Travels in Alaska

While I was at Wrangell the chiefs and head men of the Stickeen tribe got up a grand dinner and entertainment in honor of their distinguished visitors, three doctors of divinity and their wives, fellow passengers on the steamer with me, whose object was to organize the Presbyterian church. To both the dinner and dances I was invited, was adopted by the Stickeen tribe, and given an Indian name (Ancoutahan) said to mean adopted chief. I was inclined to regard this honor as being unlikely to have any practical value, but I was assured by Mr. Vanderbilt, Mr. Young, and others that it would be a great safeguard while I was on my travels among the different tribes of the archipelago. For travelers without an Indian name might be killed and robbed without the offender being called to account as long as the crime was kept secret from the whites; but, being adopted by the Stickeens, no one belonging to the other tribes would dare attack me, knowing that the Stickeens would hold them responsible.

The dinner-tables were tastefully decorated with flowers, and the food and general arrangements were in good taste, but there was no trace of Indian dishes. It was mostly imported canned stuff served Boston fashion. After the dinner we assembled in Chief Shakes's large block-house and were entertained with lively examples of their dances and amusements, carried on with great spirit, making a very novel barbarous durbar. The dances seemed to me wonderfully like those of the American Indians in general, a monotonous stamping accompanied by hand-clapping, head-jerking, and explosive grunts kept in time to grim drum-beats. The chief dancer and leader scattered great quantities of downy feathers like a snowstorm as blessings on everybody, while all chanted, “Hee-ee-ah-ah, hee-ee-ah-ah,” jumping up and down until all were bathed in perspiration.

After the dancing excellent imitations were given of the gait, gestures, and behavior of several animals under different circumstances–walking, hunting, capturing, and devouring their prey, etc. While all were quietly seated, waiting to see what next was going to happen, the door of the big house was suddenly thrown open and in bounced a bear, so true to life in form and gestures we were all startled, though it was only a bear-skin nicely fitted on a man who was intimately acquainted with the animals and knew how to imitate them. The bear shuffled down into the middle of the floor and made the motion of jumping into a stream and catching a wooden salmon that was ready for him, carrying it out on to the bank, throwing his head around to listen and see if any one was coming, then tearing it to pieces, jerking his head from side to side, looking and listening in fear of hunters' rifles. Besides the bear dance, there were porpoise and deer dances with one of the party imitating the animals by stuffed specimens with an Indian inside, and the movements were so accurately imitated that they seemed the real thing.

These animal plays were followed by serious speeches, interpreted by an Indian woman: “Dear Brothers and Sisters, this is the way we used to dance. We liked it long ago when we were blind, we always danced this way, but now we are not blind. The Good Lord has taken pity upon us and sent his son, Jesus Christ, to tell us what to do. We have danced to-day only to show you how blind we were to like to dance in this foolish way. We will not dance any more.”

Another speech was interpreted as follows: “‘Dear Brothers and Sisters,’ the chief says, ‘this is else way we used to dance and play. We do not wish to do so any more. We will give away all the dance dresses you have seen us wearing, though we value them very highly.’ He says he feels much honored to have so many white brothers and sisters at our dinner and plays.”

Several short explanatory remarks were made all through the exercises by Chief Shakes, presiding with grave dignity. The last of his speeches concluded thus: “Dear Brothers and Sisters, we have been long, long in the dark. You have led us into strong guiding light and taught us the right way to live and the right way to die. I thank you for myself and all my people, and I give you my heart.”

At the close of the amusements there was a potlatch when robes made of the skins of deer, wild sheep, marmots, and sables were distributed, and many of the fantastic head-dresses that had been worn by Shamans. One of these fell to my share.

The floor of the house was strewn with fresh hemlock boughs, bunches of showy wild flowers adorned the walls, and the hearth was filled with huckleberry branches and epilobium. Altogether it was a wonderful show.

