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,
