the glacial problems of the high Sierra; with passionate interest he kept at his task. “The grandeur of these forces and their glorious results,” he once wrote, “overpower me and inhabit my whole being. Waking or sleeping, I have no rest. In dreams I read blurred sheets of glacial writing, or follow lines of cleavage, or struggle with the difficulties of some extraordinary rock-form.”
There is a note of pathos, the echo of an unfulfilled hope, in the record of his later visit to Concord. “It was seventeen years after our parting on Wawona ridge that I stood beside his [Emerson's] grave under a pine tree on the hill above Sleepy Hollow. He had gone to higher Sierras, and, as I fancied, was again waving his hand in friendly recognition.” And now John Muir has followed his friend of other days to the “higher Sierras.” His earthly remains lie among trees planted by his own hand. To the pine tree of Sleepy Hollow answers a guardian sequoia in the sunny Alhambra Valley.
In 1879 John Muir went to Alaska for the first time. Its stupendous living glaciers aroused his unbounded interest, for they enabled him to verify his theories of glacial action. Again and again he returned to this continental laboratory of landscapes. The greatest of the tide-water glaciers appropriately commemorates his name. Upon this book of Alaska travels, all but finished before his unforeseen departure, John Muir expended the last months of his life. It was begun soon after his return from Africa in 1912. His eager leadership of the ill-fated campaign to save his beloved Hetch-Hetchy Valley from commercial destruction seriously interrupted his labors. Illness, also, interposed some checks as he worked with characteristic care and thoroughness through the great mass of Alaska notes that had accumulated under his hands for more than thirty years.
The events recorded in this volume end in the middle of the trip of 1890. Muir's notes on the remainder of the journey have not been found, and it is idle to speculate how he would have concluded the volume if he had lived to complete it. But no one will read the fascinating description of the Northern Lights without feeling a poetical appropriateness in the fact that his last work ends with a portrayal of the auroras–one of those phenomena which elsewhere he described as “the most glorious of all the terrestrial manifestations of God.”
Muir's manuscripts bear on every page impressive evidence of the pains he took in his literary work, and the lofty standard he set himself in his scientific studies. The counterfeiting of a fact or of an experience was a thing unthinkable in connection with John Muir. He was tireless in pursuing the meaning of a physiographical fact, and his extraordinary physical endurance usually enabled him to trail it to its last hiding-place. Often, when telling the tale of his adventures in Alaska, his eyes would kindle with youthful enthusiasm, and he would live over again the red-blooded years that yielded him “shapeless harvests of revealed glory.”
For a number of months just prior to his death he had the friendly assistance of Mrs. Marion Randall Parsons. Her familiarity with the manuscript, and with Mr. Muir's expressed and penciled intentions of revision and arrangement, made her the logical person to prepare it in final form for publication. It was a task to which she brought devotion as well as ability. The labor involved was the greater in order that the finished work might exhibit the last touches of Muir's master-hand, and yet contain nothing that did not flow from his pen. All readers of this book will feel grateful for her labor of love.
I add these prefatory lines to the work of my departed friend with pensive misgiving, knowing that he would have deprecated any discharge of musketry over his grave. His daughters, Mrs. Thomas Rea Hanna and Mrs. Buel Alvin Funk, have honored me with the request to transmit the manuscript for publication, and later to consider with them what salvage may be made from among their father's unpublished writings. They also wish me to express their grateful acknowledgments to Houghton Mifflin Company, with whom John Muir has always maintained close and friendly relations.
William Frederic Badè.Berkeley, California, May, 1915.Part I
The Trip of 1879
Chapter I
Puget Sound and British Columbia
After eleven years of study and exploration in the Sierra Nevada of California and the mountain-ranges of the Great Basin, studying in particular their glaciers, forests, and wild life, above all their ancient glaciers and the influence they exerted in sculpturing the rocks over which they passed with tremendous pressure, making new landscapes, scenery, and beauty which so mysteriously influence every human being, and to some extent all life, I was anxious to gain some knowledge of the regions to the northward, about Puget Sound and Alaska. With this grand object in view I left San Francisco in May, 1879, on the steamer Dakota, without any definite plan, as with the exception of a few of the Oregon peaks and their forests all the wild north was new to me.
