Travels in Alaska. John Muir
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patches; but when we contemplate the whole globe as one great dewdrop, striped and dotted with continents and islands, flying through space with other stars all singing and shining together as one, the whole universe appears as an infinite storm of beauty.
The California coast-hills and cliffs look bare and uninviting as seen from the ship, the magnificent forests keeping well back out of sight beyond the reach of the sea winds; those of Oregon and Washington are in some places clad with conifers nearly down to the shore; even the little detached islets, so marked a feature to the northward, are mostly tree-crowned. Up through the Straits of Juan de Fuca the forests, sheltered from the ocean gales and favored with abundant rains, flourish in marvelous luxuriance on the glacier-sculptured mountains of the Olympic Range.
We arrived in Esquimault Harbor, three miles from Victoria, on the evening of the fourth day, and drove to the town through a magnificent forest of Douglas spruce,–with an undergrowth in open spots of oak, madrone, hazel, dogwood, alder, spiræa, willow, and wild rose,–and around many an upswelling moutonné rock, freshly glaciated and furred with yellow mosses and lichens.
Victoria, the capital of British Columbia, was in 1879 a small old-fashioned English town on the south end of Vancouver Island. It was said to contain about six thousand inhabitants. The government buildings and some of the business blocks were noticeable, but the attention of the traveler was more worthily attracted to the neat cottage homes found here, embowered in the freshest and floweriest climbing roses and honeysuckles conceivable. Californians may well be proud of their home roses loading sunny verandas, climbing to the tops of the roofs and falling over the gables in white and red cascades. But here, with so much bland fog and dew and gentle laving rain, a still finer development of some of the commonest garden plants is reached. English honeysuckle seems to have found here a most congenial home. Still more beautiful were the wild roses, blooming in wonderful luxuriance along the woodland paths, with corollas two and three inches wide. This rose and three species of spiræa fairly filled the air with fragrance after showers; and how brightly then did the red dogwood berries shine amid the green leaves beneath trees two hundred and fifty feet high.
Strange to say, all of this exuberant forest and flower vegetation was growing upon fresh moraine material scarcely at all moved or in any way modified by post-glacial agents. In the town gardens and orchards, peaches and apples fell upon glacier-polished rocks, and the streets were graded in moraine gravel; and I observed scratched and grooved rock bosses as unweathered and telling as those of the High Sierra of California eight thousand feet or more above sea-level. The Victoria Harbor is plainly glacial in origin, eroded from the solid; and the rock islets that rise here and there in it are unchanged to any appreciable extent by all the waves that have broken over them since first they came to light toward the close of the glacial period. The shores also of the harbor are strikingly grooved and scratched and in every way as glacial in all their characteristics as those of new-born glacial lakes. That the domain of the sea is being slowly extended over the land by incessant wave-action is well known; but in this freshly glaciated region the shores have been so short a time exposed to wave-action that they are scarcely at all wasted. The extension of the sea affected by its own action in post-glacial times is probably less than the millionth part of that affected by glacial action during the last glacier period. The direction of the flow of the ice-sheet to which all the main features of this wonderful region are due was in general southward.
From this quiet little English town I made many short excursions–up the coast to Nanaimo, to Burrard Inlet, now the terminus of the Canadian Pacific Railroad, to Puget Sound, up Fraser River to New Westminster and Yale at the head of navigation, charmed everywhere with the wild, new-born scenery. The most interesting of these and the most difficult to leave was the Puget Sound region, famous the world over for the wonderful forests of gigantic trees about its shores. It is an arm and many-fingered hand of the sea, reaching southward from the Straits of Juan de Fuca about a hundred miles into the heart of one of the noblest coniferous forests on the face of the globe. All its scenery is wonderful–broad river-like reaches sweeping in beautiful curves around bays and capes and jutting promontories, opening here and there into smooth, blue, lake-like expanses dotted with islands and feathered with tall, spiry evergreens, their beauty doubled on the bright mirror-water.
