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YOSEMITE AND ITS HIGH SIERRA BY JOHN H WILLIAMS

YOSEMITE AND ITS HIGH SIERRA BY JOHN H WILLIAMS

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Page 1: YOSEMITE AND ITS HIGH SIERRA BY JOHN H WILLIAMS

YOSEMITE AND ITSHIGH SIERRABY JOHN H WILLIAMS

Page 2: YOSEMITE AND ITS HIGH SIERRA BY JOHN H WILLIAMS

On the Coulterville Road through Pierced Grove of Big Trees.

ILLUSTRATED BOOKS BY JOHN H . WILLIAMS

"THE MOUNTAIN THAT WAS ` GOD ' "

" THE GUARDIANS OF THE COLUMBIA "

" THE CANOE AND THE SADDLE "BY THEODORE WINTHROP

to which are now first added his WESTERN LETTERS

AND JOURNALS . Edited with an Introduction

and Notes by John H. Williams .

Page 3: YOSEMITE AND ITS HIGH SIERRA BY JOHN H WILLIAMS

"There is no death ; love paid the debt;Tho' moons may wane and men forget,The mountain 's heart beats on for aye;IPlho truly loved us cannot die ."

And so I wait, nor fear the tideThat comes so swiftly on to hideMy little light. The mountains glow;1 have their promise, and I know.

—Richardson : "The Promise of the Sierra ."

Page 4: YOSEMITE AND ITS HIGH SIERRA BY JOHN H WILLIAMS

+IIl~linu.Iltlpl n l n

1,111'A . IRII,F1 1 .~ I

'1'Iie ( iw . . of '1 u .w•ulilr .

Page 5: YOSEMITE AND ITS HIGH SIERRA BY JOHN H WILLIAMS

YOSEMITEand its HIGH SIERRA

By JOHN H . WILLIAMSAuthor of "THE MOUNTAIN THAT WAS ` GOD'"

" THE GUARDIANS OF THE COLUMBIA" etc.

WITH MORE THAN TWO HUNDRED ILLUSTRATIONS

INCLUDING EIGHT COLOR PLATES FROM

PAINTINGS BY CHRIS JORGENSEN

TACOMA AND SAN FRANCISCOJOHN H. WILLIAMS

1914

Page 6: YOSEMITE AND ITS HIGH SIERRA BY JOHN H WILLIAMS

The "Washington" and ''Lincoln," Giant Sequoias inMariposa Grove.

COPYRIGHT, 1914, eY JOHN H . WILLIAMS

Page 7: YOSEMITE AND ITS HIGH SIERRA BY JOHN H WILLIAMS

On the Summit of Clouds Rest, looking southeast over Little Yosemite and the MercedCanon to Mt. Clark.

TO

THE SIERRA CLUBTHIS VOLUME ABOUT A NOBLE REGION

WHICH PP HAS LABORED TO CONSERVE AND MAKE ACCESSIBLE

IS CORDIALLY DEDICATED

Have you gazed on naked grandeur where there' snothing else to gaze on,

Set pieces and drop-curtain scenes galore,Big mountains heaved to heaven, which the blinding

sunsets blazon,Black canons where the rapids rip and roar?

*

*

*

*

*

Have you seen God in His splendors, heard the textthat Nature renders,

You'll never hear it in the family pew,The simple things, the true things, the silent men

who do things?Then listen to the Wild—it' s calling you.

—Robert tr. Service.

Starting for the Ascent of Mt . Lyell .

Page 8: YOSEMITE AND ITS HIGH SIERRA BY JOHN H WILLIAMS

North Dome, Royal Arches and Washington Column, seen fromthe Merced River. The concentric formation in the granite,which is characteristic of the Yosemite region, is nowherebetter shown. The imposing architectural aspect of thisgroup, as if it were the ruins of some vast, decaying me-dieval cathedral, with crumbling arches and broken cam-panile, makes it the most interesting rock feature in theValley.

Page 9: YOSEMITE AND ITS HIGH SIERRA BY JOHN H WILLIAMS

The Half Dome, seen from the Overhanging Rock at Glacier Point, more than half a mileabove the floor of Yosemite.

FOREWORD

The present addition to my series about the great mountains of the West will servea happy purpose if it does no more than to gain new readers for the splendid books onYosemite that have preceded it. One who follows in the footsteps of J . D. Whitney,Clarence King, Galen Clark, John Muir, and Smeaton Chase must needs enter upon histask with diffidence . Nevertheless, it is largely a new work that I have undertaken,namely, to describe and exhibit, not merely the famous Yosemite Valley, but the entireYosemite National Park, so far as may be possible, by the aid of telling pictures . Thefield is so vast, its mountains, canons, lakes, waterfalls, and forests are so important andspectacular, that even the unprecedented number of illustrations given here can onlysuggest its riches of wonder and beauty . In order to make room for the largest numberof views, I have confined my text to those matters which persons visiting Yosemite forthe first time may naturally wish to know,—an outline of the great physical features ofthe Yosemite country and their causes, the story of its native inhabitants and theirworthy but pathetically hopeless fight to hold their alpine fastness, and the increasingfacilities for the enjoyment of its renowned valleys and equally inviting highlands . Ishall feel it no defect in this brief essay if among my readers some Oliver Twist mayperchance ask for more!