I have found southeastern Alaska a good, healthy country to live in. The climate of the islands and shores of the mainland is remarkably bland and temperate and free from extremes of either heat or cold throughout the year. It is rainy, however,–so much so that hay-making will hardly ever be extensively engaged in here, whatever the future may show in the way of the development of mines, forests, and fisheries. This rainy weather, however, is of good quality, the best of the kind I ever experienced, mild in temperature, mostly gentle in its fall, filling the fountains of the rivers and keeping the whole land fresh and fruitful, while anything more delightful than the shining weather in the midst of the rain, the great round sun-days of July and August, may hardly be found anywhere, north or south. An Alaska summer day is a day without night. In the Far North, at Point Barrow, the sun does not set for weeks, and even here in southeastern Alaska it is only a few degrees below the horizon at its lowest point, and the topmost colors of the sunset blend with those of the sunrise, leaving no gap of darkness between. Midnight is only a low noon, the middle point of the gloaming. The thin clouds that are almost always present are then colored yellow and red, making a striking advertisement of the sun's progress beneath the horizon. The day opens slowly. The low arc of light steals around to the northeastward with gradual increase of height and span and intensity of tone; and when at length the sun appears, it is without much of that stirring, impressive pomp, of flashing, awakening, triumphant energy, suggestive of the Bible imagery, a bridegroom coming out of his chamber and rejoicing like a strong man to run a race. The red clouds with yellow edges dissolve in hazy dimness; the islands, with grayish-white ruffs of mist about them, cast ill-defined shadows on the glistening waters, and the whole down-bending firmament becomes pearl-gray. For three or four hours after sunrise there is nothing especially impressive in the landscape. The sun, though seemingly unclouded, may almost be looked in the face, and the islands and mountains, with their wealth of woods and snow and varied beauty of architecture, seem comparatively sleepy and uncommunicative.

As the day advances toward high noon, the sun-flood streaming through the damp atmosphere lights the water levels and the sky to glowing silver. Brightly play the ripples about the bushy edges of the islands and on the plume-shaped streaks between them, ruffled by gentle passing wind-currents. The warm air throbs and makes itself felt as a life-giving, energizing ocean, embracing all the landscape, quickening the imagination, and bringing to mind the life and motion about us–the tides, the rivers, the flood of light streaming through the satiny sky; the marvelous abundance of fishes feeding in the lower ocean; the misty flocks of insects in the air; wild sheep and goats on a thousand grassy ridges; beaver and mink far back on many a rushing stream; Indians floating and basking along the shores; leaves and crystals drinking the sunbeams; and glaciers on the mountains, making valleys and basins for new rivers and lakes and fertile beds of soil.

Through the afternoon, all the way down to the sunset, the day grows in beauty. The light seems to thicken and become yet more generously fruitful without losing its soft mellow brightness. Everything seems to settle into conscious repose. The winds breathe gently or are wholly at rest. The few clouds visible are downy and luminous and combed out fine on the edges. Gulls here and there, winnowing the air on easy wing, are brought into striking relief; and every stroke of the paddles of Indian hunters in their canoes is told by a quick, glancing flash. Bird choirs in the grove are scarce heard as they sweeten the brooding stillness; and the sky, land, and water meet and blend in one inseparable scene of enchantment. Then comes the sunset with its purple and gold, not a narrow arch on the horizon, but oftentimes filling all the sky. The level cloud-bars usually present are fired on the edges, and the spaces of clear sky between them are greenish-yellow or pale amber, while the orderly flocks of small overlapping clouds, often seen higher up, are mostly touched with crimson like the out-leaning sprays of maple-groves in the beginning of an Eastern Indian Summer. Soft, mellow purple flushes the sky to the zenith and fills the air, fairly steeping and transfiguring the islands and making all the water look like wine. After the sun goes down, the glowing gold vanishes, but because it descends on a curve nearly in the same plane with the horizon, the glowing portion of the display lasts much longer than in more southern latitudes, while the upper colors with gradually lessening intensity of tone sweep around to the north, gradually increase to the eastward, and unite with those of the morning.