Sailing from Victoria, the Olympic Mountains are seen right ahead, rising in bold relief against the sky, with jagged crests and peaks from six to eight thousand feet high,–small residual glaciers and ragged snow-fields beneath them in wide amphitheatres opening down through the forest-filled valleys. These valleys mark the courses of the Olympic glaciers at the period of their greatest extension, when they poured their tribute into that portion of the great northern ice-sheet that overswept Vancouver Island and filled the strait between it and the mainland.
On the way up to Olympia, then a hopeful little town situated at the end of one of the longest fingers of the Sound, one is often reminded of Lake Tahoe, the scenery of the widest expanses is so lake-like in the clearness and stillness of the water and the luxuriance of the surrounding forests. Doubling cape after cape, passing uncounted islands, new combinations break on the view in endless variety, sufficient to satisfy the lover of wild beauty through a whole life. When the clouds come down, blotting out everything, one feels as if at sea; again lifting a little, some islet may be seen standing alone with the tops of its trees dipping out of sight in gray misty fringes; then the ranks of spruce and cedar bounding the water's edge come to view; and when at length the whole sky is clear the colossal cone of Mt. Rainier may be seen in spotless white, looking down over the dark woods from a distance of fifty or sixty miles, but so high and massive and so sharply outlined, it seems to be just back of a strip of woods only a few miles wide.
Mt. Rainier, or Tahoma (the Indian name), is the noblest of the volcanic cones extending from Lassen Butte and Mt. Shasta along the Cascade Range to Mt. Baker. One of the most telling views of it hereabouts is obtained near Tacoma. From a bluff back of the town it was revealed in all its glory, laden with glaciers and snow down to the forested foothills around its finely curved base. Up to this time (1879) it had been ascended but once. From observations made on the summit with a single aneroid barometer, it was estimated to be about 14,500 feet high. Mt. Baker, to the northward, is about 10,700 feet high, a noble mountain. So also are Mt. Adams, Mt. St. Helens, and Mt. Hood. The latter, overlooking the town of Portland, is perhaps the best known. Rainier, about the same height as Shasta, surpasses them all in massive icy grandeur,–the most majestic solitary mountain I had ever yet beheld. How eagerly I gazed and longed to climb it and study its history only the mountaineer may know, but I was compelled to turn away and bide my time.
The species forming the bulk of the woods here is the Douglas spruce (Pseudotsuga douglasii), one of the greatest of the western giants. A specimen that I measured near Olympia was about three hundred feet in height and twelve feet in diameter four feet above the ground. It is a widely distributed tree, extending northward through British Columbia, southward through Oregon and California, and eastward to the Rocky Mountains. The timber is used for shipbuilding, spars, piles, and the framework of houses, bridges, etc. In the California lumber markets it is known as “Oregon pine.” In Utah, where it is common on the Wahsatch Mountains, it is called “red pine.” In California, on the western slope of the Sierra Nevada, it forms, in company with the yellow pine, sugar pine, and incense cedar, a pretty well-defined belt at a height of from three to six thousand feet above the sea; but it is only in Oregon and Washington, especially in this Puget Sound region, that it reaches its very grandest development,–tall, straight, and strong, growing down close to tidewater.
All the towns of the Sound had a hopeful, thrifty aspect. Port Townsend, picturesquely located on a grassy bluff, was the port of clearance for vessels sailing to foreign parts. Seattle was famed for its coal-mines, and claimed to be the coming town of the North Pacific Coast. So also did its rival, Tacoma, which had been selected as the terminus of the much-talked-of Northern Pacific Railway. Several coal-veins of astonishing thickness were discovered the winter before on the Carbon River, to the east of Tacoma, one of them said to be no less than twenty-one feet, another twenty feet, another fourteen, with many smaller ones, the aggregate thickness of all the veins being upwards of a hundred feet. Large deposits of magnetic iron ore and brown hematite, together with limestone, had been discovered in advantageous proximity to the coal, making a bright outlook for the Sound region in general in connection with its railroad