"Hanging Glacier,"

"Hanging Glacier," or ice fall, above Cowlitz Glacier.

A visit to this less known but no less interesting side involves the necessity of packing an outfit. But arrangements for horses and packers are easily made, and each year an increasing number of parties make Spray Park their headquarters, spending, if they are wise, at least a week in this wide region of flowering alpine valleys and commanding heights. From there they go south, over the west-side glaciers, or east, across the Carbon and through the great White river country. They camp on the south side of the Sluiskin mountains, in Moraine Park, and there have ready access to Carbon and Winthrop glaciers, with splendid views of the vast precipices that form the north face of the Mountain. Thence they climb east and south over the Winthrop and White glaciers. They visit the beautiful Grand Park and Summerland, and either make the ascent to the summit from "Steamboat Prow" on the "Wedge," over the long ice slope of the White glacier, or continue around to the Paradise country and Longmire Springs.

Leaving the National Park Inn at Longmire Springs for Paradise Park.

Leaving the National Park Inn at Longmire Springs for Paradise Park.

On the Summit.

On the Summit, showing Columbia's Crest, the great mound of snow that has, most curiously, formed on this wide, wind-swept platform. This, the actual top of the Mountain, is 14,363 feet above sea level.
Copyright, 1909, By Asahel Curtis.

The west side has been less visited than the others, but there is a trail from the North Mowich to the Nisqually, and from this adventurous explorers reach North and South Mowich and Puyallup glaciers. No one has yet climbed the Mountain over those glaciers, or from the north side. A view from any of the trails will explain why. The great rock spines are more precipitous than elsewhere, the glaciers more broken; and the summit is fronted on either side by a huge parapet of rock which hurls defiance at anything short of an airship. Doubtless, we shall some day travel to Crater Peak by aeroplanes, but until these vehicles are equipped with runners for landing and starting on the snow, we shall do best to plan our ascents from the south or east side.

Paradise Valley or "Park".

Paradise Valley or "Park," and Tatoosh Mountains, from slope below Paradise Glacier. The highest of the peaks are about 7,000 feet above sea level and 1,700 feet above the floor of the valley.

On the Government Road a mile above Longmires.

On the Government Road a mile above Longmires, bound for the Nisqually Glacier.

Near "Gap Point".

Near "Gap Point," where the road turns from the Nisqually canyon into that of Paradise River.

I have thus briefly pointed out the favorite routes followed in exploring the National Park. The time is fast approaching when it will be a truly national recreation ground, well known to Americans in every State. The coming of new railways to Puget Sound and the development of new facilities for reaching the Mountain make this certain.[3]

Snout of Nisqually Glacier.

Snout of Nisqually Glacier, with the river which it feeds. Though much shrunken since the epoch when it filled the whole canyon, the glacier is still a vast river of ice; and its front, seen several hundred yards above the bridge, rises sheer 500 feet. The new road to Narada Falls and Paradise Park crosses the Nisqually here. Automobiles are not permitted to go above this point.

Pony bridge over the Nisqually.

Pony bridge over the Nisqually, on trail to Paradise. Note the granite boulders which the stream has rounded in rolling them down from the glacier.

Every step taken for the conservation of the natural beauty of the Park and its opening to proper use and enjoyment is a public benefit. Outside the national reserves, our lumbermen are fast destroying the forests; but, if properly guarded against fire, the great Park forest will still teach future generations how lavishly Nature plants, just as the delightful glacial valleys and towering landmarks teach how powerful and artistic a sculptor she is. Experienced travelers and alpinists who have visited the Mountain unite in declaring its scenery, combining as it does great vistas of ice with vast stretches of noble forest, to be unequaled elsewhere in America, and unsurpassed anywhere. In the fascination of its glacial story, as well as in the grandeur of its features, it has few rivals among the great peaks of the world. The geologist, the botanist, the weary business man, the sportsman, all find it calling them to study, to rest, or to strenuous and profitable recreation. Here is a resource more lasting than our timber. When the loggers shall have left us only naked ranges, without the reserves, the Park may yield a crop more valuable.

The road a mile above the bridge.

The road a mile above the bridge, overlooking Nisqually Canyon and Glacier.

On the Pony Trail to Paradise.