The most extravagantly colored of all the sunsets I have yet seen in Alaska was one I enjoyed on the voyage from Portland to Wrangell, when we were in the midst of one of the most thickly islanded parts of the Alexander Archipelago. The day had been showery, but late in the afternoon the clouds melted away from the west, all save a few that settled down in narrow level bars near the horizon. The evening was calm and the sunset colors came on gradually, increasing in extent and richness of tone by slow degrees as if requiring more time than usual to ripen. At a height of about thirty degrees there was a heavy cloud-bank, deeply reddened on its lower edge and the projecting parts of its face. Below this were three horizontal belts of purple edged with gold, while a vividly defined, spreading fan of flame streamed upward across the purple bars and faded in a feather edge of dull red. But beautiful and impressive as was this painting on the sky, the most novel and exciting effect was in the body of the atmosphere itself, which, laden with moisture, became one mass of color–a fine translucent purple haze in which the islands with softened outlines seemed to float, while a dense red ring lay around the base of each of them as a fitting border. The peaks, too, in the distance, and the snow-fields and glaciers and fleecy rolls of mist that lay in the hollows, were flushed with a deep, rosy alpenglow of ineffable loveliness. Everything near and far, even the ship, was comprehended in the glorious picture and the general color effect. The mission divines we had aboard seemed then to be truly divine as they gazed transfigured in the celestial glory. So also seemed our bluff, storm-fighting old captain, and his tarry sailors and all.

About one third of the summer days I spent in the Wrangell region were cloudy with very little or no rain, one third decidedly rainy, and one third clear. According to a record kept here of a hundred and forty-seven days beginning May 17 of that year, there were sixty-five on which rain fell, forty-three cloudy with no rain, and thirty-nine clear. In June rain fell on eighteen days, in July eight days, in August fifteen days, in September twenty days. But on some of these days there was only a few minutes' rain, light showers scarce enough to count, while as a general thing the rain fell so gently and the temperature was so mild, very few of them could be called stormy or dismal; even the bleakest, most bedraggled of them all usually had a flush of late or early color to cheer them, or some white illumination about the noon hours. I never before saw so much rain fall with so little noise. None of the summer winds make roaring storms, and thunder is seldom heard. I heard none at all. This wet, misty weather seems perfectly healthful. There is no mildew in the houses, as far as I have seen, or any tendency toward mouldiness in nooks hidden from the sun; and neither among the people nor the plants do we find anything flabby or dropsical.

In September clear days were rare, more than three fourths of them were either decidedly cloudy or rainy, and the rains of this month were, with one wild exception, only moderately heavy, and the clouds between showers drooped and crawled in a ragged, unsettled way without betraying hints of violence such as one often sees in the gestures of mountain storm-clouds.

July was the brightest month of the summer, with fourteen days of sunshine, six of them in uninterrupted succession, with a temperature at 7 A.M. of about 60°, at 12 M., 70°. The average 7 A.M. temperature for June was 54.3°; the average 7 A.M. temperature for July was 55.3°; at 12 M. the average temperature was 61.45°; the average 7 A.M. temperature for August was 54.12°; 12 M., 61.48°; the average 7 A.M. temperature for September was 52.14°; and 12 M., 56.12°.

The highest temperature observed here during the summer was seventy-six degrees. The most remarkable characteristic of this summer weather, even the brightest of it, is the velvet softness of the atmosphere. On the mountains of California, throughout the greater part of the year, the presence of an atmosphere is hardly recognized, and the thin, white, bodiless light of the morning comes to the peaks and glaciers as a pure spiritual essence, the most impressive of all the terrestrial manifestations of God. The clearest of Alaskan air is always appreciably substantial, so much so that it would seem as if one might test its quality by rubbing it between the thumb and finger. I never before saw summer days so white and so full of subdued lustre.

The winter storms, up to the end of December when I left Wrangell, were mostly rain at a temperature of thirty-five or forty degrees, with strong winds which sometimes roughly lash the shores and carry scud far into the woods. The long nights are then gloomy enough and the value of snug homes with crackling yellow cedar fires may be finely appreciated. Snow falls frequently, but never to any great depth or to lie long. It is said that only once since the settlement of Fort Wrangell has the ground been covered to a depth of four feet. The mercury seldom falls more than five or six degrees below the freezing-point, unless the wind blows steadily from the mainland. Back from the coast, however, beyond the mountains, the winter months are very cold. On the Stickeen River at Glenora, less than a thousand feet above the level of the sea, a temperature of from thirty to forty degrees below zero is not uncommon.