To the mountaineer a sea voyage is a grand, inspiring, restful change. For forests and plains with their flowers and fruits we have new scenery, new life of every sort; water hills and dales in eternal visible motion for rock waves, types of permanence.
It was curious to note how suddenly the eager countenances of the passengers were darkened as soon as the good ship passed through the Golden Gate and began to heave on the waves of the open ocean. The crowded deck was speedily deserted on account of seasickness. It seemed strange that nearly every one afflicted should be more or less ashamed.
Next morning a strong wind was blowing, and the sea was gray and white, with long breaking waves, across which the Dakota was racing half-buried in spray. Very few of the passengers were on deck to enjoy the wild scenery. Every wave seemed to be making enthusiastic, eager haste to the shore, with long, irised tresses streaming from its tops, some of its outer fringes borne away in scud to refresh the wind, all the rolling, pitching, flying water exulting in the beauty of rainbow light. Gulls and albatrosses, strong, glad life in the midst of the stormy beauty, skimmed the waves against the wind, seemingly without effort, oftentimes flying nearly a mile without a single wing-beat, gracefully swaying from side to side and tracing the curves of the briny water hills with the finest precision, now and then just grazing the highest.
And yonder, glistening amid the irised spray, is still more striking revelation of warm life in the so-called howling waste,–a half-dozen whales, their broad backs like glaciated bosses of granite heaving aloft in near view, spouting lustily, drawing a long breath, and plunging down home in colossal health and comfort. A merry school of porpoises, a square mile of them, suddenly appear, tossing themselves into the air in abounding strength and hilarity, adding foam to the waves and making all the wilderness wilder. One cannot but feel sympathy with and be proud of these brave neighbors, fellow citizens in the commonwealth of the world, making a living like the rest of us. Our good ship also seemed like a thing of life, its great iron heart beating on through calm and storm, a truly noble spectacle. But think of the hearts of these whales, beating warm against the sea, day and night, through dark and light, on and on for centuries; how the red blood must rush and gurgle in and out, bucketfuls, barrelfuls at a beat!
The cloud colors of one of the four sunsets enjoyed on the voyage were remarkably pure and rich in tone. There was a well-defined range of cumuli a few degrees above the horizon, and a massive, dark-gray rain-cloud above it, from which depended long, bent fringes overlapping the lower cumuli and partially veiling them; and from time to time sunbeams poured through narrow openings and painted the exposed bosses and fringes in ripe yellow tones, which, with the reflections on the water, made magnificent pictures. The scenery of the ocean, however sublime in vast expanse, seems far less beautiful to us dry-shod animals than that of the land seen only in comparatively small patches; but when we contemplate the whole globe as one great dewdrop, striped and dotted with continents and islands, flying through space with other stars all singing and shining together as one, the whole universe appears as an infinite storm of beauty.
The California coast-hills and cliffs look bare and uninviting as seen from the ship, the magnificent forests keeping well back out of sight beyond the reach of the sea winds; those of Oregon and Washington are in some places clad with conifers nearly down to the shore; even the little detached islets, so marked a feature to the northward, are mostly tree-crowned. Up through the Straits of Juan de Fuca the forests, sheltered from the ocean gales and favored with abundant rains, flourish in marvelous luxuriance on the glacier-sculptured mountains of the Olympic Range.
We arrived in Esquimault Harbor, three miles from Victoria, on the evening of the fourth day, and drove to the town through a magnificent forest of Douglas spruce,–with an undergrowth in open spots of oak, madrone, hazel, dogwood, alder, spiræa, willow, and wild rose,–and around many an upswelling moutonné rock, freshly glaciated and furred with yellow mosses and lichens.
