Along Alaska's Great River A Popular Account of the Travels of an Alaska Exploring Expedition along the Great Yukon River, from Its Source to Its Mouth, in the British — A Closer Reading

This Alaskan exploring expedition was composed of the following members: Lieut. Schwatka, U.S.A., commanding; Dr. George F. Wilson, U.S.A., Surgeon; Topographical Assistant Charles A. Homan, U.S. Engineers, Topographer and Photographer; Sergeant Charles A. Gloster, U.S.A., Artist; Corporal Shircliff, U.S.A., in charge of stores; Private Roth, assistant, and Citizen J. B. McIntosh, a miner, who had lived in Alaska and was well acquainted with its methods of travel. Indians and others were added and discharged from time to time as hereafter noted.

The main object of the expedition was to acquire such information of the country traversed and its wild inhabitants as would be valuable to the military authorities in the future, and as a map would be needful to illustrate such information well, the party's efforts were rewarded with making the expedition successful in a geographical sense. I had hoped to be able, through qualified subordinates, to extend our scientific knowledge of the country explored, especially in regard to its botany, geology, natural history, etc.; and, although these subjects would not in any event have been adequately discussed in a popular treatise like the present, it must be admitted that little was accomplished in these branches. The explanation of this is as follows: When authority was asked from Congress for a sum of money to make such explorations under military supervision and the request was disapproved by the General of the Army and Secretary of War. This disapproval, combined with the active opposition of government departments which were assigned to work of the same general character and coupled with the reluctance of Congress to make any appropriations whatever that year, was sufficient to kill such an undertaking. When the military were withdrawn from Alaska by the President, about the year 1878, a paragraph appeared at the end of the President's order stating that no further control would be exercised by the army in Alaska; and this proviso was variously interpreted by the friends of the army and its enemies, as a humiliation either to the army or to the President, according to the private belief of the commentator. It was therefore seriously debated whether any military expedition or party sent into that country for any purpose whatever would not be a direct violation of the President's proscriptive order, and when it was decided to waive that consideration, and send in a party, it was considered too much of a responsibility to add any specialists in science, with the disapproval of the General and the Secretary hardly dry on the paper. The expedition was therefore, to avoid being recalled, kept as secret as possible, and when, on May 22d, it departed from Portland, Oregon, upon the _Victoria_, a vessel which had been specially put on the Alaska route, only a two or three line notice had gotten into the Oregon papers announcing the fact; a notice that in spreading was referred to in print by one government official as "a junketing party," by another as a "prospecting" party, while another bitterly acknowledged that had he received another day's intimation he could have had the party recalled by the authorities at Washington. Thus the little expedition which gave the first complete survey to the third[1] river of our country stole away like a thief in the night and with far less money in its hands to conduct it through its long journey than was afterward appropriated by Congress to publish its report.

[1] The largest river on the North American continent so far as this mighty stream flows within our boundaries.... The people of the United States will not be quick to take to the idea that the volume of water in an Alaskan river is greater than that discharged by the mighty Mississippi; but it is entirely within the bounds of honest statement to say that the Yukon river ... discharges every hour one-third more water than the "Father of Waters."--Petroff's Government Report on Alaska.

Leaving Portland at midnight on the 22d, the _Victoria_ arrived at Astoria at the mouth of the Columbia the forenoon of the 23d, the remaining hours of daylight being employed in loading with supplies for a number of salmon canneries in Alaska, the large amount of freight for which had necessitated this extra steamer. That night we crossed the Columbia River bar and next morning entered the Strait of Juan de Fuca, the southern entrance from the Pacific Ocean which leads to the inland passage to Alaska.

THE INLAND PASSAGE TO ALASKA.

"The Inland Passage" to Alaska is the fjörd-like channel, resembling a great river, which extends from the north-western part of Washington Territory, through British Columbia, into south-eastern Alaska. Along this coast line for about a thousand miles, stretches a vast archipelago closely hugging the mainland of the Territories named above, the southernmost important island being Vancouver, almost a diminutive continent in itself, while to the north Tchichagoff Island limits it on the seaboard.

From the little town of Olympia at the head of Puget Sound, in Washington Territory, to Chilkat, Alaska, at the head of Lynn Channel, or Canal, one sails as if on a grand river, and it is really hard to comprehend that it is a portion of the ocean unless one can imagine some deep fjörd in Norway or Greenland, so deep that he can sail on its waters for a fortnight, for the fjörd-like character is very prominent in these channels to which the name of "Inland Passage" is usually given.

