第51章 XVII(2)

For the tourist sailing to Puget Sound from San Francisco there is but little that is at all striking in the scenery within reach by the way until the mouth of the Strait of Juan de Fuca is reached. The voyage is about four days in length and the steamers keep within sight of the coast, but the hills fronting the sea up to Oregon are mostly bare and uninviting, the magnificent redwood forests stretching along this portion of the California coast seeming to keep well back, away from the heavy winds, so that very little is seen of them; while there are no deep inlets or lofty mountains visible to break the regular monotony. Along the coast of Oregon the woods of spruce and fir come down to the shore, kept fresh and vigorous by copious rains, and become denser and taller to the northward until, rounding Cape Flattery, we enter the Strait of Fuca, where, sheltered from the ocean gales, the forests begin to hint the grandeur they attain in Puget Sound. Here the scenery in general becomes exceedingly interesting; for now we have arrived at the grand mountain-walled channel that forms the entrance to that marvelous network of inland waters that extends along the margin of the continent to the northward for a thousand miles.

This magnificent inlet was named for Juan de Fuca, who discovered it in 1592 while seeking a mythical strait, supposed to exist somewhere in the north, connecting the Atlantic and Pacific. It is about seventy miles long, ten or twelve miles wide, and extends to the eastward in a nearly straight line between the south end of Vancouver Island and the Olympic Range of mountains on the mainland.

Cape Flattery, the western termination of the Olympic Range, is terribly rugged and jagged, and in stormy weather is utterly inaccessible from the sea. Then the ponderous rollers of the deep Pacific thunder amid its caverns and cliffs with the foam and uproar of a thousand Yosemite waterfalls. The bones of many a noble ship lie there, and many a sailor. It would seem unlikely that any living thing should seek rest in such a place, or find it. Nevertheless, frail and delicate flowers bloom there, flowers of both the land and the sea; heavy, ungainly seals disport in the swelling waves, and find grateful retreats back in the inmost bores of its storm-lashed caverns; while in many a chink and hollow of the highest crags, not visible from beneath, a great variety of waterfowl make homes and rear their young.

But not always are the inhabitants safe, even in such wave-defended castles as these, for the Indians of the neighboring shores venture forth in the calmest summer weather in their frail canoes to spear the seals in the narrow gorges amid the grinding, gurgling din of the restless waters. At such times also the hunters make out to scale many of the apparently inaccessible cliffs for the eggs and young of the gulls and other water birds, occasionally losing their lives in these perilous adventures, which give rise to many an exciting story told around the campfires at night when the storms roar loudest.

Passing through the strait, we have the Olympic Mountains close at hand on the right, Vancouver Island on the left, and the snowy peak of Mount Baker straight ahead in the distance. During calm weather, or when the clouds are lifting and rolling off the mountains after a storm, all these views are truly magnificent. Mount Baker is one of that wonderful series of old volcanoes that once flamed along the summits of the Sierras and Cascades from Lassen to Mount St. Elias.

Its fires are sleeping now, and it is loaded with glaciers, streams of ice having taken the place of streams of glowing lava. Vancouver Island presents a charming variety of hill and dale, open sunny spaces and sweeps of dark forest rising in swell beyond swell to the high land in the distance.

But the Olympic Mountains most of all command attention, seen tellingly near and clear in all their glory, rising from the water's edge into the sky to a height of six or eight thousand feet. They bound the strait on the south side throughout its whole extent, forming a massive sustained wall, flowery and bushy at the base, a zigzag of snowy peaks along the top, which have ragged-edged fields of ice and snow beneath them, enclosed in wide amphitheaters opening to the waters of the strait through spacious forest-filled valleys enlivened with fine, dashing streams. 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 the south end of Vancouver Island and filled the strait with flowing ice as it is now filled with ocean water.

The steamers of the Sound usually stop at Esquimalt on their way up, thus affording tourists an opportunity to visit the interesting town of Victoria, the capital of British Columbia. The Victoria harbor is too narrow and difficult of access for the larger class of ships; therefore a landing has to be made at Esquimalt. The distance, however, is only about three miles, and the way is delightful, winding on through a charming forest of Douglas spruce, with here and there groves of oak and madrone, and a rich undergrowth of hazel, dogwood, willow, alder, spiraea, rubus, huckleberry, and wild rose. Pretty cottages occur at intervals along the road, covered with honeysuckle, and many an upswelling rock, freshly glaciated and furred with yellow mosses and lichen, telling interesting stories of the icy past.

Victoria is a quiet, handsome, breezy town, beautifully located on finely modulated ground at the mouth of the Canal de Haro, with charming views in front, of islands and mountains and far-reaching waters, ever changing in the shifting lights and shades of the clouds and sunshine. In the background there are a mile or two of field and forest and sunny oak openings; then comes the forest primeval, dense and shaggy and well-nigh impenetrable.