On the Pony Trail to Paradise. This trail winds through the dense forest above Longmires, crosses the Nisqually, and then follows Paradise River, with its miles of picturesque cascades. It is one of the most beautiful mountain paths in America.

Until recent years this was known only to the hardy few who delight in doing difficult things for great rewards. But that day of isolation has passed. The value of the Park to the whole American people is more and more appreciated by them, if not yet by their official representatives. While Congress has dealt less liberally with this than with the other great National Parks, what it has appropriated has been well spent in building an invaluable road, which opens one of the most important upland regions to public knowledge and use. This road is a continuation of the well-made highway maintained by Pierce County from Tacoma, which passes through an attractive country of partly wooded prairies and follows the picturesque Nisqually valley up the heavily forested slopes to the Forest Reserve and the southwestern corner of the Park. The public has been quick to seize the opportunity which the roads offered. The number of persons entering the Park, as shown by the annual reports of the Superintendent, has grown from 1,786 in 1906 to more than 8,000 in 1910. In the same period, the Yellowstone National Park, with its greater age, its wider advertising, its many hotels, its abundance of government money, increased its total of visitors from 17,182 to 19,575.

Sierra Club lunching on Nisqually Glacier.

Sierra Club lunching on Nisqually Glacier. The huge ice wall in the distance is the west branch of the Nisqually, and is sometimes miscalled "Stevens Glacier." As seen here, it forms a "hanging glacier," which empties into the main glacier over the cliff.

For one thing, these roads have put it within the power of automobilists from all parts of the Coast to reach the grandest of American mountains and the largest glaciers of the United States south of Alaska. They connect at Tacoma, with excellent roads from Seattle and other cities on the Sound, as well as from Portland and points farther south. The travel from these cities has already justified the construction of the roads, and is increasing every year. Even from California many automobile parties visit the Mountain. The railway travel is also fast increasing, and the opening this year of its transcontinental service by the Milwaukee Railway, which owns the Tacoma Eastern line to Ashford, is likely soon to double the number of those who journey to the Mountain by rail.

A Mountain Celery.

A Mountain Celery.

The new government road to Paradise and the trails connecting with it have, however made only a fraction of the Park accessible. The most important work for the conservation of this great alpine area and its opening to the public still remains to be done. Congress is now asked to provide funds for the survey and gradual extension of the road to the other plateaus on all sides of the peak. Pending the construction of the road, it is highly important that, as soon as the surveys can be made, bridle trails be built on the easy grades thus established. Not only are these roads and trails much needed for the convenience of visitors to the Mountain, but, with the closer approach of logging operations, they are year by year becoming more necessary to the proper policing of the Park and its protection against forest fires. For want of them, great sections of forest within the Park are liable to be swept away at any time, before the rangers could find their way over the scant and broken trails now existing. The request for better access to the other sides of the Mountain has received the earnest indorsement of the Washington legislature, the commercial organizations of the entire Coast, and the several mountain clubs in different parts of the country. Only Congress remains blind to its importance.

Narada Falls.

Narada Falls, 185 feet, on Paradise River (altitude, 4,572 feet). Both trail and road pass it. "Narada" is an East Indian word meaning "peace." The name was given many years ago by a party of Theosophists who visited the falls. Happily, the effort to change the name to "Cushman Falls" has failed.

Congressional action affecting this immediate area began in 1899. A tract eighteen miles square, 207,360 acres, to be known as "Ranier National Park,"[4] was withdrawn from the 2,146,600 acres of the Pacific Forest Reserve, previously created. The area thus set apart as "a public park for the benefit and enjoyment of the people" (Act of March 2, 1899) was already known to a few enthusiasts and explorers as one of the world's great wonderlands. In 1861 James Longmire, a prospector, had built a trail from Yelm over Mashell mountain and up the Nisqually river to Bear Prairie. This he extended in 1884 to the spot now known as Longmire Springs, and thence up the Nisqually and Paradise rivers to the region now called Paradise Park. Part of this trail was widened later into a wagon road, used for many years by persons seeking health at the remarkable mineral springs on the tract which the Longmires acquired from the government before the establishment of the Forest Reserve.

Washington Torrents.

Washington Torrents, on Paradise River; a series of falls a mile in length, seen from the new road to Paradise and still better from the pony trail.

Portion of Paradise Park and the Tatoosh Range.

