John Muir

The songs of the Yosemite winds and waterfalls are delightfully enriched with bird song, especially in the nesting time of spring and early summer. The most familiar and best known of all is the common robin, who may be seen every day, hopping about briskly on the meadows and uttering his cheery, enlivening call. The black-headed grosbeak, too, is here, with the Bullock oriole, and western tanager, brown song-sparrow, hermit thrush, the purple finch, - a fine singer, with head and throat of a rosy-red hue, - several species of warblers and vireos, kinglets, flycatchers, etc.

With the exception of a few spires and pinnacles, the South Dome is the only rock about the Valley that is strictly inaccessible without artificial means, and its inaccessibility is expressed in severe terms. Nevertheless many a mountaineer, gazing admiringly, tried hard to invent a way to the top of its noble crown - all in vain, until in the year 1875, George Anderson, an indomitable Scotchman, undertook the adventure.

All California has been glaciated, the low plains and valleys as well as the mountains. Traces of an ice-sheet, thousands of feet in thickness, beneath whose heavy folds the present landscapes have been molded, may be found everywhere, though glaciers now exist only among the peaks of the High Sierra. No other mountain chain on this or any other of the continents that I have seen is so rich as the Sierra in bold, striking, well-preserved glacial monuments. Indeed, every feature is more or less tellingly glacial.

In the wild gold years of 1849 and '50, the Indian tribes along thus western Sierra foothills became alarmed at the sudden invasion of their acorn orchard and game fields by miners, and soon began to make war upon them, in their usual murdering, plundering style. This continued until the United States Indian Commissioners succeeded in gathering them into reservations, some peacefully, others by burning their villages and stores of food.

Ambitious climbers, seeking adventures and opportunities to test their strength and skill, occasionally attempt to penetrate the wilderness on the west side of the Sound, and push on to the summit of Mount Olympus. But the grandest excursion of all to be make hereabouts is to Mount Rainier, to climb to the top of its icy crown. The mountain is very high[29], fourteen thousand four hundred feet, and laden with glaciers that are terribly roughened and interrupted by crevasses and ice cliffs. Only good climbers should attempt to gain the summit, led by a guide of proved nerve and endurance.

The monuments of the Ice Age in the Great Basin have been greatly obscured and broken, many of the more ancient of them having perished altogether, leaving scarce a mark, however faint, of their existence - a condition of things due not alone to the long-continued action of post-glacial agents, but also in great part to the perishable character of the rocks of which they were made.

Oregon is a large, rich, compact section of the west side of the continent, containing nearly a hundred thousand square miles of deep, wet evergreen woods, fertile valleys, icy mountains, and high, rolling wind-swept plains, watered by the majestic Columbia River and its countless branches. It is bounded on the north by Washington, on the east by Idaho, on the south by California and Nevada, and on the west by the Pacific Ocean.

Nevada is one of the very youngest and wildest of the States; nevertheless it is already strewn with ruins that seem as gray and silent and time-worn as if the civilization to which they belonged had perished centuries ago. Yet, strange to say, all these ruins are results of mining efforts made within the last few years.

Like the forests of Washington, already described, those of Oregon are in great part made up of the Douglas spruce[32], or Oregon pine (Abies Douglasii). A large number of mills are at work upon this species, especially along the Columbia, but these as yet have made but little impression upon its dense masses, the mills here being small as compared with those of the Puget Sound region.

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