Before reaching the Dalles, and afterwards, we had several superb views of glorious Mt. Hood. All good Oregonians claim Hood is the highest peak in the United States; but Californians boast their Shasta equals, while Whitney out-tops it. A party of savans had recently ascended Hood, and they reported the general range, of which Hood is a part, as 4,400 feet above the sea; above which Hood still shot up 13,000 feet. The summit proved to be crescent-shaped, half a mile long, by from three feet to fifty wide. The north front was a precipice, of naked columnar rock, falling sheer down—perpendicularly—a mile or more at a jump. On the west side was an ancient crater, a thousand feet in depth from which clouds of sulphurous smoke still issued occasionally. On the flanks were true glaciers, with terminal and lateral moraines, the same as among the Alps. Smoke about his summit, just before we reached the Dalles, heralded a smart shock of earthquake there, and no doubt he is the safety-valve of all that region. We had caught a glimpse or two of Mt. Hood in descending the Blue Mountains, and again from Umatilla: but it was only for a moment, and usually with his night-cap on. But in threading the cañon of the Columbia, one morning as we rounded a rocky bastion, suddenly, a hundred miles away, Hood stood before us, a vast pyramidal peak, snow-clad from base to summit, resting in solitary grandeur on a great mountain range—itself black with firs and pines. From the apparent level or slight undulation of the general Cascade Range, Hood quickly shoots up loftily into the sky, individual and alone, and serene and unapproachable dominates the far-stretching landscape. From all points of view, whether descending the Columbia, where the cañon often frames him in like a picture, or at Fort Vancouver, where he stands superb and glorious against the sapphire sky, Hood always gives you the impression of vast loftiness, of serene majesty, of heaven-kissing superiority and power, and Oregonians may well be proud of him. Butman's two pictures of Hood are both good, but neither does justice to his great merits. The White Mountains and the Alleghanies are well enough in their way. The Rocky Mountains are indeed noble and majestic. But once see Hood, and all these pall upon the mind, and he alone rules the memory and imagination afterwards. Up the Columbia and down, off at sea, and pretty much all over Oregon, Hood is a great and magnificent landmark; and, of itself, is well worth a trip across the continent.

MOUNT HOOD.

Past the Cascade Mountains, we came suddenly out into a new region, and a totally different climate. From Umatilla to the Mountains we had the same clear atmosphere and perfect sky, that we had found everywhere from the Plains to the Columbia, substantially. The country naturally was the same barren and sterile region as at Salt Lake, abounding only in sage-brush and grease-wood; and, indeed, the whole internal basin of the continent, from the Rocky Mountains to the Sierra Nevadas, and from British America down to Mexico, appeared to be of this same general character—from want of regular rains in summer. Over most of this vast region, there had been no rains for weeks, or indeed months; and for days together as we journeyed along, we had never seen a cloud or mist even, to mar the absolute ultramarine of those perfect skies. But now, in descending the Columbia, as we approached the Mountains, we descried the clouds on their western slope ever trying to float over, but never apparently succeeding, their white discs gleaming in the sun; and when we drew nearer, we beheld a fleecy mist drifting up the Columbia, and streaming eastward like a pennon. Nearer still, we encountered a stiff breeze sweeping through the cañon, as through a funnel; and when we got well down into the jaws of the gorge, it needed all our steam, as well as the strong westward current to carry us forward. Sometimes, it was said, the Columbia just here becomes so rough, because of this conflicting wind and current, as to cause real sea-sickness on the boats, and occasionally indeed they have to cast anchor, unable to descend. Farther down, this mist thickened into rain, and when we got fairly through and out of the Mountains, (it raining most of the way), we debouched into the Coast Region, where it was still raining steadily, as it had been for many days, and continued to for weeks together afterwards. As soon as we struck the rain, trees and herbage at once made their appearance, clothing the mountains and bottoms everywhere; lichens and mosses again decorated all the rocks; and when we got well out of the Mountains, behold such forests of fir, pine, cedar, oak, etc., as never appear East. In half a day, you may thus pass from a comparatively rainless to a thoroughly rainy region; and in winter from a severely cold, to a comparatively moderate climate. The contrast is very striking, and you soon feel it keenly in every sense. Your eyes glaze, your skin becomes moist, and if there is a weak spot about your lungs, you will find it out very quickly. The proximity of the Pacific, of course, explains it all—the warm, humid winds from which sweep up against the Cascade Range, but find in their lofty crest an insurmountable barrier. If light enough to ascend, their wealth of moisture is condensed as rain or snow along the mountain sides or summit, by the cold of the upper regions, as with your hand you squeeze a sponge; and, consequently, they topple over the Range dry and clear—to curse a vast region beyond with their sterility. If unable to ascend, they career along the western slope of the Mountains, and hover over the Coast Region generally, literally deluging Western Oregon and Washington, at certain seasons of the year, with rains and fogs. The year before, at Fort Vancouver, they had had one hundred and twenty consecutive days of rain, in one year, without counting the intervening showers; and they said, it wasn't "much of a year for rain" either! Another year, they didn't see the sun there for eighty days together, without reckoning the occasional fogs. No wonder the Oregonians are called "Web-Feet." They do say, the children there are all born web-footed, like ducks and geese, so as to paddle about, and thus get along well in that amphibious region. Perhaps this is rather strong, even for Darwinism; but I can safely vouch for Oregon's all-sufficing rains and fogs, whatever their effects on the species.

Our fellow-passengers down the Columbia were chiefly returning miners, going below to winter and recruit; but rough as they were and merry at times, they were, as a rule, self-respecting and orderly. Our Fenian friends, who had raced with us down Powder River and Grande Ronde Valleys and across the Blue Mountains, turned up here again—"Shanks," "Fatty," and all—and subsequently embarked on the same steamer with us at Portland for San Francisco. A few Chinamen also were on board; but they behaved civilly, and were treated kindly.


[CHAPTER XVI.]