Portion of Paradise Park and the Tatoosh Range.

The Longmire road, rough as it was, long remained the best route; but in 1903 the Mountain found a tireless friend in the late Francis W. Cushman, representative from this State, who persuaded Congress to authorize the survey and construction of a better highway. Work was not begun, however, until 1906. The yearly appropriations have been small, and total only $240,000 for surveys, construction and maintenance, to the end of the last session.

View from north side of the Tatoosh.

View from north side of the Tatoosh. 1. Crater Peak. 2. South Peak, or Peak Success. 3. Nisqually Glacier, with feeders. 4. Gibraltar Rock. 5. Camp Muir, on Cowlitz Cleaver. 6. Cathedral Rocks. 7. Little Tahoma. 8. Paradise Glacier. 9. Alta Vista. 10. Camp of the Clouds. 11. Reese's Camp. 12. Sluiskin Falls. 13. Paradise River and Valley. 14. Mazama Ridge. 15. Reflection Lake. 16. Van Trump Glacier. 17. Von Trump Park. 18. Kautz Glacier. 19. Pyramid Peak. 20. Tahoma Glaciers. 21. Indian Henry's. Dotted line shows South-side route to the summit.

Ice Bridge, Stevens Glacier.

Ice Bridge, Stevens Glacier.

Mountain Sports.

Mountain Sports. Tug of War between teams picked from the feminine contingent of the Mountaineers.

The road, as now open to Paradise valley, is a monument to the engineering skill of Mr. Eugene Ricksecker, United States Assistant Engineer, in local charge of the work. Over its even floor you go from the west boundary of the Forest Reserve up the north bank of the Nisqually river, as far as the foot of its glacier. Crossing on the bridge here, you climb up and up, around the face of a bluff known as Gap Point, where a step over the retaining wall would mean a sheer drop of a thousand feet into the river below. Thus you wind over to the Paradise river and famous Narada Falls, switch back up the side of the deep Paradise canyon to the beautiful valley of the same name above, and, still climbing, reach Camp of the Clouds and its picturesque tent hotel. The road has brought you a zigzag journey of twenty-five miles to cover an air-line distance of twelve and a gain in elevation of 3,600 feet. It is probably unique in its grades. It has no descents. Almost everywhere it is a gentle climb. Below Longmire Springs the maximum grade is 2.5 per cent., and the average, 1.6 per cent. Beyond, the grade is steeper, but nowhere more than 4 per cent.

Tatoosh Mountains and Paradise Park in Winter.

Tatoosh Mountains and Paradise Park in Winter.
Copyright, 1911, By J. H. Weer.

The alignment and grades originally planned have been followed, but for want of funds only one stretch, a mile and a quarter, has yet been widened to the standard width of eighteen feet. Lacking money for a broader road, the engineers built the rest of it twelve feet wide. They wisely believed that early opening of the route for vehicles to Paradise, even though the road be less than standard width, would serve the public by making the Park better known, and thus arouse interest in making it still more accessible. It will require about $60,000 to complete the road to full width, and render it thoroughly secure.

Hiking through Paradise in Winter.

Hiking through Paradise in Winter.
Copyright, 1911, By J. H. Weer.

Of still greater importance, however, to the safety of the Park and its opening to public use is the carrying out of Mr. Ricksecker's fine plan for a road around the Mountain. His new map of the Park, printed at the end of this volume, shows the route proposed. Leaving the present road near Christine Falls, below the Nisqually glacier, he would double back over the hills to Indian Henry's, thence dropping into the canyon of Tahoma Fork, climbing up to St. Andrew's Park, and so working round to the Mowich glaciers, Spray Falls, and the great "parks" on the north. The snout of each glacier would be reached in turn, and the high plateaus which the glaciers have left would be visited.

Waterfall from snowfields on ridge above Paradise Valley.

Waterfall from snowfields on ridge above Paradise Valley.
Copyright, 1910, By Asahel Curtis.

Looking from Stevens Glacier down into Stevens Canyon.

Looking from Stevens Glacier down into Stevens Canyon, and across the Tatoosh and Cascade ranges to Mt. Adams.

