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Into this wonderland the visitor enters by one of two roads. Either he leaves the railroad at Glacier Park on the east side of the continental divide or at Belton on the west side. In either event he can cross to the other side only afoot or on horseback over passes. The usual way in is through Glacier Park. There is a large hotel at the station from which automobile-stages run northward to chalets at Two Medicine Lake, the Cut Bank Valley, and St. Mary Lake, and to the Many Glacier Hotel and chalets at Lake McDermott. A road also reaches Lake McDermott from Canada by way of Babb, and Canadian visitors can reach the trails at the head of Waterton Lake by boat from their own Waterton Lakes Park. Those entering at Belton, where the park headquarters are located, find chalets at the railroad-station and an excellent hotel near the head of Lake McDonald. There is also a comfortable chalet close to the Sperry Glacier.

To see Glacier as thoroughly as Glacier deserves and to draw freely on its abundant resources of pleasure and inspiration, one must travel the trails and pitch his tent where day's end brings him. But that does not mean that Glacier cannot be seen and enjoyed by those to whom comfortable hotel accommodations are a necessity, or even by those who find trail-travelling impossible.

Visitors, therefore, fall into three general classes, all of whom may study scenery which quite fully covers the range of Glacier's natural phenomena and peculiar beauty. The largest of these classes consists of those who can travel, or think they can travel, only in vehicles, and can find satisfactory accommodations only in good hotels. The intermediate class includes those who can, at a pinch, ride ten or twelve miles on comfortably saddled horses which walk the trails at two or three miles an hour, and who do not object to the somewhat primitive but thoroughly comfortable overnight accommodations of the chalets. Finally comes the small class, which constantly will increase, of those who have the time and inclination to leave the beaten path with tent and camping outfit for the splendid wilderness and the places of supreme magnificence which are only for those who seek.

The man, then, whose tendency to gout, let us say, forbids him ride a horse or walk more than a couple of easy miles a day may, nevertheless, miss nothing of Glacier's meaning and magnificence provided he takes the trouble to understand. But he must take the trouble; he must comprehend the few examples that he sees; this is his penalty for refusing the rich experience of the trail, which, out of its very fulness, drives meaning home with little mental effort. His knowledge must be got from six places only which may be reached by vehicle, at least three of which, however, may be included among the world's great scenic places. He can find at Two Medicine, St. Mary, and McDermott superb examples of Glacier's principal scenic elements.

Entering at Glacier Park, he will have seen the range from the plains, an important beginning; already, approaching from the east, he has watched it grow wonderfully on the horizon. So suddenly do these painted mountains spring from the grassy plain that it is a relief to recognize in them the advance guard of the Lewis Overthrust, vast fragments of the upheavals of the depths pushed eastward by the centuries to their final resting-places upon the surface of the prairie. From the hotel porches they glow gray and yellow and purple and rose and pink, according to the natural coloring of their parts and the will of the sun—a splendid ever-changing spectacle.

The Two Medicine Country

An hour's automobile-ride from Glacier Park Hotel will enable our traveller to penetrate the range at a point of supreme beauty and stand beside a chalet at the foot of Two Medicine Lake. He will face what appears to be a circular lake in a densely forested valley from whose shore rises a view of mountains which will take his breath. In the near centre stands a cone of enormous size and magnificence—Mount Rockwell—faintly blue, mistily golden, richly purple, dull silver, or red and gray, according to the favor of the hour and the sky. Upon its left and somewhat back rises a smaller similar cone, flatter but quite as perfectly proportioned, known as Grizzly Mountain, and upon its right less regular masses. In the background, connecting all, are more distant mountains flecked with snow, the continental divide. Towering mountains close upon him upon both sides, that upon his right a celebrity in red argillite known as Rising Wolf. He sees all this from a beach of many-colored pebbles.