The choosing of more than two hundred illustrations from many thousands of photo-graphs involved no little labor . Much of the district was, until lately, very inadequatelyphotographed . Yosemite Valley has long been the best illustrated scenic spot in America,but the wonderful High Sierra back of it has been surprisingly neglected by the profes-sional photographers . Fortunately for this book, however, the large membership of theSierra Club includes many expert amateurs, and the club's different expeditions into themountains have produced a multitude of photographs that are equal to the best pro-fessional work . My first acknowledgment must therefore be to the photographers amongmy fellow-members for the unanimity with which they have placed their negatives at mydisposal . Without such help, it would have been possible to show little more than thebeaten paths of Yosemite Valley and the Big Tree Groves . I am also indebted to the pas-senger departments of the Southern Pacific, Santa Fe and Yosemite Valley Railways formany fine photographs ; to the professional photographers, Messrs . Fiske, Pillsbury, Tib-bitts, Boysen and others, for their interest and cooperation, and to Mr . M. M . O' Shaugh-nessy, City Engineer of San Francisco, for invaluable photographs of Hetch Hetchy .

Page 10: YOSEMITE AND ITS HIGH SIERRA BY JOHN H WILLIAMS

IO

FOREWORD

Thanks are also due to the directors of the Bohemian Club of San Francisco for per-mission to reproduce Mr . Chris Jorgensen's spirited painting of Yosemite from Inspira-tion Point . The book is much enriched by this picture and by the others painted by Mr.Jorgensen especially for it.

Mr . William E . Colby, the Sierra Club's untiring secretary, has kindly read proofs,and aided me greatly with his expert counsel . Prof. C . A. Kofoid and Prof. Willis LinnJepson, of the University of California, Rev . Joseph S. Swain , of Cambridge, Mass ., Mr.Russ Avery, of Los Angeles, Mr . Mark A . Daniels, of San Francisco, Superintendent of theNational Parks, Messrs . Herbert Bashford and Homer T . Miller, of the same city . MisaMary A. Byrne, of the San Francisco Public Library, and Mr. John B . Kaiser, of theTacoma Public Library, have made me their debtor by many courtesies . I must alsothank the Houghton-Mifflin Company , of Boston ; the Century Company, of New York, andthe Blair-Murdock Company and Mr . A. M. Robertson, of San Francisco, for liberty toquote from copyrighted works of Muir, Burt, Chase, Symmes, Sterling and Richardson.

This book is an acknowledgment of a long-standing debt to the Sierra. Years ago,while a resident of California, I became a lover of her mountains . It has since been mygood fortune to study other great mountain districts, and to learn that each has its ownspecial inspiration ; but on returning to the Yosemite upland after a decade of absence,I have still found in its nobly sculptured heights and gentle valleys a peculiar and lastingcharm possessed by no other wild landscape, American or European, with which I am ac-quainted , —a mingling of sublimity and tenderness that should make it the joy of allAmericans, and the best-guarded treasure of California.

"With frontier strength ye stand your ground;With grand content ye circle round,Tumultuous silence for all sound, . . .Like some vast fleet,Sailing through winter's cold and summer's heat;Still holding on your high emprise,Until ye find a home amid the skies ."

Tacoma. Nov . 15, 1914.

Jack Main Cation and Wilmer Lake, north of Retch Hetehy Valley .

Page 11: YOSEMITE AND ITS HIGH SIERRA BY JOHN H WILLIAMS

Lunch Time on the Tuolumne, at the Sierra Club's Camp near Soda Springs.

CONTENTS

L THE YOSEMITE NATIONAL PARK 17

II. THE CA\ON OF YOSEMITE 61

III. ON THE CALIFORNIA SKY-LINE 93

IV. TUOLUMNE GRAND CAI\ON AND HETCH HETCHY 113

V. THE "KING OF THE FOREST" 137

NOTES 143

ILLUSTRATIONS

The * indicates engravings from copyrighted photographs . See notice under theillustration .

FOUR-COLOR HALFTONES

From paintings by Chris Jorgensen.

The Canon of Yosemite By courtesy of the Bohemian Club

4Cathedral Rocks and Spires 19Yosemite Falls, seen from the Merced Meadows 24Cascades at the Head of Happy Isles 41Half Dome in the Alpen-Glow 60Vernal Fall 77Mt. Lyell and its Glacier 111in Mariposa Grove 130

ONE-COLOR HALFTONES.

Title

Photographer

PageOn the Coulterville Road S . A . Gray

2"'Washington" and "Lincoln" Trees, Mariposa Grove

H . C. Tibbitts

6On the Summit of Clouds Rest Pillsbury Picture Co .

7Starting for the Ascent of Mt. Lyell Pillsbury Picture Co .