These channels between the islands and mainland are strikingly uniform in width, and therefore river-like in appearance as one steams or sails through, them. At occasional points they connect with the Pacific Ocean, and if there be a storm on the latter, a few rolling swells may enter at these places and disturb the equilibrium of sensitive stomachs for a brief hour, but at all other places the channel is as quiet as any broad river, whatever the weather. On the south we have the Strait of Juan de Fuca and to the north Cross Sound as the limiting channels, while between the two are found Dixon Entrance, which separates Alaska from British Columbia, Queen Charlotte Sound, and other less important outlets.

On the morning of the 24th of May we entered the Strait of Juan de Fuca, named after an explorer--if such he may be called--who never entered this beautiful sheet of water, and who owes his immortality to an audacious guess, which came so near the truth as to deceive the scientific world for many a century. To the left, as we enter, i.e., northward, is the beautiful British island of Vancouver, the name of which commemorates one of the world's most famous explorers. Its high rolling hills are covered with shaggy firs, broken near the beach into little prairies of brighter green, which are dotted here and there with pretty little white cottages, the humblest abodes we see among the industrious, British or American, who live in the far west.

The American side, to the southward, gives us the same picture backed by the high range of the Olympian Mountains, whose tops are covered with perpetual snow, and upon whose cold sides drifting clouds are condensed.

Through British Columbia the sides of this passage are covered with firs and spruce to the very tops of the steep mountains forming them, but as Northing is gained and Alaska is reached the summits are covered with snow and ice at all months of the year, and by the time we cast anchor in Chilkat Inlet, which is about the northernmost point of this great inland salt-water river, we find in many places these crowns of ice debouching in the shape of glaciers to the very water's level, and the tourist beholds, on a regular line of steamboat travel, glaciers and icebergs, and many of the wonders of arctic regions, although upon a reduced scale. Alongside the very banks and edges of these colossal rivers of ice one can gather the most beautiful of Alpine flowers and wade up to his waist in grasses that equal in luxuriance the famed fields of the pampas; while the singing of the birds from the woods and glens and the fragrance of the foliage make one easily imagine that the Arctic circle and equator have been linked together at this point.

Entering Juan de Fuca Strait a few hours were spent in the pretty little anchorage of Neah Bay, the first shelter for ships after rounding Cape Flattery, and here some merchandise was unloaded in the huge Indian canoes that came alongside, each one holding at least a ton.

Victoria, the metropolis of British Columbia, was reached the same day, and as it was the Queen's birthday we saw the town in all its bravery of beer, bunting and banners. Our vessel tooted itself hoarse outside the harbor to get a pilot over the bar, but none was to be had till late in the day, when a pilot came out to us showing plainly by his condition that he knew every bar in and about Victoria. With the bar pilot on the bridge, as to save insurance should an accident occur, we entered the picturesque little harbor in safety, despite the discoveries of our guide that since his last visit all the buoys had been woefully misplaced, and even the granite channel had changed its course. But Victoria has many embellishments more durable than bunting and banners, and most conspicuous among them are her well arranged and well constructed roads, in which she has no equal on the Pacific coast of North America, and but few rivals in any other part of the world.

On the 26th we crossed over to Port Townsend, the port of entry for Puget sound, and on the 27th we headed for Alaska by way of the Inland Passage.

For purposes of description this course should have been designated the "inland passages," in the plural, for its branches are almost innumerable, running in all directions like the streets of an irregular city, although now and then they are reduced to a single channel or fjörd which the steamer is obliged to take or put out to sea. At one point in Discovery Passage leading from the Gulf of Georgia toward Queen Charlotte Sound, the inland passage is so narrow that our long vessel had to steam under a slow bell to avoid accidents, and at this place, called Seymour Narrows, there was much talk of bridging the narrow way in the grand scheme of a Canadian Pacific Railway, which should have its western terminus at Victoria. Through this contracted way the water fairly boils when at its greatest velocity, equaling ten miles an hour in spring tides, and at such times the passage is hazardous even to steamers, while all other craft avoid it until slack water. Jutting rocks increase the danger, and on one of these the United States man-of-war _Saranac_ was lost just eight years before we passed through. At the northern end of this picturesque Discovery Passage you see the inland passage trending 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.

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 with a few modifications to about Mount St. Elias.