Few casual visitors have more than a midday view of Two Medicine Lake, for the stage returns in the afternoon. The glory of the sunset and the wonder before sunrise are for the few who stay over at the chalet. The lover of the exquisite cannot do better, for, though beyond lie scenes surpassing this in the qualities which bring to the lips the shout of joy, I am convinced that nothing elsewhere equals the Two Medicine canvas in the perfection of delicacy. It is the Meissonier of Glacier.

Nor can the student of Nature's processes afford to miss the study of Two Medicine's marvellously complete and balanced system of cirques and valleys—though this of course is not for the rheumatic traveller but for him who fears not horse and tent. Such an explorer will find thrills with every passing hour. Giant Mount Rockwell will produce one when a sideview shows that its apparent cone is merely the smaller eastern end of a ridge two miles long which culminates in a towering summit on the divide; Pumpelly Piller, with the proportions of a monument when seen from near the lake, becomes, seen sideways, another long and exceedingly beautiful ridge; striking examples, these, of the leavings of converging glaciers of old. Two Medicine Lake proves to be long and narrow, the chalet view being the long way, and Upper Two Medicine Lake proves to be an emerald-encircled pearl in a silvery-gray setting. The climax of such a several days' trip is a night among the coyotes at the head of the main valley and a morning upon Dawson Pass overlooking the indescribable tangle of peak, precipice, and canyon lying west of the continental divide.

Taken as a whole, the Two Medicine drainage-basin is an epitome of Glacier in miniature. To those entering the park on the east side and seeing it first it becomes an admirable introduction to the greater park. To those who have entered on the west side and finish here it is an admirable farewell review, especially as its final picture sounds the note of scenic perfection. Were there nothing else of Glacier, this spot would become in time itself a world celebrity. Incidentally, exceedingly lively Eastern brook-trout will afford an interesting hour to one who floats a fly down the short stream into the lakelet at the foot of Two Medicine Lake not far below the chalet. There are also fish below Trick Falls.

The Spectacle of St. Mary

St. Mary Lake, similarly situated in the outlet valley of a much greater group of cirques north of Two Medicine, offers a picture as similar in kind as two canvases are similar which have been painted by the same hand; but they widely differ in composition and magnificence; Two Medicine's preciousness yields to St. Mary's elemental grandeur. The steamer which brings our rheumatic traveller from the motor-stage at the foot of the lake lands him at the upper chalet group, appropriately Swiss, which finds vantage on a rocky promontory for the view of the divide. Gigantic mountains of deep-red argillite, grotesquely carved, close in the sides, and with lake and sky wonderfully frame the amazing central picture of pointed pyramids, snow-fields, hanging glaciers, and silvery ridges merging into sky. Seen on the way into Glacier, St. Mary is a prophecy which will not be fulfilled elsewhere in charm though often far exceeded in degree. Seen leaving Glacier, it combines with surpassing novelty scenic elements whose possibilities of further gorgeous combination the trip through the park has seemed to exhaust.

The St. Mary picture is impossible to describe. Its colors vary with the hours and the atmosphere's changing conditions. It is silver, golden, mauve, blue, lemon, misty white, and red by turn. It is seen clearly in the morning with the sun behind you. Afternoons and sunsets offer theatrical effects, often baffling, always lovely and different. Pointed Fusillade and peaked Reynolds Mountains often lose their tops in lowering mists. So, often, does Going-to-the-Sun Mountain in the near-by right foreground. So, not so often, does keel-shaped Citadel Mountain on the near-by left; also, at times, majestic Little Chief, he of lofty mien and snow-dashed crown, and stolid Red Eagle, whose gigantic reflection reddens a mile of waters. It is these close-up monsters even more than the colorful ghosts of the Western horizon which stamp St. Mary's personality.

From the porches of the chalets and the deck of the steamer in its evening tour of the lake-end the traveller will note the enormous size of those upper valleys which once combined their glaciers as now they do their streams. He will guess that the glacier which once swept through the deep gorge in whose bottom now lies St. Mary Lake was several thousand feet in thickness. He will long to examine those upper valleys and reproduce in imagination the amazing spectacle of long ago. But they are not for him. That vision is reserved for those who ride the trails.