Crossing Spray Park, Moraine Park and Winthrop glacier's old bed, the road would ascend to Grand Park and the Sour-Dough country—a region unsurpassed anywhere on the Mountain for the breadth and grandeur of its views. More descents, climbs and detours would bring it to the foot of White glacier, and thence through Summerland and Cowlitz Park, and westward to a junction with the existing road in Paradise. Its elevation would range between four and seven thousand feet above the sea. The route, as indicated on the contour map, suggests very plainly the engineering feats involved in hanging roads on these steep and deeply-carved slopes.

Reese's Camp, a tent hotel on a ridge in Paradise Park.

Reese's Camp, a tent hotel on a ridge in Paradise Park, below Camp of the Clouds (Elevation, 5,557 feet). This is the usual starting point of parties to the summit over the South-side route, via Gibraltar. See p. 60.

Between eighty and a hundred miles of construction work would be required, costing approximately $10,000 a mile. Including the completion of the present road to standard width, Congress will thus have to provide a round million if it wishes to give reasonable protection to the Park and fully achieve the purpose of "benefit and enjoyment" for which it was created. Such a road would justify the Congress which authorizes it, immortalize the engineers who build it, and honor the nation that owns it.

Climbing the "horn" on the summit of Unicorn Peak.

Climbing the "horn" on the summit of Unicorn Peak, the highest crag in the Tatoosh (Elevation, about 7,000 feet). The man who first reached the top is dimly seen in the shadow on the left.

Stevens Canyon in October.

Stevens Canyon in October, with Mt. Adams over eastern end of Tatoosh range on right, and Cascade range on left. The snow summits on the Cascade sky-line are "Goat Peaks." Goat Lick Basin is in lower left corner of the picture.

Sluiskin Falls, 150 feet, just below Paradise Glacier.

Sluiskin Falls, 150 feet, just below Paradise Glacier, named after Sluiskin, the famous Indian who guided Van Trump and Stevens to the snow line in 1870.

Talking with President David Starr Jordan of Stanford University a few weeks ago, I found that famous climber of mountains greatly interested in the project for better roads and trails in the National Park. "How much will the whole thing cost?" he asked. I told him.

An eminent scientist practices the simple life.

An eminent scientist practices the simple life in camp near the Timber Line.

"Why, a million dollars would pay for the upkeep of one of our battleships for a whole year!" exclaimed the great advocate of disarmament. Whether Congress can be induced to value scenery as highly as battleships remains to be seen. It has already done very well by the Yellowstone National Park, where $2,142,720 of government money had been spent on road building and administration up to July 1, 1910. No one who knows the glories of that park will deem the amount excessive. But with its still grander scenery, its important glaciers, its priceless forests, and the greater population within easy reach of its opportunities for study and recreation, the claims of the Rainier National Park are at least equal to those of the Yellowstone, and they should be as liberally met.

Nisqually Glacier.

Nisqually Glacier, with its sources in the snow field of the summit. On the right is Gibraltar Rock and on the extreme left Kautz Glacier flows down from Peak Success. Note the medial moraines, resulting from junction of ice streams above. These apparently small lines of dirt are often great ridges of rocks, cut from the cliffs. The picture also illustrates how the marginal crevasses of a glacier point down stream from the center, though the center flows faster than the sides.

The Sierra Club on Nisqually Glacier.

The Sierra Club on Nisqually Glacier. This active California organization sent a large party to the Mountain in 1905.

It is not desired that the whole sum named be appropriated at once. Indeed, the recommendation of the engineers has been far more modest. As far back as 1907, Maj. H. M. Chittenden of the United States Engineer Corps, in charge, wrote as follows in his report to the Secretary of War:

A bridle trail around the Mountain, just under the glacier line, is absolutely essential to the proper policing of the Park, and very necessary for the convenience of tourists, if they are really to have access to the attractions of the Park. The trail should be so located that in time it may be enlarged into a wagon road.

Lost to the World, 7,500 feet above sea level, with an ocean of cloud rising.

Lost to the World, 7,500 feet above sea level, with an ocean of cloud rising.
Copyright, 1909, Asahel Curtis.