7Royal Arches and the Merced River H . C. Tibbitts

8Half Dome , from Overhanging Rock, Glacier Point

H . C . Tibbitts

9Jack Main Canon J . F . Kinman 10Lunch Time on the Tuolumne Pillsbury Picture Co . 11The Gates of Yosemite Pillsbury Picture Co . 16Regulation Peak and Rodgers Lake J . F. Kinman 17

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I2

ILLUSTRATIONS

Title Photographer

PageReturning from Summit of Mt. Hoffman Dr . Edward Gray 17Upper Yosemite Fall Arthur W. Wilding 18Bridal Veil Fall Pillsbury Picture Co . 20Sentinel Rock (2) Fiske and Pillsbury 21A Glacier Landscape : Tuolumne Canon C . H. Hamilton 22Another Glacier Landscape :

Mt . Starr King, etc . George R. King 22El Capitan, from East Side George Fiske 23First View of Lyell and its Neighbors Prof. Everett Shepardson 25White Cascade, in Tuolumne River Walter LeRoy Huber 25Indian Grist-Mill George R. King 26Snow-Creek Falls Lena M. Reddington 26Three Brothers H . C . Tibbitts 27The Domes in a Winter Storm Pillsbury Picture Co . 28Two North-side Lakes (2) J . F. Kinman 29"Apron" and Glacial Tarn, in Little Yosemite Hazel E . Roberts 29Cathedral Peak Walter LeRoy Huber 30Dome at Head of Tenaya Lake Pillsbury Picture Co . 30View East from Glacier Point J. T . Boysen 31The "Governor Tod" Group Pillsbury Picture Co . 32A Study in Clouds and Mountains Clinton C . Clarke 33Buttercups Following Retreat of the Snow Clinton C . Clarke 33Washburn Lake J . T . Boysen 34North Dome, seen from Happy Isles H . C . Tibbitts 34The Tuolumne Grand Canon Walter LeRoy Huber 35The Terraced Walls of Hetch Hetchy Pillsbury Picture Co . 36Giant Sequoias at Cabin in Mariposa Grove H . C . Tibbitts 37View South from Kuna Crest Walter LeRoy Huber 38White Firs on Eagle Peak Trail Prof . George J . Young 38Mt. Dana, seen from Tioga Lake H. E. Bailey 39Sugar Pine Loaded with Cones George R . King 40Crossing Cold Canon Meadows Ruth I . Dyar 40View down from Clouds Rest J . T . Boysen 42Yosemite Squaw, with Papoose J . T . Boysen 43Polemonium near Parker Pass Rose M. Higley 43Mono Pass ; with Bloody Canon and Mono Lake (2) Francis P . Farquhar 44*Happy Hours! (Deer in the Park) J . T . Boysen 44Sardine Lake in Bloody Canon J . T . Boysen 45Mt . Hoffman, from Snow Flat on the Tioga Road Philip S . Carlton 45Yosemite Valley, seen from Yosemite Falls Trail George Fiske 46Distinguished Visitors to the Grizzly Giant Pillsbury Picture Co . 46Western End of Yosemite, from Union Point George Fiske 47Indian Acorn Cache H . C. Tibbitts 48Tenaya Peak , with Tenaya Lake Pillsbury Picture Co . 48In Tenaya Canon (2) Prof . J . N . Le Conte 49Tenaya Lake J. T. Boysen 50Gates of Tenaya Canon in Winter George Fiske 51South Merced Valley, from Lookout Point J. T. Boysen 52A Yosemite Wood-Gatherer George Fiske 52Mirror Lake and Mt. Watkins Pillsbury Picture Co . 53Yosemite Indian Basket-Maker J. T . Boysen 54"Umbrella Tree" George Fiske 54Wild Flowers beneath the Royal Arches Pillsbury Picture Co . 55The "Forest Queen" in the Mariposa Grove J . T . Boysen 56*"Watch Me!" (Bear Cub) J . T . Boysen 56*On the Overhanging Rock in Winter Pillsbury Picture Co . 57Blue Jay in Merced Canon Prof . Everett Shepardson 57John Muir in Hetch Hetchy George R. King 58Ready for the Trails H . C . Tibbitts 58Tenaya Canon and Half Dome, from Glacier Point George Fiske 59Merced River and the Forest in Yosemite H . C. Tibbitts 61Lost Arrow Trail H. C. Tibbitts 61Chilnualna Falls, near Wawona J . T. Boysen 62"New England Bridge," at Wawona George Fiske 62Bridal Veil Meadow H. C . Tibbitts 63

Page 13: YOSEMITE AND ITS HIGH SIERRA BY JOHN H WILLIAMS

ILLUSTRATIONS

13

Title

Photographer

PageOn Wawona Road George Fiske 63The Merced River above El Portal Pillsbury Picture Co . 64Cascade Falls J . T . Boysen

65Bridal Veil Fall in Early Winter George Fiske 66Winter Sports in Yosemite Philip S . Carlton

66El Capitan and Three Brothers Pillsbury Picture Co .

67A Glimpse of North Dome George Fiske 67North Wall of Yosemite Valley Pillsbury Picture Co . 68Panoramic View East from Washburn Point Pillsbury Picture Co . 68Cathedral Rocks and Spires Pillsbury Picture Co .

69The "Back Road," South Side of Yosemite George Fiske 70Yosemite Falls, seen from North-side Trail Pillsbury Picture Co.

71Cliff at Head of Yosemite Falls U . S. Geological Survey 72Leopard Lily Arthur W. Wilding 72Evening Primroses and the Half Dome Pillsbury Picture Co . 73Ice Cone at Upper Yosemite Fall (2) George Fiske 74Overhanging Rock at Glacier Point George Fiske 75Glacier Point Jutting into Yosemite Pacific Photo and Art Co .

76-Illilouette Fall Pillsbury Picture Co .

78The Merced at Happy Isles (2) Pillsbury Picture Co.