The Scenic Climax of the Swiftcurrent

Again passing north, the automobile-stage reaches road's end at McDermott Lake, the fan-handle of the Swiftcurrent drainage-basin. Overlooking a magnificent part of each of its contributing valleys, the lake, itself supremely beautiful, may well deserve its reputation as Glacier's scenic centre. I have much sympathy with the thousands who claim supremacy for McDermott Lake. Lake McDonald has its wonderfully wooded shores, its majestic length and august vista; Helen Lake its unequalled wildness; Bowman Lake its incomparable view of glacier-shrouded divide. But McDermott has something of everything; it is a composite, a mosaic masterpiece with every stone a gem. There is no background from which one looks forward to "the view." Its horizon contains three hundred and sixty degrees of view. From the towering south gable of that rock-temple to God the Creator, which the map calls Mount Gould, around the circle, it offers an unbroken panorama in superlative.

In no sense by way of comparison, which is absurd between scenes so different, but merely to help realization by contrast with what is well known, let us recall the Yosemite Valley. Yosemite is a valley, Swiftcurrent an enclosure. Yosemite is gray and shining, Swiftcurrent richer far in color. Yosemite's walls are rounded, peaked, and polished, Swiftcurrent's toothed, torn, and crumbling; the setting sun shines through holes worn by frost and water in the living rock. Yosemite guards her western entrance with a shaft of gray granite rising thirty-six hundred feet from the valley floor, and her eastern end by granite domes of five thousand and six thousand feet; Swiftcurrent's rocks gather round her central lake—Altyn, thirty-two hundred feet above the lake's level; Henkel, thirty-eight hundred feet; Wilbur, forty-five hundred feet; Grinnell, four thousand; Gould, forty-seven hundred; Allen, forty-five hundred—all of colored strata, green at base, then red, then gray. Yosemite has its winding river and waterfalls, Swiftcurrent its lakes and glaciers.

Swiftcurrent has the repose but not the softness of Yosemite. Yosemite is unbelievably beautiful. Swiftcurrent inspires wondering awe.

McDermott Lake, focus point of all this natural glory, is scarcely a mile long, and narrow. It may be vivid blue and steel-blue and milky-blue, and half a dozen shades of green and pink all within twice as many minutes, according to the whim of the breeze, the changing atmosphere, and the clouding of the sun. Often it suggests nothing so much as a pool of dull-green paint. Or it may present a reversed image of mountains, glaciers, and sky in their own coloring. Or at sunset it may turn lemon or purple or crimson or orange, or a blending of all. Or, with rushing storm-clouds, it may quite suddenly lose every hint of any color, and become a study in black, white, and intermediate grays.

From a photograph by Bailey Willis

From a photograph by A.J. Baker

There are times when, from hotel porch, rock, or boat, the towering peaks and connecting limestone walls become suddenly so fairy-like that they lose all sense of reality, seeming to merge into their background of sky, from which, nevertheless, they remain sharply differentiated. The rapidity and the variety of change in the appearance of the water is nothing to that in the appearance of these magical walls and mountains. Now near, now distant; now luring, now forbidding; now gleaming as if with their own light; now gloomy in threat, they lose not their hold on the eye for a moment. The unreality of McDermott Lake, the sense it often imparts of impossibility, is perhaps its most striking feature. One suspects he dreams, awake.