This recommendation has been indorsed by Major Chittenden's successor, Maj. C. W. Kutz, and may be taken as expressing the conviction of the government engineers as to the minimum of work needed in the Park at once. For the necessary surveys and the building of the trails, Mr. Ricksecker informs me that $50,000 will probably be enough. This is so insignificant in comparison with the good sought and the value of the national property to be protected and made accessible that its immediate appropriation by Congress should be beyond question. Nevertheless, half that amount has twice been asked for in measures introduced by Senator S. H. Piles, but in neither case did the appropriation pass both houses. It is to be hoped that the present Congress will give the full amount of $50,000, which will enable the surveys to be completed over the entire route, and trails to be built on most, if not all, of that route. Their widening into permanent roads will follow in due time, when the wonders of glacier, canyon and forest which they make accessible are once known.

"Sunshine."

"Sunshine." View of the Mountain from above Sluiskin Falls at 3 p. m.

"Storm."

"Storm." View near the same point an hour later.

The road recently completed to Paradise Valley should be widened, by all means, and made safer by retaining walls at every danger point. But it is doubtful whether automobiles will ever be permitted above the bridge at the Nisqually glacier. Some automobile owners regard the Park as an automobile-club preserve, and insist that nothing more be done toward the opening of its scenery or the conservation of its forest until it is made safe for them to run their touring cars into Paradise. This is unfortunate, because it betrays ignorance of the purpose of Congress in creating the National Parks, namely, the education and enjoyment of all the people, not the pleasure of a class. Moreover, no matter how wide or well-guarded the road may be above the bridge, it can never be wide enough to prevent a reckless chauffeur from causing a terrible fatality. It is necessarily a very crooked road, hung upon the high ledges of precipitous cliffs. While the road is safe for coaches drawn by well-broken horses and driven by trustworthy drivers, it would be criminal folly to open it to the crowd of automobiles that would rush to Paradise Valley. If automobiles are permitted to go beyond the Nisqually glacier, it should be only when in charge of a park officer.

Looking down on Nisqually Glacier.

Looking down on Nisqually Glacier from top of Gibraltar Rock, with storm clouds veiling the Mountain.

Measuring the Ice Flow in Nisqually Glacier.

Measuring the Ice Flow in Nisqually Glacier. In 1905 Prof. J. N. Le Conte of Berkeley, Cal., established the fact that this glacier has an average flow, in summer, of 16.2 inches a day. The movement is greater at the center than on the sides, and greater on the convex side of a curve than on the concave side. It thus is a true river, though a slow one. The measurements are taken by running a line from one lateral moraine to the other with a transit, setting stakes across the glacier at short intervals, and ascertaining the advance they make from day to day.

Even from the older and wider roads of the Yellowstone automobiles have been excluded, although there are no large cities near by, as there are here, to send hundreds of cars into that park on any pleasant day. The automobilists will be wise to accept their privilege of access to the foot of the glacier, and use it with care, too. Several serious accidents have already occurred, and if greater care is not exercised, the Interior Department will apply the Yellowstone rule, at least to the extent of stopping all cars at Longmires.

Miss Fay Fuller exploring a crevasse.

Miss Fay Fuller exploring a crevasse.
Copyright, 1897, By E. S. Curtis.

Ice Cave, Paradise Glacier.

Ice Cave, Paradise Glacier.
Copyright 1906, By A. H. Barnes.

Questions like this, involving conflict between the interests of a class and the vital needs of the Park as a public institution, give especial emphasis to the recommendation made by Secretary Ballinger on his last annual report. Owing to the great number and extent of the National Parks, and the inefficiency of the present "perfunctory policy" in their administration, Mr. Ballinger asked Congress to put the management of these institutions under a Bureau of National Parks, conducted by a competent commissioner, and organized for efficient field administration and careful inspection of all public work and of the conduct of concessionaries. Regarding the need of such a systematic and scientific organization for the development of the parks, he says:

A definite policy for their maintenance, supervision and improvement should be established, which would enable them to be gradually opened up for the convenience of tourists and campers and for the careful preservation of their natural features. Complete and comprehensive plans for roads, trails, telegraph and telephone lines, sewer and water systems, hotel accommodations, transportation, and other conveniences should be made before any large amount of money is expended. The treatment of our national parks, except as regards the Yellowstone, has not heretofore had the benefit of any well-considered or systematic plans. In all of them the road and trail problems for public travel and convenience to enable tourists to obtain the benefits of scenic beauties are primary, but sewage, water, and electric-power problems are after all of equal importance.