79Le Conte Memorial George Fiske 80The "Fallen Monarch" U . S . Forestry Bureau 80Vernal Fall, from Clark's Point George Fiske

81Vernal Fall in Winter George Fiske 82At the Head of Nevada Fall W. J. Grow 82The "Cataract of Diamonds" Pillsbury Picture Co .

83Little Yosemite, from Liberty Cap Pillsbury Picture Co .

83Nevada Fall (2) Pillsbury Picture Co .

84Little Yosemite, with Clouds Rest George Fiske 85Sugar-Loaf Dome, in Little Yosemite George Fiske 85Climbing the Half Dome (2) R. O . Quesnal 86Overhang at Summit of Half Dome R . O. Quesnal 87Phlox Pillsbury Picture Co .

87Half Dome at Sunrise Violet Ehrman 88On the "Short Trail" to Glacier Point Pillsbury Picture Co .

88Lake Merced J . T. Boysen 89A Characteristic Dome Landscape Pacific Photo and Art Co. 90Sentinel Dome George Fiske 90Jeffrey Pine on Sentinel Dome Pillsbury Picture Co .

91Aspen Forest at Lake Merced W. W. Lyman 92Triple Divide Peal: William Templeton Johnson 93Climbing Mt . Clark F . R. v. Bichowsky 93Tuolumne Pass (2)

. . .

Clair S . Tappaan and Dr. Edward Gray 94On Lake Washburn at Sunset W. W. Lyman 94Vogelsang Pass and Vogelsang Peak Pillsbury Picture Co. 95View South from Vogelsang Pass Pillsbury Picture Co. 95Summer Snowfields in the Sierra (3) Charles W . Michael 96Cathedral Peak, from Cathedral Pass J . Floyd Place 97Looking up Lyell Fork of the Tuolumne Prof. Everett Shepardson 98Pack Train at Vogelsang Pass Pillsbury Picture Co . 98Kuna Crest, from Meadows near Mono Pass Rose M. Higley 99Mountain Hemlocks Ruth I. Dyar 99In Alpine California (2) . . .

Prof . E . Shepardson and F. P. Farquhar 100Cutting Steps up Snow-Finger on Mt . Lyell Walter LeRoy Huber 100Luncheon on Lyell Summit Pillsbury Picture Co. 101Sierra Club Climbing Mt . Lyell Pillsbury Picture Co. 101Rodgers, Electra and Davis Peaks J . Floyd Place 102A Convenient Crack Clinton C. Clarke 102Summit of Mt . Lyell Prof. Everett Shepardson 103The "Bergschrund" of Lyell Glacier H. E. Bailey 104The Uplands in July : Echo Peak from Unicorn Francis P . Farquhar 104Mts. Dana and Gibbs (2) Ruth I . Dyar 105The Craters of Mono County J . T . Boysen 105Summit of Mt. Conness (2) F. R. v. Bichowsky 106

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14

ILLUSTRATIONS

Title Photographer PageCathedral Peak Range, from Tuolumne Meadows

. Philip S . Carlton 107Tenaya Lake, from Old Tioga Road Pillsbury Picture Co . 10SLambert Dome and Tuolumne Meadows Pillsbury Picture Co . 10SMatterhorn Cation, from its East Slope Ruth I . Dyar 109The Hammond Fly-Catcher Rose M. Higley 109View East, from Benson Pass Walter LeRoy Huber 110Snow Plant J . T . Boysen 110Mts . Ritter and Banner, from Shadow Lake Walter LeRoy Huber 112Group of 250-foot Sequoias U . S . Forestry Bureau 113Nearing the Summit of Mt . Lyell Pillsbury Picture Co . 113Piute Mountain and Lakelet in Seavey Pass C . H. Hamilton 114A Typical Glacial Cirque U . S . Geological Survey 114Upper Hetch Hetchy, from Le Conte Point Walter LeRoy Huber 115Coasting on the Granite Pillsbury Picture Co . 115Lower End of Tuolumne Meadows, from Lambert Dome

. Ruth I. Dyar 116Cathedral Creek Falls Robert L . Lipman 116Glen Aulin and Wildcat Point Philip S . Carlton 117Spermophiles at Conness Creek Ruth I . Dyar 117Tuolumne Falls Walter LeRoy Huber 118Grand Cation of the Tuolumne River Walter LeRoy Huber 119Largest of the Waterwheels Francis P . Farquhar 120A Fair Knapsacker Lucile R . Grunewald 120Waterwheel Falls, Tuolumne Canon Francis P . Farquhar 121Benson Lake (2) Prof . Ralph R . Lawrence 122Cookstoves on the March Ruth I. Dyar 122Rodgers Lake Rose M. Higley 123Heart of Tuolumne Canon ; Entrance to Muir Gorge (2)

. Francis P. Farquhar 124*Lower End of Muir Gorge Francis M. Fultz 125Little Hetch Hetchy John S. P . Dean 126Weighing the Dunnage

.

.

. Elizabeth Underwood 126River, Meadow and Forest, in Hetch Hetchy Pillsbury Picture Co . 127Waterfalls and Cascades in Tuolumne Canon

.

