LITMIR.BIZ

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groves of spruce and pine are bowed down as by a gentle hand and put to rest, not again to see the light or move leaf or limb until the grand awakening of the springtime, while the larger animals and most of the birds seek food and shelter in the foothills on the borders of the valleys and plains.

      The lofty volcanic peaks are yet more heavily snow-laden. To their upper zones no summer comes. They are white always. From the steep slopes of the summit the new-fallen snow, while yet dry and loose, descends in magnificent avalanches to feed the glaciers, making meanwhile the most glorious manifestations of power. Happy is the man who may get near them to see and hear. In some sheltered camp nest on the edge of the timberline one may lie snug and warm, but after the long shuffle on snowshoes we may have to wait more than a month ere the heavens open and the grand show is unveiled. In the mean time, bread may be scarce, unless with careful forecast a sufficient supply has been provided and securely placed during the summer. Nevertheless, to be thus deeply snowbound high in the sky is not without generous compensation for all the cost. And when we at length go down the long white slopes to the levels of civilization, the pains vanish like snow in sunshine, while the noble and exalting pleasures we have gained remain with us to enrich our lives forever.

      The fate of the high-flying mountain snow-flowers is a fascinating study, though little may we see of their works and ways while their storms go on. The glinting, swirling swarms fairly thicken the blast, and all the air, as well as the rocks and trees, is as one smothering mass of bloom, through the midst of which at close intervals come the low, intense thunder-tones of the avalanches as they speed on their way to fill the vast fountain hollows. Here they seem at last to have found rest. But this rest is only apparent. Gradually the loose crystals by the pressure of their own weight are welded together into clear ice, and, as glaciers, march steadily, silently on, with invisible motion, in broad, deep currents, grinding their way with irresistible energy to the warmer lowlands, where they vanish in glad, rejoicing streams.

      In the sober weather of Oregon lightning makes but little show. Those magnificent thunderstorms that so frequently adorn and glorify the sky of the Mississippi Valley are wanting here. Dull thunder and lightning may occasionally be seen and heard, but the imposing grandeur of great storms marching over the landscape with streaming banners and a network of fire is almost wholly unknown.

      Crossing the Cascade Range, we pass from a green to a gray country, from a wilderness of trees to a wilderness of open plains, level or rolling or rising here and there into hills and short mountain spurs. Though well supplied with rivers in most of its main sections, it is generally dry. The annual rainfall is only from about five to fifteen inches, and the thin winter garment of snow seldom lasts more than a month or two, though the temperature in many places falls from five to twenty-five degrees below zero for a short time. That the snow is light over eastern Oregon, and the average temperature not intolerably severe, is shown by the fact that large droves of sheep, cattle, and horses live there through the winter without other food or shelter than they find for themselves on the open plains or down in the sunken valleys and gorges along the streams.

      When we read of the mountain ranges of Oregon and Washington with detailed descriptions of their old volcanoes towering snow-laden and glacier-laden above the clouds, one may be led to imagine that the country is far icier and whiter and more mountainous than it is. Only in winter are the Coast and Cascade Mountains covered with snow. Then as seen from the main interior valleys they appear as comparatively low, bossy walls stretching along the horizon and making a magnificent display of their white wealth. The Coast Range in Oregon does not perhaps average more than three thousand feet in height. Its snow does not last long, most of its soil is fertile all the way to the summits, and the greater part of the range may at some time be brought under cultivation. The immense deposits on the great central uplift of the Cascade Range are mostly melted off before the middle of summer by the comparatively warm winds and rains from the coast, leaving only a few white spots on the highest ridges, where the depth from drifting has been greatest, or where the rate of waste has been diminished by specially favorable conditions as to exposure. Only the great volcanic cones are truly snow-clad all the year, and these are not numerous and make but a small portion of the general landscape.

      As we approach Oregon from the coast in summer, no hint of snowy mountains can be seen, and it is only after we have sailed into the country by the Columbia, or climbed some one of the commanding summits, that the great white peaks send us greeting and make telling advertisements of themselves and of the country over which they rule. So, also, in coming to Oregon from the east the country by no means impresses one as being surpassingly mountainous, the abode of peaks and glaciers. Descending the spurs of the Rocky Mountains into the basin of the Columbia, we see hot, hundred-mile plains, roughened here the there by hills and ridges that look hazy and blue in the distance, until we have pushed well to the westward. Then one white point after another comes into sight to refresh the eye and the imagination; but they are yet a long way off, and have much to say only to those who know them or others of their kind. How grand they are, though insignificant-looking on the edge of the vast landscape! What noble woods they nourish, and emerald meadows and gardens! What springs and streams and waterfalls sing about them and to what a multitude of happy creatures they give homes and food!

      The principal mountains of the range are Mounts Pitt, Scott, and Thielson, Diamond Peak, the Three Sisters, Mounts Jefferson, Hood, St. Helen's, Adams, Rainier, Aix, and Baker. Of these the seven first named belong to Oregon, the others to Washington. They rise singly at irregular distances from one another along the main axis of the range or near it, with an elevation of from about eight thousand to fourteen thousand four hundred feet above the level of the sea. From few points in the valleys may more than three or four of them be seen, and of the more distant ones of these only the tops appear. Therefore, speaking generally, each of the lowland landscapes of the State contains only one grand snowy mountain.

      The heights back of Portland command one of the best general views of the forests and also of the most famous of the great mountains both of Oregon and Washington. Mount Hood is in full view, with the summits of Mounts Jefferson, St. Helen's, Adams, and Rainier in the distance. The city of Portland is at our feet, covering a large area along both banks of the Willamette, and, with its fine streets, schools, churches, mills, shipping, parks, and gardens, makes a telling picture of busy, aspiring civilization in the midst of the green wilderness in which it is planted. The river is displayed to fine advantage in the foreground of our main view, sweeping in beautiful curves around rich, leafy islands, its banks fringed with willows.

      A few miles beyond the Willamette flows the renowned Columbia, and the confluence of these two great rivers is at a point only about ten miles below the city. Beyond the Columbia extends the immense breadth of the forest, one dim, black, monotonous field with only the sky, which one is glad to see is not forested, and the tops of the majestic old volcanoes to give diversity to the view. That sharp, white, broad-based pyramid on the south side of the Columbia, a few degrees to the south of east from where you stand, is the famous Mount Hood. The distance to it in a straight line is about fifty miles. Its upper slopes form the only bare ground, bare as to forests, in the landscape in that direction. It is the pride of Oregonians, and when it is visible is always pointed out to strangers as the glory of the country, the mountain of mountains. It is one of the grand series of extinct volcanoes extending from Lassen's Butte to Mount Baker, a distance of about six hundred miles, which once flamed like gigantic watch-fires along the coast. Some of them have been active in recent times, but no considerable addition to the bulk of Mount Hood has been made for several centuries, as is shown by the amount of glacial denudation it has suffered. Its summit has been ground to a point, which gives it a rather thin, pinched appearance. It has a wide-flowing base, however, and is fairly well proportioned. Though it is eleven thousand feet high, it is too far off to make much show under ordinary conditions in so extensive a landscape. Through a great part of the summer it is invisible on account of smoke poured into the sky from burning woods, logging camps, mills, etc., and in winter for weeks at a time, or even months, it is in the clouds. Only in spring and early summer and in what there may chance to be of bright weather in winter is it or any of its companions at all clear or telling. From the Cascades on the Columbia it may be seen at a distance of twenty miles or thereabouts, or from other points up and down the river, and with the magnificent foreground it is very impressive. It gives the supreme touch of grandeur to all the main Columbia

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