Victoria, the capital of British Columbia, was in 1879 a small old-fashioned English town on the south end of Vancouver Island. It was said to contain about six thousand inhabitants. The government buildings and some of the business blocks were noticeable, but the attention of the traveler was more worthily attracted to the neat cottage homes found here, embowered in the freshest and floweriest climbing roses and honeysuckles conceivable. Californians may well be proud of their home roses loading sunny verandas, climbing to the tops of the roofs and falling over the gables in white and red cascades. But here, with so much bland fog and dew and gentle laving rain, a still finer development of some of the commonest garden plants is reached. English honeysuckle seems to have found here a most congenial home. Still more beautiful were the wild roses, blooming in wonderful luxuriance along the woodland paths, with corollas two and three inches wide. This rose and three species of spiræa fairly filled the air with fragrance after showers; and how brightly then did the red dogwood berries shine amid the green leaves beneath trees two hundred and fifty feet high.
Strange to say, all of this exuberant forest and flower vegetation was growing upon fresh moraine material scarcely at all moved or in any way modified by post-glacial agents. In the town gardens and orchards, peaches and apples fell upon glacier-polished rocks, and the streets were graded in moraine gravel; and I observed scratched and grooved rock bosses as unweathered and telling as those of the High Sierra of California eight thousand feet or more above sea-level. The Victoria Harbor is plainly glacial in origin, eroded from the solid; and the rock islets that rise here and there in it are unchanged to any appreciable extent by all the waves that have broken over them since first they came to light toward the close of the glacial period. The shores also of the harbor are strikingly grooved and scratched and in every way as glacial in all their characteristics as those of new-born glacial lakes. That the domain of the sea is being slowly extended over the land by incessant wave-action is well known; but in this freshly glaciated region the shores have been so short a time exposed to wave-action that they are scarcely at all wasted. The extension of the sea affected by its own action in post-glacial times is probably less than the millionth part of that affected by glacial action during the last glacier period. The direction of the flow of the ice-sheet to which all the main features of this wonderful region are due was in general southward.
From this quiet little English town I made many short excursions–up the coast to Nanaimo, to Burrard Inlet, now the terminus of the Canadian Pacific Railroad, to Puget Sound, up Fraser River to New Westminster and Yale at the head of navigation, charmed everywhere with the wild, new-born scenery. The most interesting of these and the most difficult to leave was the Puget Sound region, famous the world over for the wonderful forests of gigantic trees about its shores. It is an arm and many-fingered hand of the sea, reaching southward from the Straits of Juan de Fuca about a hundred miles into the heart of one of the noblest coniferous forests on the face of the globe. All its scenery is wonderful–broad river-like reaches sweeping in beautiful curves around bays and capes and jutting promontories, opening here and there into smooth, blue, lake-like expanses dotted with islands and feathered with tall, spiry evergreens, their beauty doubled on the bright mirror-water.
Sailing from Victoria, the Olympic Mountains are seen right ahead, rising in bold relief against the sky, with jagged crests and peaks from six to eight thousand feet high,–small residual glaciers and ragged snow-fields beneath them in wide amphitheatres opening down through the forest-filled valleys. These valleys mark the courses of the Olympic glaciers at the period of their greatest extension, when they poured their tribute into that portion of the great northern ice-sheet that overswept Vancouver Island and filled the strait between it and the mainland.
On the way up to Olympia, then a hopeful little town situated at the end of one of the longest fingers of the Sound, one is often reminded of Lake Tahoe, the scenery of the widest expanses is so lake-like in the clearness and stillness of the water and the luxuriance of the surrounding forests. Doubling cape after cape, passing uncounted islands, new combinations break on the view in endless variety, sufficient to satisfy the lover of wild beauty through a whole life. When the clouds come down, blotting out everything, one feels as if at sea; again lifting a little, some islet may be seen standing alone with the tops of its trees dipping out of sight in gray misty fringes; then the ranks of spruce and cedar bounding the water's edge come to view; and when at length the whole sky is clear the colossal cone of Mt. Rainier may be seen in spotless white, looking down over the dark woods from a distance of fifty or sixty miles, but so high and massive and so sharply outlined, it seems to be just back of a strip of woods only a few miles wide.
