away to the eastward, with quite a bay on the left around Chatham Point, and while you are wondering in that half soliloquizing way of a traveler in new lands what you will see after you have turned to the right, the great ship swings suddenly to the left, and you find that what you took for a bay is after all the inland passage itself, which stretches once more before you like the Hudson looking upward from West Point, or the Delaware at the Water Gap. For all such little surprises must the tourist be prepared on this singular voyage.
The new bend now becomes Johnstone Strait and so continues to Queen Charlotte Sound, with which it connects by one strait, two passages and a channel, all alike, except in name, and none much over ten miles long. At nearly every point where a new channel diverges both arms take on a new name, and they change as rapidly as the names of a Lisbon street, which seldom holds the same over a few blocks. The south side of Johnstone Strait is particularly high, rising abruptly from the water fully 5,000 feet, and in grandeur not unlike the Yellowstone Cañon. These summits were still covered with snow and probably on northern slopes snow remains the summer through. One noticeable valley was on the Vancouver Island side, with a conspicuous conical hill in its bosom that may have been over a thousand feet in height. These cone-like hills are so common in flat valleys in north-western America that I thought it worth while to mention the fact in this place. I shall have occasion to do so again at a later point in my narrative. Occasionally windrows occur through the dense coniferous forests of the inland passage, where the trees have been swept or leveled in a remarkable manner. Such as were cut vertically had been caused by an avalanche, and in these instances the work of clearing had been done as faithfully as if by the hands of man. Sometimes the bright green moss or grass had grown up in these narrow ways, and when there was more than one of about the same age there was quite a picturesque effect of stripings of two shades of green, executed on a most colossal plan. These windrows of fallen trees sometimes stretched along horizontally in varying widths, an effect undoubtedly produced by heavy gales rushing through the contracted "passage."
One's notice is attracted by a species of natural beacon which materially assists the navigator. Over almost all the shoals and submerged rocks hang fields of kelp, a growth with which the whole "passage" abounds, thus affording a timely warning badly needed where the channel has been imperfectly charted. As one might surmise the water is very bold, and these submerged and ragged rocks are in general most to be feared. Leaving Johnstone Strait we enter Queen Charlotte Sound, a channel which was named, lacking only three years, a century ago. It widens into capacious waters at once and we again felt the "throbbing of old Neptune's pulse," and those with sensitive stomachs perceived a sort of flickering of their own.
One who is acquainted merely in a general way with the history and geography of this confusing country finds many more Spanish names than he anticipates, and to his surprise, a conscientious investigation shows that even as it is the vigorous old Castilian explorers have not received all the credit to which they are entitled, for many of their discoveries in changing hands changed names as well: the Queen Charlotte Islands, a good day's run to the north-westward of us, were named in 1787 by an Englishman, who gave the group the name of his vessel, an appellation which they still retain, although as Florida Blanca they had known the banner of Castile and Leon thirteen years before. Mount Edgecumbe, so prominent in the beautiful harbor of Sitka, was once Monte San Jacinto, and a list of the same tenor might be given that would prove more voluminous than interesting. American changes in the great north-west have not been so radical. Boca de Quadra Inlet has somehow become Bouquet Inlet to those knowing it best. La Creole has degenerated into Rickreall, and so on: the foreign names have been mangled but not annihilated. We sail across Queen Charlotte Sound as if we were going to bump right into the high land ahead of us, but a little indentation over the bow becomes a valley, then a bay, and in ample time to prevent accidents widens into another salt-water river, about two miles wide and twenty times as long, called Fitzhugh Sound. Near the head of the sound we turn abruptly westward into the Lama Passage, and on its western shores we see nearly the first sign of civilization in the inland passage, the Indian village of Bella Bella, holding probably a dozen native houses and a fair looking church, while a few cattle grazing near the place had a still more civilized air.
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SCENES IN THE INLAND PASSAGE.
As we steamed through Seaforth Channel, a most tortuous affair, Indians were seen paddling in their huge canoes from one island to another or along the high, rocky shores, a cheering sign of habitation not previously noticed.
The great fault of the inland passage as a resort for tourists is in the constant dread of fogs that may at any time during certain months of the year completely obscure the grand scenery that tempted the travelers thither. The waters of the Pacific Ocean on the seaboard of Alaska are but a deflected continuation of the warm equatorial current called the Kuro Siwo of the Japanese; from these waters the air is laden with moisture, which being thrown by the variable winds against the snow-clad and glacier-covered summits of the higher mountains, is precipitated as fog and light rain, and oftentimes every thing is wrapped for weeks in these most annoying mists. July, with June and August, are by far the most favorable months for the traveler. The winter months are execrable, with storms of rain, snow and sleet constantly occurring, the former along the Pacific frontage, and the latter near the channels of the mainland.
Milbank Sound gave us another taste of the ocean swells which spoiled the flavor of our food completely, for although we were only exposed for less than an hour that hour happened to come just about dinner time; after which we entered Finlayson Passage, some twenty-five miles long. This is a particularly picturesque and bold channel of water, its shores covered with shaggy conifers as high as the eye can reach, and the mountains, with their crowns of snow and ice, furnishing supplies of spray for innumerable beautiful waterfalls. At many places in the inland passage from here on, come down the steep timbered mountains the most beautiful waterfalls fed from the glaciers hidden in the fog. At every few miles we pass the mouths of inlets and channels, leading away into the mountainous country no one knows whither. There are no charts which show more than the mouths of these inlets. Out of or into these an occasional canoe speeds its silent way perchance in quest of salmon that here abound, but the secrets of their hidden paths are locked in the savage mind. How tempting they must be for exploration, and how strange that, although so easy of access, they still remain unknown. After twisting around through a few "reaches," channels and passages, we enter the straightest of them all, Grenville Channel, so straight that it almost seems to have been mapped by an Indian. As you steam through its forty or fifty miles of mathematically rectilinear exactness you think the sleepy pilot might tie his wheel, put his heels up in the spokes, draw his hat over his eyes and take a quiet nap. In one place it seems to be not over two or three hundred yards wide, but probably is double that, the high towering banks giving a deceptive impression. The windrows through the timber of former avalanches of snow or landslides, now become thicker and their effects occasionally picturesque in the very devastation created. Beyond Grenville Channel the next important stretch of salt water is Chatham Sound, which is less like a river than any yet named. Its connection with Grenville Channel is by the usual number of three or four irregular water-ways dodging around fair sized islands, which had at one time, however, a certain importance because it was thought that the Canadian Pacific Railway might make Skeena Inlet off to our right its western terminus.
On the 29th of May, very early in the morning, we crossed Dixon Entrance, and were once more on American soil, that is, in a commercial sense, the United States having drawn a check for its value of $7,200,000, and the check having been honored; but in regard to government the country may be called no man's land, none existing in the territory. Dixon Entrance bore once a Spanish name in honor of its discoverer, a name which is heard no more, although a few still call the channel by its Indian name, Kaiganee. Broad Dixon Entrance contracts into the narrow Portland Inlet, which, putting back into the mainland for some seventy-five miles, forms the water boundary between Alaska and British Columbia. From here it becomes a thirty mile wide strip drawn "parallel to tide-water," which continues