The Scenic Circle

To realize the spot as best we may, let us pause on the bridge among those casting for trout below the upper fall and glance around. To our left rises Allen Mountain, rugged, irregular, forest-clothed half-way up its forty-five hundred feet of elevation above the valley floor. Beyond it a long gigantic wall sets in at right angles, blue, shining, serrated, supporting, apparently on the lake edge, an enormous gable end of gray limestone banded with black diorite, a veritable personality comparable with Yosemite's most famous rocks. This is Mount Gould. Next is the Grinnell Glacier, hanging glistening in the air, dripping waterfalls, backgrounded by the gnawed top of the venerable Garden Wall. Then comes in turn the majestic mass of Mount Grinnell, four miles long, culminating at the lakeside in an enormous parti-colored pyramid more impressive from the hotel than even Rockwell is from Two Medicine chalets. Then, upon its right, appears a wall which is the unnamed continuation of the Garden Wall, and, plastered against the side of Swiftcurrent Mountain, three small hanging glaciers, seeming in the distance like two long parallel snow-banks. Then Mount Wilbur, another giant pyramid, gray, towering, massively carved, grandly proportioned, kingly in bearing! Again upon its right emerges still another continuation, also unnamed, of the Garden Wall, this section loftiest of all and bitten deeply by the ages. A part of it is instantly recognized from the hotel window as part of the sky-line surrounding famous Iceberg Lake. Its right is lost behind the nearer slopes of red Mount Henkel, which swings back upon our right, bringing the eye nearly to its starting-point. A glance out behind between mountains, upon the limitless lake-dotted plain, completes the scenic circle.

McDermott Lake, by which I here mean the Swiftcurrent enclosure as seen from the Many Glacier Hotel, is illustrative of all of Glacier. There are wilder spots, by far, some which frighten; there are places of nobler beauty, though as I write I know I shall deny it the next time I stand on McDermott's shores; there are supreme places which at first glance seem to have no kinship with any other place on earth. Nevertheless, McDermott contains all of Glacier's elements, all her charm, and practically all her combinations. It is the place of places to study Glacier. It is also a place to dream away idle weeks.

So he who cannot ride or walk the trails may still see and understand Glacier in her majesty. Besides the places I have mentioned he may see, from the Cut Bank Chalet, a characteristic forested valley of great beauty, and at Lewis's hotel on Lake McDonald the finest spot accessible upon the broad west side, the playground, as the east side is the show-place, of hundreds of future thousands.

So many are the short horseback trips from Many Glacier Hotel to places of significance and beauty that it is hard for the timid to withstand the temptation of the trail. Four miles will reach Grinnell Lake at the foot of its glacier, six miles will penetrate the Cracker Lake Gorge at the perpendicular base of Mount Siyeh, eight miles will disclose the astonishing spectacle of Iceberg Lake, and nine miles will cross the Swiftcurrent Pass to the Granite Park Chalet.

Iceberg Lake Typical of All

In some respects Iceberg Lake is Glacier's supreme spectacle. There are few spots so wild. There may be no easily accessible spot in the world half so wild. Imagine a horseshoe of perpendicular rock wall, twenty-seven hundred to thirty-five hundred feet high, a glacier in its inmost curve, a lake of icebergs in its centre. The back of the tower-peak of Mount Wilbur is the southern end of this horseshoe. This enclosure was not built up from below, as it looks, but bitten down within and without; it was left. On the edge of the lake in early July the sun sets at four o'clock.

Stupendous as Iceberg Lake is as a spectacle, its highest purpose is illustrative. It explains Glacier. Here by this lakeside, fronting the glacier's floating edge and staring up at the jagged top in front and on either side, one comprehends at last. The appalling story of the past seems real.

The Climax at Granite Park

It is at Granite Park that one realizes the geography of Glacier. You have crossed the continental divide and emerged upon a lofty abutment just west of it. You are very nearly in the park's centre, and on the margin of a forested canyon of impressive breadth and depth, lined on either side by mountain monsters, and reaching from Mount Cannon at the head of Lake McDonald northward to the Alberta plain. The western wall of this vast avenue is the Livingston Range. Its eastern wall is the Lewis Range. Both in turn carry the continental divide, which crosses the avenue from Livingston to Lewis by way of low-crowned Flattop Mountain, a few miles north of where you stand, and back to Livingston by way of Clements Mountain, a few miles south. Opposite you, across the chasm, rises snowy Heavens Peak. Southwest lies Lake McDonald, hidden by Heavens' shoulder. South is Logan Pass, carrying another trail across the divide, and disclosing hanging gardens beyond on Reynolds' eastern slope. Still south of that, unseen from here, is famous Gunsight Pass.

