If Claude Melnotte had wanted to paint a fairer picture to his lady, he should have told Pauline of this glorious northwest coast, fringed with islands, seamed with fathomless channels of clear, green, sea water, and basking in the soft, mellow radiance of this summer sunshine. The scenery gains everything from being translated through the medium of a soft, pearly atmosphere, where the light is as gray and evenly diffused as in Old England itself. The distant mountain ranges are lost in the blue vaporous shadows, and nearer at hand the masses and outlines show in their pure contour without the obtrusion of all the garish details that rob so many western mountain scenes of their grander effects. The calm of the brooding air, the shimmer of the opaline sea around one, and the ranges of green and russet hills, misty purple mountains, and snowy summits on the faint horizon, give a dream-like coloring to all one’s thoughts. A member of the Canadian Parliament, in speaking of this coast country of British Columbia, called it the “sea of mountains” and the channels of the ocean through which one winds for days are but as endless valleys and steep cañons between the peaks and ranges that rise abruptly from the water’s edge. Only the fiords and inlets of the coast of Norway, and the wooded islands in the Inland Sea of Japan, present anything like a counterpart to the wonderful scenery of these archipelagos of the North Pacific. From the head of Puget Sound to the mouth of the Chilkat River there are seven hundred and thirty-two miles of latitude, and the trend of the coast and the ship’s windings between and around the islands make it an actual voyage of more than a thousand miles on inland waters.
The Strait or Gulf of Georgia, that separates Vancouver’s Island from the mainland, although widening at times to forty miles, is for the most part like a broad river or lake, landlocked, walled by high mountain ranges on both sides, and choked at either end with groups of islands. The mighty current of the Frazer River rolls a pale green flood of fresh water into it at the southern entrance, and the river water, with its different density and temperature floating on the salt water, and cutting through it in a body, shows everywhere a sharply defined line of separation. In the broad channels schools of whales are often seen spouting and leaping, and on a lazy, sunny afternoon, while even the mountains seemed dozing in the waveless calm, the idlers on the after deck were roused by the cry of “Whales!” For an hour we watched the frolicking of the snorting monsters, as they spouted jets of water, arched their black backs and fins above the surface, and then disappeared with perpendicular whisks of their huge tails.
Toward the north end of Vancouver’s Island, where Valdes Island is wedged in between it and the mainland shore, the ship enters Discovery Pass, in which are the dangerous tide rips of Seymour Narrows. The tides rushing in and out of the Strait of Georgia dash through this rocky gorge at the rate of four and eight knots an hour on the turn, and the navigators time their sailing hours so as to reach this perilous place in daylight and at the flood tide. Even at that time the water boils in smooth eddies and deep whirlpools, and a ship is whirled half round on its course as it threads the narrow pass between the reefs. At other times the water dashes over the rapids and raises great waves that beat back an opposing bow, and the dullest landsman on the largest ship appreciates the real dangers of the run through this wild ravine, where the wind races with the water and howls in the rigging after the most approved fashion for thrilling marine adventures. Nautical gossips tell one of vessels that, steaming against the furious tide, have had their paddle wheels reversed by its superior strength, and have been swept back to wait the favorable minutes of slack water. Others, caught by the opposing current, are said to have been slowly forced back, or, steaming at full speed, have not gained an inch of headway for two hours. The rise and fall of the tides is thirteen feet in these narrows, and although there are from twenty to sixty fathoms of water in the true channel, there is an ugly ledge and isolated rocks in the middle of the pass on which there are only two and a quarter fathoms. Long before Vancouver carried his victorious ensign through these unknown waters, the Indians had known and dreaded these rapids as the abode of an evil spirit, and for half a century the adventurous Hudson Bay traders went warily through the raging whirlpools.
Although the British Admiralty have made careful surveys, and the charts are in the main accurate, there have been serious wrecks on this part of the coast. The United States man-of-war Saranac was lost in Seymour Narrows on the 18th of June, 1875. The Saranac was an old side-wheel steamer of the second rate in naval classification, carrying eleven guns, and was making its third trip to Alaskan waters. There was an unusually low tide the morning the Saranac entered the pass, and the ship was soon caught in the wild current, and sent broadside on to the mid-rock. It swung off, and was headed for the Vancouver shore, and made fast with hawsers to the trees, but there was only time to lower a boat with provisions and the more important papers before the Saranac sunk, and not even the masts were left visible. The men camped on shore while a party went in the small boats to Nanaimo for help. No attempt was ever made to raise the ship, and in the investigation it was shown that the boilers were in such a condition when they reached Victoria, that striking the rock in Seymour Narrows was only one of the perils that awaited those on board. No lives were lost by this disaster, and Dr. Bessels, of the Smithsonian Institute, who was on his way up the coast to make a collection of Indian relics for the Centennial Exposition, showed a scientist’s zeal in merely regretting the delay, and continuing on his journey by the first available craft. In April, 1883, the steamer Grappler, which plied between Victoria and the trading-posts on the west coast, took fire late at night, just as it was entering Seymour Narrows. The flames reached the hempen rudder-ropes, and the boat was soon helplessly drifting into the rapids. Flames and clouds of smoke made it difficult to launch the boats, and all but one were swamped. The frantic passengers leaped overboard while the ship was whirling and careening in the rapids, and the captain, with life-preserver on, was swept off, and disappeared in midstream. The Grappler finally drifted in to the Vancouver shore, and burned until daylight. Another United States war vessel, the Suwanee was lost a hundred miles beyond the Seymour Narrows by striking an unknown rock at the entrance to Queen Charlotte Sound.
In crossing this forty-mile stretch of Queen Charlotte Sound the voyager feels the swell, and touches the outer ocean for the first time. If the wind is strong there may be a chopping sea, but in general it is a stilled expanse on which fog and mist eternally brood. The Kuro Siwo, or Black Stream, or Japan Current, of the Pacific, which corresponds to the Gulf Stream of the Atlantic, touches the coast near this Sound, and the colder air from the land striking this warm river of the sea produces the heavy vapors which lie in impenetrable banks for miles, or float in filmy and downy clouds along the green mountain shores. It is this warm current which modifies the climate of the whole Pacific coast, bends the isothermal lines northward, and makes temperature depend upon the distance from the sea instead of upon distance from the equator. Bathed in perpetual fog, like the south coast of England and Ireland, there is a climatic resemblance in many ways between the islands of Great Britain and the islands of the British Columbia shore. The constant moisture and the long days force vegetation like a hothouse, and the density of the forests and the luxuriance of the undergrowth are equalled only in the tropics. The pine-trees cover the mountain slopes as thickly as the grass on a hillside, and as fires have never destroyed the forests, only the spring avalanches and land-slides break their continuity. There is an inside passage between the mountains from Queen Charlotte to Milbank Sound that gave us an afternoon and evening in the midst of fine scenery, but for another whole day we passed through the grandest of fiords on the British Columbia coast.
The sun rose at three o’clock on that rare summer morning, when the ship thrust her bow into the clear, mirror-like waters of the Finlayson Channel, and at four o’clock a dozen passengers were up in front watching the matchless panorama of mountain walls that slipped silently past us. The clear, soft light, the pure air, and the stillness of sky, and shore, and water, in the early morning, made it seem like the dawn of creation in some new paradise. The breath of the sea and the breath of the pine forest were blended in the air, and the silence and calm added to the inspiration of the surroundings. The eastern wall of the channel lay in pure shadow, the forest slopes were deep unbroken waves of green, with a narrow base-line of sandstone washed snowy white, and beneath that every tree and twig lay reflected in the still mirror of waters of a deeper, purer, and softer green