Chapter IV

The Stickeen River

The most interesting of the short excursions we made from Fort Wrangell was the one up the Stickeen River to the head of steam navigation. From Mt. St. Elias the coast range extends in a broad, lofty chain beyond the southern boundary of the territory, gashed by stupendous cañons, each of which carries a lively river, though most of them are comparatively short, as their highest sources lie in the icy solitudes of the range within forty or fifty miles of the coast. A few, however, of these foaming, roaring streams–the Alsek, Chilcat, Chilcoot, Taku, Stickeen, and perhaps others–head beyond the range with some of the southwest branches of the Mackenzie and Yukon.

The largest side branches of the main-trunk cañons of all these mountain streams are still occupied by glaciers which descend in showy ranks, their messy, bulging snouts lying back a little distance in the shadows of the walls, or pushing forward among the cotton-woods that line the banks of the rivers, or even stretching all the way across the main cañons, compelling the rivers to find a channel beneath them.

The Stickeen was, perhaps, the best known of the rivers that cross the Coast Range, because it was the best way to the Mackenzie River Cassiar gold-mines. It is about three hundred and fifty miles long, and is navigable for small steamers a hundred and fifty miles to Glenora, and sometimes to Telegraph Creek, fifteen miles farther. It first pursues a westerly course through grassy plains darkened here and there with groves of spruce and pine; then, curving southward and receiving numerous tributaries from the north, it enters the Coast Range, and sweeps across it through a magnificent cañon three thousand to five thousand feet deep, and more than a hundred miles long. The majestic cliffs and mountains forming the cañon walls display endless variety of form and sculpture, and are wonderfully adorned and enlivened with glaciers and waterfalls, while throughout almost its whole extent the floor is a flowery landscape garden, like Yosemite. The most striking features are the glaciers, hanging over the cliffs, descending the side cañons and pushing forward to the river, greatly enhancing the wild beauty of all the others.

Gliding along the swift-flowing river, the views change with bewildering rapidity. Wonderful, too, are the changes dependent on the seasons and the weather. In spring, when the snow is melting fast, you enjoy the countless rejoicing waterfalls; the gentle breathing of warm winds; the colors of the young leaves and flowers when the bees are busy and wafts of fragrance are drifting hither and thither from miles of wild roses, clover, and honeysuckle; the swaths of birch and willow on the lower slopes following the melting of the winter avalanche snow-banks; the bossy cumuli swelling in white and purple piles above the highest peaks; gray rain-clouds wreathing the outstanding brows and battlements of the walls; and the breaking-forth of the sun after the rain; the shining of the leaves and streams and crystal architecture of the glaciers; the rising of fresh fragrance; the song of the happy birds; and the serene color-grandeur of the morning and evening sky. In summer you find the groves and gardens in full dress; glaciers melting rapidly under sunshine and rain; waterfalls in all their glory; the river rejoicing in its strength; young birds trying their wings; bears enjoying salmon and berries; all the life of the cañon brimming full like the streams. In autumn comes rest, as if the year's work were done. The rich hazy sunshine streaming over the cliffs calls forth the last of the gentians and goldenrods; the groves and thickets and meadows bloom again as their leaves change to red and yellow petals; the rocks also, and the glaciers, seem to bloom like the plants in the mellow golden light. And so goes the song, change succeeding change in sublime harmony through all the wonderful seasons and weather.

My first trip up the river was made in the spring with the missionary party soon after our arrival at Wrangell. We left Wrangell in the afternoon and anchored for the night above the river delta, and started up the river early next morning when the heights above the “Big Stickeen” Glacier and the smooth domes and copings and arches of solid snow along the tops of the cañon walls were glowing in the early beams. We arrived before noon at the old trading-post called “Buck's” in front of the Stickeen Glacier, and remained long enough to allow the few passengers who wished a nearer view to cross the river to the terminal moraine. The sunbeams streaming through the ice pinnacles along its terminal wall produced a wonderful glory of color, and the broad, sparkling crystal prairie and the distant snowy fountains were wonderfully attractive and made me pray for opportunity to explore them.