From a photograph by Haynes

From a photograph by A.J. Thiri

It is a stirring spectacle. But wait. A half-hour's climb to the summit of Swiftcurrent Mountain close at hand (the chalet is most of the way up, to start with) and all of Glacier lies before you like a model in relief. Here you see the Iceberg Cirque from without and above. The Belly River chasm yawns enormously. Mount Cleveland, monarch of the region, flaunts his crown of snow among his near-by court of only lesser monsters. The Avenue of the Giants deeply splits the northern half of the park, that land of extravagant accent, mysterious because so little known; the Glacier of tourists lying south. A marvellous spectacle, this, indeed, and one which clears up many misconceptions. The Canadian Rockies hang on the misty northern horizon, the Montana plains float eastward, the American Rockies roll south and west.

Over Gunsight Pass

To me one of the most stirring sights in all Glacier is the view of Gunsight Pass from the foot of Gunsight Lake. The immense glaciered uplift of Mount Jackson on the south of the pass, the wild whitened sides of Gunsight Mountain opposite dropping to the upturned strata of red shale at the water's edge, the pass itself—so well named—perched above the dark precipice at the lake's head, the corkscrew which the trail makes up Jackson's perpendicular flank and its passage across a mammoth snow-bank high in air—these in contrast with the silent black water of the sunken lake produce ever the same thrill however often seen. The look back, too, once the pass is gained, down St. Mary's gracious valley to Going-to-the-Sun Mountain and its horizon companions! Sun Mountain (for short), always a personality, is never from any other point of view so undeniably the crowned majesty as from Gunsight Pass. And finally, looking forward, which in this speaking means westward, the first revelation of Lake Ellen Wilson gives a shock of awed astonishment whose memory can never pass.

Truly, Gunsight is a pass of many sensations, for, leaving Lake Ellen Wilson and its eighteen hundred feet of vertical frothing outlet, the westward trail crosses the shoulder of Lincoln Peak to the Sperry Glacier and its inviting chalet (where the biggest hoary marmot I ever saw sat upon my dormitory porch), and, eight miles farther down the mountain, beautiful Lake McDonald.

Destiny of the West Side

Although it was settled earlier, Glacier's west side is less developed than its east side; this because, for the most part, its scenery is less sensational though no less gorgeously beautiful. Its five long lakes, of which McDonald is much the longest and largest, head up toward the snowy monsters of the divide; their thin bodies wind leisurely westward among superbly forested slopes. Its day is still to come. It is the land of the bear, the moose, the deer, the trout, and summer leisure. Its destiny is to become Glacier's vacation playground.

The Coming Splendors of the North

The wild north side of Glacier, its larger, bigger-featured, and occasionally greater part, is not yet for the usual tourist; for many years from this writing, doubtless, none will know it but the traveller with tent and pack-train. He alone, and may his tribe increase, will enjoy the gorgeous cirques and canyons of the Belly River, the wild quietude of the Waterton Valley, the regal splendors of Brown Pass, and the headwater spectacles of the Logging, Quartz, Bowman, and Kintla valleys. He alone will realize that here is a land of greater power, larger measures, and bigger horizons.

And yet with Kintla comes climax. Crossing the border the mountains subside, the glaciers disappear. Canada's Waterton Lakes Park begins at our climax and merges in half a dozen miles into the great prairies of Alberta. It is many miles northwest before the Canadian Rockies assume proportions of superlative scenic grandeur.

The Belly River Valleys

To realize the growing bigness of the land northward one has only to cross the wall from Iceberg Lake into the Belly River canyon. "Only," indeed! In 1917 it took us forty miles of detour outside the park, even under the shadow of Chief Mountain, to cross the wall from Iceberg Lake, the west-side precipice of which is steeper even than the east. The Belly River drainage-basin is itself bigger, and its mountains bulk in proportion. Eighteen glaciers contribute to the making of perhaps as many lakes. The yellow mountains of its northern slopes invade Canada. The borders of its principal valley are two monster mountains, Cleveland, the greatest in the park for mass and height and intricate outline; the other, Merritt, in some respects the most interesting of Glacier's abundant collection of majestic peaks.