. Pillsbury Picture Co . 127Sunrise in Hetch Hetchy Rose M. Higley 12SUnnamed Lake in Eleanor Canon J . F. Kinman 12SThe "Twins" Walter LeRoy Huber 129Five-Finger Falls, in Hetch Hetchy Walter LeRoy Huber 131Lake Eleanor J . F . Kinman 131Central Hetch Hetchy Taber Photo Co . 132Upper Hetch Hetchy H. B . Chaffee 133Yellow Pines George Fiske 134Overhanging Rock at Eleanor Carton Robert Schaezlein, Jr. 134Lower Hetch Hetchy H. B . Chaffee 135A Contemporary of Noah :

the "Grizzly Giant" H. C. Tibbitts 136Cavalrymen at Cabin in Mariposa Grove Pillsbury Picture Co . 137A Fish Story from Laurel Lake J . F . Kinman 137Wawona Meadows and South Merced Valley J . T . Boysen 13SRed Fir Meyer Lissner 139"Alabama ." in the Mariposa Grove J . T . Boysen 139

140Maul Oak, on Wawona Road H. C . TibbittsMariposa Lily Prof . Ralph R. Lawrence 140The "King of the Forest" (2) Walter LeRoy Huber 141Three Veterans E . N . Baxter 142Del Portal Hotel , at El Portal J . T . Boysen 143Camp Curry

(2) Pacific Photo and Art Co . 144Watching the Sunrise at Mirror Lake Pillsbury Picture Co . 145

MAPS

From Yosemite Valley to Wawona and Mariposa Grove, Drawn by Chris Jorgensen 146Travel-Guide Map, Yosemite National Park . U. S . Geological Survey . Inside Back CoverYosemite Valley . Drawn by Chris Jorgensen Inside Back Cover

Page 15: YOSEMITE AND ITS HIGH SIERRA BY JOHN H WILLIAMS

THE GATES OF YOSEMITE.

Here the glacier ground thestone,

Here spake God and it wasdone;

Buttress, pinnacle and wall,

River, forest, waterfall,

And God' s right hand overall.

Hear the mountain torrentscall,

Swung colossal from thesteep;

See them, wind-tossed, waveand sweep ;

Hear them sound like harp-er ' s hands

On the quivering granitestrands,

Now with thunderous thudand moan,

Now with giant undertone;

While the pine trees whis-per low,

And the sunset ' s shadowsslow

Up the vast gnarled ridgesgo

To the roseate far snow.

—Rev. Joseph Cook:"Yosemite"

"Soon, quitting the narrow, cluttered wildness of the lower river, thenewcomer is face to face with the ordered peace and glory of the EnchantedValley . Here, fully spread before him, is that combination or sylvan charmwith stupendous natural phenomena which makes Yosemite unique amongEarth's great pictures. He sees the canton's level floor, telling, of an ancientglacial lake that has given place to wide, grassy meadows ; fields of glad

mountain flowers ; forests of many greens and lavenders ; the fascinationof the winding Merced; and, gleaming high above this world of gentleloveliness, the amazing gray face of El Capitan, while Pohono drops froma `banging valley' superbly sculptured, and so beautiful that he maywell deem it the noblest setting Nature has given to any of her famouswaterfalls ."—P . 66 .

Page 16: YOSEMITE AND ITS HIGH SIERRA BY JOHN H WILLIAMS

Regulation Peak (el . 10,500 ft .), and Rodgers Lnke, the best known of many beautifulmountain lakes in the northern part of the Park.

YOSEMITE AND ITS HIGH SIERRA

I.

THE YOSEMITE NATIONAL PARK

God of the open air,To Thee I make my prayer . .

By the breadth of the blue that shines in silence o'er me,By the length of the mountain lines that stretch before me,By the height of the cloud that sails, with rest in motion,Over the plains and the vales to the measureless ocean(Oh, how the sight of the things that are great enlarges the eyes!),Lead me out of the narrow life to the peace of the hills and the skies.

—Henry Van Dyke.

THE Yosemite Country invites all lovers of the thronging mountains.It offers the enjoyment of a landscape famous for its elements ofsurprise and wonder. It promises the lasting interest of upland

grandeur, softened by the beauty of lake and forest, flowers and fallingwaters. A land of superlatives, it may truthfully boast the most splendidhigh-walled valleys, theloftiest cataracts, the oldest,stateliest, and most note-worthy trees, in the world.It multiplies the delightsof mountaineering with thenmost equable of sunny

if* ,'mountain climates . Finally,—and this is its loudest callto thousands of true nature-lovers,—it presents a legible

Returning from the Summit of :lit . Hoffman.

Page 17: YOSEMITE AND ITS HIGH SIERRA BY JOHN H WILLIAMS

IS

YOSEMITE AND ITS HIGH SIERRA

Upper Yosemite Fall, seen from Yosemite Point Trail.In its drop of 1,430 feet, the stream, even at flood,becomes a cloud of spray, which the wind catchesas on a cushion, and sways from side to side.

and absorbing record of themaking of great scenery.

It is a commonplace offoreign visitors of the boule-vard type, and of some Ameri-cans who know the towns andspas of Europe better than theglory of their own land, thatthe mountain scenery of West-ern America is a scenery ofmere savage bigness, ratherthan of predominant beauty.This easy complaint may becharged in good part to ourmodern demand for luxury,and will be forgotten with themultiplication of automobileroads and expensive hotels . Afashionable inn on its summithas made many a third-ratehill in Europe the goal ofspell-bound tourists, includingdroves of our globe-trottingfellow-countrymen . Neverthe-less, the trite criticism has in ita half-truth . It is true of theRocky Mountain and Sierrasystems to the same extent thatit is true of the Swiss plateaussupporting the great snowpeaks, or the Tyrolese up-lands, or the cirque countryof the Pyrenees . The beautyof such scenes is not to bemeasured on the scale ofcountry estates and well-trimmed pastoral landscape.