Fairy Falls in Goat Lick Basin, below Stevens Glacier.

Fairy Falls in Goat Lick Basin, below Stevens Glacier.

In line with Secretary Ballinger's report, Senator Flint of California introduced a bill authorizing the creation of such a bureau in the Interior Department. The bill failed to get through at the last session, but I am informed by Senator Jones that it will be reintroduced. Its purpose is of great public importance, and the indorsement of the very intelligent directors of the Sierra Club in California argues well for its form. Every person interested in the development of our National Parks to fullest usefulness and the proper conservation of their natural beauty should work for the passage of the bill.[Back to content]

Gibraltar and its Neighbors.

Gibraltar and its Neighbors, showing a mile of the deeply crevassed ice-field inside the angle of which the great crag is the apex. On the left are Cowlitz Cleaver and the Bee-Hive; on the right, Cathedral Rocks.
Copyright, 1897, By E. S. Curtis.

 

Crossing Carbon Glacier.

Crossing Carbon Glacier. On the ice slopes, it is customary to divide a large party into companies of ten, with an experienced alpinist at the head of each. Note the medial moraines on the glacier.

III.

THE STORY OF THE MOUNTAIN.

I asked myself, How was this colossal work performed? Who chiseled these mighty and picturesque masses out of a mere protuberance of earth? And the answer was at hand. Ever young, ever mighty, with the vigor of a thousand worlds still within him, the real sculptor was even then climbing up the eastern sky. It was he who planted the glaciers on the mountain slopes, thus giving gravity a plough to open out the valleys; and it is he who, acting through the ages, will finally lay low these mighty monuments, * * * so that the people of an older earth may see mould spread and corn wave over the hidden rocks which at this moment bear the weight of the Jungfrau.—John Tyndall: "Hours of Exercise in the Alps."

The life of a glacier is one eternal grind.—John Muir.

Our stately Mountain, in its youth, was as comely and symmetrical a cone as ever graced the galaxy of volcanic peaks. To-day, while still young as compared with the obelisk crags of the Alps, it has already taken on the venerable and deeply-scarred physiognomy of a veteran. It is no longer merely an overgrown boy among the hills, but, cut and torn by the ice of centuries, it is fast assuming the dignity and interest of a patriarch of the mountains.

Reflection Lake.

Reflection Lake, below Pinnacle Peak and the Mountain.
Copyright, 1897, By E. S. Curtis.

To some, no doubt, the smooth, youthful contours of an active volcano seem more beautiful than the rugged grandeur of the Weisshorn. The perfect cone of Mt. St. Helens, until recently in eruption, pleases them more than the broad dome of Mt. Adams, rounded by an explosion in the unknown past. But for those who love nature and the story written upon its face, mountains have character as truly as men, and they show it in their features as clearly.

Looking up from Cowlitz Chimneys to Gibraltar and the summit.

Looking up from Cowlitz Chimneys to Gibraltar and the summit. 1, Crater and Columbia's Crest. 2, Peak Success. 3, Upper snow fields of Nisqually Glacier. 4, Gibraltar Rock. 5, Cowlitz Cleaver. 6, Cathedral Rocks. 7, Little Tahoma. 8, Cowlitz Glacier. 9, Ingraham Glacier, emptying into the Cowlitz.

Divide of Paradise and Stevens Glaciers.

Divide of Paradise and Stevens Glaciers. Once probably separated by a chine of rock, they are now one save for a slight elevation in their bed, which turns them respectively toward Paradise Valley and Stevens Canyon.

Old Moraine of Stevens Glacier.

Old Moraine of Stevens Glacier. Now comparatively small and harmless, this glacier did heavy work in its prime. Witness, Stevens Canyon (p. 66) and this huge pile of debris, showing that some time ago the glacier, finding a cliff in its way, cut it down and dumped it here.

Nowhere is this better exemplified than in the monarch of the Cascades. No longer the huge conical pimple which a volcano erected on the earth's crust, it bears upon it the history of its own explosion, which scattered its top far over the landscape, and of its losing battle with the sun, which, employing the heaviest of all tools, is steadily destroying it. It has already lost a tenth of its height and a third of its bulk. The ice is cutting deeper and deeper into its sides. Upon three of them, it has excavated great amphitheaters, which it is ceaselessly driving back toward the heart of the peak. As if to compensate for losses in size and shapeliness, the Mountain presents the most important phenomena of glacial action to be seen in the United States.