Of the many glaciers, a hundred or more, that adorn the walls of the great Stickeen River Cañon, this is the largest. It draws its sources from snowy mountains within fifteen or twenty miles of the coast, pours through a comparatively narrow cañon about two miles in width in a magnificent cascade, and expands in a broad fan five or six miles in width, separated from the Stickeen River by its broad terminal moraine, fringed with spruces and willows. Around the beautifully drawn curve of the moraine the Stickeen River flows, having evidently been shoved by the glacier out of its direct course. On the opposite side of the cañon another somewhat smaller glacier, which now terminates four or five miles from the river, was once united front to front with the greater glacier, though at first both were tributaries of the main Stickeen Glacier which once filled the whole grand cañon. After the main trunk cañon was melted out, its side branches, drawing their sources from a height of three or four to five or six thousand feet, were cut off, and of course became separate glaciers, occupying cirques and branch cañons along the tops and sides of the walls. The Indians have a tradition that the river used to run through a tunnel under the united fronts of the two large tributary glaciers mentioned above, which entered the main cañon from either side; and that on one occasion an Indian, anxious to get rid of his wife, had her sent adrift in a canoe down through the ice tunnel, expecting that she would trouble him no more. But to his surprise she floated through under the ice in safety. All the evidence connected with the present appearance of these two glaciers indicates that they were united and formed a dam across the river after the smaller tributaries had been melted off and had receded to a greater or lesser height above the valley floor.

The big Stickeen Glacier is hardly out of sight ere you come upon another that pours a majestic crystal flood through the evergreens, while almost every hollow and tributary cañon contains a smaller one, the size, of course, varying with the extent of the area drained. Some are like mere snow-banks; others, with the blue ice apparent, depend in massive bulging curves and swells, and graduate into the river-like forms that maze through the lower forested regions and are so striking and beautiful that they are admired even by the passing miners with gold-dust in their eyes.

Thirty-five miles above the Big Stickeen Glacier is the “Dirt Glacier,” the second in size. Its outlet is a fine stream, abounding in trout. On the opposite side of the river there is a group of five glaciers, one of them descending to within a hundred feet of the river.

Near Glenora, on the northeastern flank of the main Coast Range, just below a narrow gorge called “The Cañon,” terraces first make their appearance, where great quantities of moraine material have been swept through the flood-choked gorge and of course outspread and deposited on the first open levels below. Here, too, occurs a marked change in climate and consequently in forests and general appearance of the face of the country. On account of destructive fires the woods are younger and are composed of smaller trees about a foot to eighteen inches in diameter and seventy-five feet high, mostly two-leaved pines which hold their seeds for several years after they are ripe. The woods here are without a trace of those deep accumulations of mosses, leaves, and decaying trunks which make so damp and unclearable mass in the coast forests. Whole mountain-sides are covered with gray moss and lichens where the forest has been utterly destroyed. The river-bank cottonwoods are also smaller, and the birch and contorta pines mingle freely with the coast hemlock and spruce. The birch is common on the lower slopes and is very effective, its round, leafy, pale-green head contrasting with the dark, narrow spires of the conifers and giving a striking character to the forest. The “tamarac pine” or black pine, as the variety of P. contorta is called here, is yellowish-green, in marked contrast with the dark lichen-draped spruce which grows above the pine at a height of about two thousand feet, in groves and belts where it has escaped fire and snow avalanches. There is another handsome spruce hereabouts, Picea alba, very slender and graceful in habit, drooping at the top like a mountain hemlock. I saw fine specimens a hundred and twenty-five feet high on deep bottom land a few miles below Glenora. The tops of some of them were almost covered with dense clusters of yellow and brown cones.

We reached the old Hudson's Bay trading-post at Glenora about one o'clock, and the captain informed me that he would stop here until the next morning, when he would make an early start for Wrangell.