High mountain lands butlately abandoned by ice-sheetand glacier wear similar as-pects the world over . Theyare the seats of sublimityrather than of the picturesque.Their fascination lies not somuch in softness of detail as,

Page 18: YOSEMITE AND ITS HIGH SIERRA BY JOHN H WILLIAMS

. There the sun himself .

Cathedral Rocks and Spires.

At the calm close of summer's longest day,Rests his substantial orb ; between those heightsSparkle the stars, as of their station proud.—Wordsworth .

Page 19: YOSEMITE AND ITS HIGH SIERRA BY JOHN H WILLIAMS

Bridal Veil Pall, the Indian Pohono . Dropping 620 feet, with 200 feet of cascades below it, this fis noteworthy in its setting, and perhaps the most graceful in form of all the Yosemite eatracts . Note the °°comets"—arrow-lil.-e masses of water shooting out from the fall .

Page 20: YOSEMITE AND ITS HIGH SIERRA BY JOHN H WILLIAMS

THE YOSEMITE NATIONAL PARK

2I

in breadth of view, in strength of line and majesty of form . They conjurewith a story of their master sculptor, the Sun, wielding vast tools of iceand snow and rush-ing torrent, to blockout peak and range,to lay broad glacialvalleys deep withsoil, to plant thehighland lakes, andto smooth the widerock benches, which,even yet unweath-ered, refuse welcometo forest or farm .

Sentinel Rock, seen frontthe east and west—thegreat, glacier-carved cliffrising 3,086 feet on thesouth side of the valley,opposite Three Brothers.The perpendicular frontof the Sentinel, sheer forhalf its height, showshow the cleavage has fol-lowed vertical jointing inthe granite.

In such alpine re-gions, whether of Eu-rope or America, thereal out-door man needsno handbook of scienceto interpret their report

elemental forces, busy until comparatively recent time. Nor does the wild--tss of their scenes, or the slight effort needed to attain them, weigh against

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22

YOSEMITE AND ITS HIGH SIERRA

the inspiration whichhe prizes more thancomfort . He is notoffended by the ab-sence of those sylvan'graces common onlyto the older low-lands. And if, hap-pily, prodigal Na-ture, in her bounty,should set down adelightful picture ofgentler beauty inthe midst of hermountain grandeurs,he appraises it themore justly for itsmighty surround-

ings. The ancient hills, he knows, are man's oldest and unfailing friends;their service, past and present, in making the earth inhabitable calls for histribute ; and year after year finds him returning with joy to learn theirlessons and receive their strength . As Maxwell Burt gaily sings,

There is no good denying it,If you be mountain born,

You hear the high hills callingLike the echo of a horn;

Like the echo of a silver horn that threads the golden day,You hear the high hills calling, and your heart goes away.

The character and accent of mountain landscape at its best distinguishthe whole of the Yosemite National Park . Its area of 1,124 square miles

Another Glacier Landscape : The domes of Mt. Starr King (right), with the Mt. Clarkgroup and its cirques beyond, forming the Illilouette water-shed.

A Glacier Landscape : Tuolumne Canon, where many thousandsof years ago, the great Tuolumne Glacier left its record inthe deep trough and polished granite slopes .

Page 22: YOSEMITE AND ITS HIGH SIERRA BY JOHN H WILLIAMS

El Capitan (the Captain), with early morning sunlight on its east face . One needs theaid of figures to appreciate the magnitude of this vast block of unjointed granite. Thebrow of El Capitan is 3,100 feet above the Merced River ; its actual summit is 500 feethigher . Each face of the cliff exceeds 160 acres in area . A lone tree growing on aledge under the arch seen in the shadow- on the right is more than eighty feet high .

Page 23: YOSEMITE AND ITS HIGH SIERRA BY JOHN H WILLIAMS

Yosemite Falls, seen from the Merced Meadows.

The cataracts blow their trumpets from the steep ; . .I hear the echoes through the mountains throng,

The winds come to me from the fields of sleep.—Wordsworth.

Page 24: YOSEMITE AND ITS HIGH SIERRA BY JOHN H WILLIAMS

THE YOSEMITE NATIONAL PARK

25

i'Frst View of Lyeil and its Neighbors, from the Lyell Fork of the Tuolumne . Mts. Lyelland McClure are seen on the sky-line . right of center.

::mbines the most rugged wildness with innumerable scenes of composedbeauty- . Extending from an average elevation of 4,500 feet on its westernBoundary to the snowy summits of the Sierra Nevada Range, at more than

;.000 feet, it includes the watersheds of two important rivers, the Mercedand the Tuolumne, and embraces a variety of upland scenery unequaled inmy other of our national parks.