Climbers preparing for a night at Camp Muir.

Climbers preparing for a night at Camp Muir (altitude 10,000 feet), in order to get an early start for the summit. This is on the Cowlitz Cleaver, below Gibraltar. John Muir, the famous mountain climber, selected this spot as a camp in 1888. A stout cabin should be built here to shelter climbers.

The Bee-Hive, a landmark on Cowlitz Cleaver, below Gibraltar.

The Bee-Hive, a landmark on Cowlitz Cleaver, below Gibraltar.

In its dimensions, however, it is still one of the world's great peaks. The Rainier National Park, eighteen miles square—as large as many counties in the East—has an elevation along its western and lowest boundary averaging four thousand feet above sea level. Assuming a diameter for the peak of only twenty miles, the area occupied by this creature of a volcano exceeds three hundred square miles. Of its vast surface upwards of 32,500 acres, or about fifty-one square miles, are covered by glaciers or the fields of perpetual snow which feed them. A straight line drawn through from the end of North Tahoma glacier, on the west side, to the end of White glacier, on the east, would be thirteen miles long. The circumference of the crest on the 10,000-foot contour is nearly seven miles. Its glacial system is, and doubtless has long been, the most extensive on the continent, south of Alaska; it is said by scientists to outrank that of any mountain in Europe. The twelve primary glaciers vary in length from three to eight miles, and from half a mile to three miles in width. There are nearly as many "interglaciers," or smaller ice streams which gather their snow supply, not from the névé fields of the summit, but within the wedges of rock which the greater glaciers have left pointing upward on the higher slopes.

Mazama Club on Cowlitz Chimneys.

Mazama Club on Cowlitz Chimneys, looking across the ice-stream of the Cowlitz Glacier.

Climbing Cowlitz Cleaver to Gibraltar.

Climbing Cowlitz Cleaver to Gibraltar. This hacked and weather-worn spine left by the glaciers forms one wing of a great inverted V, with Gibraltar as its apex. On the other side of it is a drop of several thousand feet to Nisqually Glacier.

The geological story may be told in a few untechnical words. As those folds in the earth's crust which parallel the coast were slowly formed by the lateral pressure of sea upon land, fractures often occurred in the general incline thus created. Through the fissures that resulted the subterranean fires thrust molten rock. In many cases, the expulsion was of sufficient amount and duration to form clearly defined volcanic craters. The most active craters built up, by continued eruptions of lava and ashes, a great series of cones now seen on both sides of the Cordillera, that huge mountain system which borders the Pacific from Behring sea to the Straits of Magellan. Tacoma-Rainier is one of the more important units in this army of volcanic giants.

Mazamas rounding Gibraltar.

Mazamas rounding Gibraltar—a reminiscence of the ascent by the Portland club in 1905. The precipice rises more than 1000 feet above the trail which offers a precarious footing at the head of a steep slope of loose talus.

Unlike some of its companions, however, it owes its bulk less to lava flows than to the explosive eruptions which threw forth bombs and scoriae. It is a mass of agglomerates, with only occasional strata of solid volcanic rock. This becomes evident to one who inspects the exposed sides of any of the canyons, or of the great cliffs, Gibraltar Rock, Little Tahoma or Russell Peak. It is made clear in such pictures as are on this page and the next.

This looseness of structure accounts for the rapidity with which the glaciers are cutting into the peak, and carrying it away. Most of them carry an extraordinary amount of debris, to be deposited in lateral or terminal moraines, or dropped in streams which they feed. They are rivers of rock as well as of ice.

Under the walls of Gibraltar.

Under the walls of Gibraltar.

That the glaciers of this and every other mountain in the northern hemisphere are receding, and that they are now mere pygmies compared with their former selves, is well known. What their destructive power must have been when their volume was many times greater than now may be judged from the moraines along their former channels. Some of these ridges are hundreds of feet in height. As you go to the Mountain from Tacoma, either by the Tacoma Eastern railway or the Nisqually canyon road, you find them everywhere above the prairies. They are largest on the north side of the Mountain, because there the largest glaciers have been busy. Many of them, on all sides, are covered with forests that must be centuries old.