Mt. Rainier, or Tahoma (the Indian name), is the noblest of the volcanic cones extending from Lassen Butte and Mt. Shasta along the Cascade Range to Mt. Baker. One of the most telling views of it hereabouts is obtained near Tacoma. From a bluff back of the town it was revealed in all its glory, laden with glaciers and snow down to the forested foothills around its finely curved base. Up to this time (1879) it had been ascended but once. From observations made on the summit with a single aneroid barometer, it was estimated to be about 14,500 feet high. Mt. Baker, to the northward, is about 10,700 feet high, a noble mountain. So also are Mt. Adams, Mt. St. Helens, and Mt. Hood. The latter, overlooking the town of Portland, is perhaps the best known. Rainier, about the same height as Shasta, surpasses them all in massive icy grandeur,–the most majestic solitary mountain I had ever yet beheld. How eagerly I gazed and longed to climb it and study its history only the mountaineer may know, but I was compelled to turn away and bide my time.
The species forming the bulk of the woods here is the Douglas spruce (Pseudotsuga douglasii), one of the greatest of the western giants. A specimen that I measured near Olympia was about three hundred feet in height and twelve feet in diameter four feet above the ground. It is a widely distributed tree, extending northward through British Columbia, southward through Oregon and California, and eastward to the Rocky Mountains. The timber is used for shipbuilding, spars, piles, and the framework of houses, bridges, etc. In the California lumber markets it is known as “Oregon pine.” In Utah, where it is common on the Wahsatch Mountains, it is called “red pine.” In California, on the western slope of the Sierra Nevada, it forms, in company with the yellow pine, sugar pine, and incense cedar, a pretty well-defined belt at a height of from three to six thousand feet above the sea; but it is only in Oregon and Washington, especially in this Puget Sound region, that it reaches its very grandest development,–tall, straight, and strong, growing down close to tidewater.
All the towns of the Sound had a hopeful, thrifty aspect. Port Townsend, picturesquely located on a grassy bluff, was the port of clearance for vessels sailing to foreign parts. Seattle was famed for its coal-mines, and claimed to be the coming town of the North Pacific Coast. So also did its rival, Tacoma, which had been selected as the terminus of the much-talked-of Northern Pacific Railway. Several coal-veins of astonishing thickness were discovered the winter before on the Carbon River, to the east of Tacoma, one of them said to be no less than twenty-one feet, another twenty feet, another fourteen, with many smaller ones, the aggregate thickness of all the veins being upwards of a hundred feet. Large deposits of magnetic iron ore and brown hematite, together with limestone, had been discovered in advantageous proximity to the coal, making a bright outlook for the Sound region in general in connection with its railroad hopes, its unrivaled timber resources, and its far-reaching geographical relations.
After spending a few weeks in the Puget Sound with a friend from San Francisco, we engaged passage on the little mail steamer California, at Portland, Oregon, for Alaska. The sail down the broad lower reaches of the Columbia and across its foamy bar, around Cape Flattery, and up the Juan de Fuca Strait, was delightful; and after calling again at Victoria and Port Townsend we got fairly off for icy Alaska.
Chapter II
Alexander Archipelago and the Home I found in Alaska
To the lover of pure wildness Alaska is one of the most wonderful countries in the world. No excursion that I know of may be made into any other American wilderness where so marvelous an abundance of noble, newborn scenery is so charmingly brought to view as on the trip through the Alexander Archipelago to Fort Wrangell and Sitka. Gazing from the deck of the steamer, one is borne smoothly over calm blue waters, through the midst of countless forest-clad islands. The ordinary discomforts of a sea voyage are not felt, for nearly all the whole long way is on inland waters that are about as waveless as rivers and lakes. So numerous are the islands that they seem to have been sown broadcast; long tapering vistas between the largest of them open in every direction.