Each of these great public outing grounds has its own especial inter-the Colorado Grand Canon, its vast gorge, with an infinite variety in

the forms and coloring of the river-sculptured rock ; the Rainier Park, itssangle volcanic peak,:7 posing beyond:ter Americanmountains, snow-crowned, and radi-E_ing a score of hugeg:aciers down itsdensely forestedf apes : the Yellow-Kone, its wonderfulthermal basins andteirgeysers ;thenewGlacier Park, likethe still grander Ca-l_dian Rockies near:. a wealth of snow-

peaks, glaciers, and The White Cascade, in Tuolumne Riser at Conness Creek Basin .

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YOSEMITE AND ITS HIGH SIERRA

Indian Grist-Mill . An important article of Sierra Indian dietwas meal made by pounding black oak acorns in rude mor- upon what is doubt-tars in the granite . The meal was bleached with hot water less the most fascin -to remove the bitter taste, and baked into hard cake bydropping heated stones into cooking baskets containing the

acing glacial land-paste. Such acorn bread is still made by the Indians . scape in America.

Such a record holds, inevitably, far greater value and concern for usthan the glaciers themselves could ever have had . The gray granite canonswhich the ice-streams dug are as deep as that in the Arizona sand-stones.Though less gorgeously colored, they are quite as wonderful in the carvingof cliff and wall . But they have other interest found nowhere else in equaldegree. Glorious waterfalls, flung banner-like from the sheer canon sides,tell of complex systems of branches . These radiated like a family tree fromthe trunk glaciers . All were bent to denude the Sierra slope of its sedi-mentary rocks, and dissect the underlying granites with hundreds of canons,gorges, and valleys . Somethousands of years ago, theglaciers retreated slowlyback upon the heights of therange . Each of the largertroughs thus abandoned boreproof of its glacial origin.Instead of the even gradesof stream-cut canons, theypresented the form of giantstairways, down which theglaciers had moved majes-tically, to yield at last to thethen tropical heat of thelower valleys . In this de-

beautiful lake-strewnvalleys.

The YosemitePark has no geysers.Its former mightyice-sheets have nowshrunk to a few pyg-my glaciers, shel-tered on the northslopes of the highestpeaks . These aremere shadows of theancient glaciers,which left the storyof their extent andwork clearly written

Snow-Creek Falls, on Tenaya Lake Trail .

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'I'1aree Brothers, an imposing mass of granite which the inclined joint-planes enabled the glaciers to carve into triple gables . Thename was given in 1851. to connneinorate the capture here of the three sons of the Yosemite chief Tenaya . The Indian name, however,was "Kona-po-pai-zes," or Frogs' Heads . Eagle Peak, the highest of these cliffs, rises 3,800 feet above the Merced, which is seenin the foreground .

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`` '- . . .

. .. .^. ^' ."" .~

Al.''""'~"^-~

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29

scent, the ice carved steps in its path, varying in height and breadth with.ts own varying mass and the character and jointing of the rock . Onthese steps hung a multitude of cataracts, and their deeply cupped treads:held hundreds of high-walled lakes.

The passing centuries have greatly relieved the primitive wildness ofthis glacial landscape.Forests as important as:hose of the RainierPark, and perhaps evenmore beautiful in theirsniversal mingling ofsunshine and shade, have_3vered the upland mo--a :nes and soil beds laid

Two North-side Lakes . UpperTwin Lake, above, is at thehead of Eleanor Creek, andforms part of the Lake Elea-nor system. Below is TildenLake, with Tower Peak (11,-704 ft .) in the central dis-tance, and Saurian Crest onthe left.

by the ice . Many of thewaterfalls on the canonstairways have cut through

their ledges, and become even more picturesque as cascades . While scores.ipon scores of the fine glacial lakes still remain—and a larger book than thiswould be required to describe and exhibit the notable lakes of the YosemitePark,—many others have been filled by stream deposit, profitably convert-_ng bare water areas into delightful mountain vales . Such is Nature's art.

Here our debt to the glaciers reaches its climax . For among the filledlake basins made possible by theirmighty sculpturing are the valleys ofYosemite and Hetch Hetchy, the chiefglories of the entire Park . By theheight and grandeur of their walls, the::nequaled majesty of their cataracts, the:arm of their level floors, and the va-riety and interest of their forests andMountain wild flowers, these famous. alleys claim place among the pre-emin-=nt treasures, not only of California, "Apron" and Glacial Tarn on Lakelet, on

the Merced at head of Little Yosemite .

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VOSkMIITE AND ITS HIGH SIERRA

but of all America . They arepart of our great national heri-tage,—part, indeed, of "thosehigher things among our pos-sessions," as Prof . Lyman hassaid, "that cannot be measuredin money, but have an untoldbearing upon the finer sensibili-ties of a nation ."

Let no one, however, whoknows only these renowned val-leys imagine that he has won hisdue share of Yosemite's inspira-tion. His birthright of beautyand grandeur here is somethingfar more worth while . The twogreat valleys are of course mag-nificent, and each day spent inthem, or in climbing their walls,will bring new rewards . But Iam sorry for those who go nofarther ; who cannot spend afew days, at least, back in theupper country of the Merced orTuolumne, among the lakes andshining granite domes of the

highlands . Even though they may climb no peaks, the high mountains willwelcome them to sit at their feet, share their gentler sunshine and broaderoutlook, breathe their diviner airs, learn the joy of the upland trails, andknow that the best of Yosemite lies far from the crowds of Yosemite Val-ley. Happily, this is now to be made easy, even for the "tenderfoot ."