There are three valleys. The North Fork finds its way quickly into Canada. The Middle Fork rises in a group of glaciers high under the continental divide and descends four giant steps, a lake upon each step, to two greater lakes of noble aspect in the valley bottom. The South Fork emerges from Helen Lake deep in the gulf below the Ahern Glacier across the Garden Wall from Iceberg Lake. Between the Middle and South Forks Mount Merritt rises 9,944 feet in altitude, minareted like a mediæval fort and hollow as a bowl, its gaping chasm hung with glaciers.

This is the valley of abundance. The waters are large, their trout many and vigorous; the bottoms are extravagantly rich in grasses and flowers; the forests are heavy and full-bodied; there is no open place, even miles beyond its boundaries, which does not offer views of extraordinary nobility. Every man who enters it becomes enthusiastically prophetic of its future. After all, the Belly River country is easily visited. A leisurely horseback journey from McDermott, that is all; three days among the strange yellow mountains of the over thrust's eastern edge, including two afternoons among the fighting trout of Kennedy Creek and Slide Lake, and two nights in camp among the wild bare arroyos of the Algonkian invasion of the prairie—an interesting prelude to the fulness of wilderness life to come.

I dwell upon the Belly valleys because their size, magnificence, and accessibility suggest a future of public use; nothing would be easier, for instance, than a road from Babb to join the road already in from Canada. The name naturally arouses curiosity. Why Belly? Was it not the Anglo-Saxon frontier's pronunciation of the Frenchman's original Belle? The river, remember, is mainly Canadian. Surely in all its forks and tributaries it was and is the Beautiful River.

The Avenue of the Giants

The Avenue of the Giants looms in any forecast of Glacier's future. It really consists of two valleys joined end on at their beginnings on Flattop Mountain; McDonald Creek flowing south, Little Kootenai flowing north. The road which will replace the present trail up this avenue from the much-travelled south to Waterton Lake and Canada is a matter doubtless of a distant future, but it is so manifestly destiny that it must be accepted as the key to the greater Glacier to come. Uniting at its southern end roads from both sides of the divide, it will reach the Belly valleys by way of Ahern Pass, the Bowman and Kintla valleys by way of Brown Pass, and will terminate at the important tourist settlement which is destined to grow at the splendid American end of Waterton Lake. Incidentally it will become an important motor-highway between Canada and America. Until then, though all these are now accessible by trail, the high distinction of the Bowman and the Kintla valleys' supreme expression of the glowing genius of this whole country will remain unknown to any considerable body of travellers.

The Climax of Bowman and Kintla

And, after all, the Bowman and Kintla regions are Glacier's ultimate expression, Bowman of her beauty, Kintla of her majesty. No one who has seen the foaming cascades of Mount Peabody and a lost outlet of the lofty Boulder Glacier emerging dramatically through Hole-in-the-Wall Fall, for all the world like a horsetail fastened upon the face of a cliff, who has looked upon the Guardhouse from Brown Pass and traced the distant windings of Bowman Lake between the fluted precipice of Rainbow Peak and the fading slopes of Indian Ridge; or has looked upon the mighty monolith of Kintla Peak rising five thousand feet from the lake in its gulf-like valley, spreading upon its shoulders, like wings prepared for flight, the broad gleaming glaciers known as Kintla and Agassiz, will withhold his guerdon for a moment.

From a photograph by the U.S. Geological Survey

From a photograph by M.R. Campbell

It heads close up under the Continental Divide, where is found some of the most striking scenery of America]

Here again we repeat, for the hundredth or more time in our leisurely survey of the park, what the Englishman said of the spectacle of St. Mary: "There is nothing like it in the world."


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