Day after day in the fine weather we enjoyed, we seemed to float in true fairyland, each succeeding view seeming more and more beautiful, the one we chanced to have before us the most surprisingly beautiful of all. Never before this had I been embosomed in scenery so hopelessly beyond description. To sketch picturesque bits, definitely bounded, is comparatively easy–a lake in the woods, a glacier meadow, or a cascade in its dell; or even a grand master view of mountains beheld from some commanding outlook after climbing from height to height above the forests. These may be attempted, and more or less telling pictures made of them; but in these coast landscapes there is such indefinite, on-leading expansiveness, such a multitude of features without apparent redundance, their lines graduating delicately into one another in endless succession, while the whole is so fine, so tender, so ethereal, that all pen-work seems hopelessly unavailing. Tracing shining ways through fiord and sound, past forests and waterfalls, islands and mountains and far azure headlands, it seems as if surely we must at length reach the very paradise of the poets, the abode of the blessed.
Some idea of the wealth of this scenery may be gained from the fact that the coast-line of Alaska is about twenty-six thousand miles long, more than twice as long as all the rest of the United States. The islands of the Alexander Archipelago, with the straits, channels, canals, sounds, passages, and fiords, form an intricate web of land and water embroidery sixty or seventy miles wide, fringing the lofty icy chain of coast mountains from Puget Sound to Cook Inlet; and, with infinite variety, the general pattern is harmonious throughout its whole extent of nearly a thousand miles. Here you glide into a narrow channel hemmed in by mountain walls, forested down to the water's edge, where there is no distant view, and your attention is concentrated on the objects close about you–the crowded spires of the spruces and hemlocks rising higher and higher on the steep green slopes; stripes of paler green where winter avalanches have cleared away the trees, allowing grasses and willows to spring up; zigzags of cascades appearing and disappearing among the bushes and trees; short, steep glens with brawling streams hidden beneath alder and dogwood, seen only where they emerge on the brown algæ of the shore; and retreating hollows, with lingering snow-banks marking the fountains of ancient glaciers. The steamer is often so near the shore that you may distinctly see the cones clustered on the tops of the trees, and the ferns and bushes at their feet.
But new scenes are brought to view with magical rapidity. Rounding some bossy cape, the eye is called away into far-reaching vistas, bounded on either hand by headlands in charming array, one dipping gracefully beyond another and growing fainter and more ethereal in the distance. The tranquil channel stretching river-like between, may be stirred here and there by the silvery plashing of upspringing salmon, or by flocks of white gulls floating like water-lilies among the sun spangles; while mellow, tempered sunshine is streaming over all, blending sky, land, and water in pale, misty blue. Then, while you are dreamily gazing into the depths of this leafy ocean lane, the little steamer, seeming hardly larger than a duck, turning into some passage not visible until the moment of entering it, glides into a wide expanse–a sound filled with islands, sprinkled and clustered in forms and compositions such as nature alone can invent; some of them so small the trees growing on them seem like single handfuls culled from the neighboring woods and set in the water to keep them fresh, while here and there at wide intervals you may notice bare rocks just above the water, mere dots punctuating grand, outswelling sentences of islands.
The variety we find, both as to the contours and the collocation of the islands, is due chiefly to differences in the structure and composition of their rocks, and the unequal glacial denudation different portions of the coast were subjected to. This influence must have been especially heavy toward the end of the glacial period, when the main ice-sheet began to break up into separate glaciers. Moreover, the mountains of the larger islands nourished local glaciers, some of them of considerable size, which sculptured their summits and sides, forming in some cases wide cirques with cañons or valleys leading down from them into the channels and sounds. These causes have produced much of the bewildering variety of which nature is so fond, but none the less will the studious observer see the underlying harmony–the general trend of the islands in the direction of the flow of the main ice-mantle from the mountains of the Coast Range, more or less varied by subordinate foothill ridges and mountains. Furthermore, all the islands, great and small, as well as the headlands and promontories of the mainland, are seen to have a rounded, over-rubbed appearance produced by the over-sweeping ice-flood during the period of greatest glacial abundance.