For the Yosemite country is a picture of contrasts and harmonies thatmake a perfect whole . It isnot to be known by its fa-mous valleys only . Theseare but the enchanting fore-ground of our scene, andgain vastly by the dignityand austerity of their highmountain setting . Viewedseparately, the valleys,splendid as they are, do notmake the picture, any more

Cathedral Peak (el . 10 .933 ft .), a prmuitent land-mark on the divide between the âMerced andTuolumne watersheds .

Dome at Head of Tenaya Lake . Note the large treegrowing halfway up the slope.

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r< East from Glacier Point . Below, in the Merced Cation, are vernal and Nevada Falls, withLiberty Cap, a quarter dome, rising a thousand feet above the latter fall . The granite slopes ofLittle Yosemite are seen beyond . Mt. Clark, the "Obelisk," tops the sky-line on the right, andw it . Florence on the extreme left.

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YOSEMITE AND ITS HIGH SIERRA

than Millet's two figures bent in prayer make the "Angelus ." We need toknow the background in order to get the true values of the foreseen . Andonly so, indeed, can the highly sensational features of the valleys them-selves, and their ancient story, be understood . Yosemite Valley and its sistercanon of Hetch Hetchy, with their lesser replicas in different parts of thePark, are all inseparable, geologically, from the High Sierra back of them.

The "Governor Tod" Group, one of the finest in the Mnriposn Grove.

The "dropped-block" theory of their origin has long been abandoned . Theyare linked by the vanished glaciers with the snow-peaks.

Thus our Yosemite picture, both scenically and historically, looks backof necessity from the warmth of its lowland grandeur to the wild sublimityof bleak highlands, till recently the home of perennial frost . Even hereare startling surprises for one who expects no beauty on the ice-sweptheights . The stern sculpturing of pinnacled granite crags that dot the wideplateaus is no more characteristic of the landscape than is their flora . Out-posts of the forests, huddled clumps of lodgepole and white-bark pine, areeverywhere bravely scaling the ridges . Throngs of hardy mountain flowers,most brilliant of Nature's children, crowd all the ravines and lakesides, andseize upon every sheltered nook . The shallowest pretense of soil, weathered

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33

A Study in Clouds and Mountains . View east from the summit of Lambert Dome . Be-ginning on the left, the peaks seen here are Dana, Gibbs and Mammoth . The cloudscenery of the Sierra is as characteristic and impressive as its landscape.

from the somber granites, is sufficient invitation . The short alpine summeris long enough for their modest needs . Boldly they rush the season, edgingaway the tardy snow-banks, and calling on Old Winter to be up and going,Hardly waiting for his departure, at once they set about their business ofhiding the glacial scars with masses of gay color . This ministry of beautybegins at the very snow-line, and grows as flowers and forest march to-gether down to the sunny glacial meadows, and on to the still older valleysof the Sierranmiddle zone, deep with soil, and glowing in the long summer.

Eager as Nature has been to plant the broad Yosemite uplandswith flowers and trees, she has scattered other wonders here with evengreater extravagance. Almost everything is on a scale of surprise . No-where else in America arehighland lakes so plentifulor their settings more su-perb . The giant cataractsof Yosemite Valley dwarf ahundred other great water-falls and cascades in thePark . These are hardlynoticed here, but any one ofthem, could it be removedto Switzerland, would be-come a center of crowded the custom of many early flowers, near the timber line.

Buttercups Following Retreat of the Snow . This is

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YOSEMITE AND ITS HIGH SIERRA

Washburn Lake (7,640 ft . el .(, on the Merced River above Lake Merced . Long Mountain(11 .465 ft.), on the crest of the Sierra, is seen in the distance.

tourist inns . The Park's genial forests of white and red firs, sugar and yel-low pines, incense cedars and mountain hemlocks, spreading up to altitudesof eight and nine thousand feet, thrill every lover of splendid trees . Butthese are overshadowed by its groves of kingly Sequoias, the marvel ofthe botanical world,—immemorial trees that might have heard blind Homer

sing the fall ofTroy, or furnishedthe timbers for Solo-mon's temple.

Colossal t h i slandscape is, but itsfeatures are so wellproportioned that intheir immensity wefeel no exaggerationor distortion . Onlywhen the visitorcompares them withmore familiar ob-jects does he clearlysee that here, truly,is a playgroundNorth Dome . seen from Happy Isles .

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The Tuolumne Grand Cation, eieeved from its north wall, above Muir ( :urge, the top of whieh is seen in the lower right-hand eorner ofthe picture . Colby Mountain, named in honor of the Secretary of the Sierra Club, rises beyond, a mile in height above the river.Grand Mountain is near the center of the sky-line, with Cathedral Creek Canon at its foot, and Falls Ridge between Cathedral Creekand the Tuolumne. 1tuua Crest is seen in the distance on the left .

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YOSEMITE AND ITS HIGH SIERRA

fashioned for giants . The very harmony of its elements makes us slow tograsp the full majesty of the whole . To know Yosemite well is the studyof a lifetime,—labor well repaying the student, as John Muir has found it.We may not quickly learn all its magic, though even the newcomer yieldsto its spell . He comes again and again who would know its mysteries . IfYosemite were of Greece, how inevitably legend, seeking the clue to suchperfection of beauty, must have peopled it with gods !

The Indians of the Sierra, however, were seldom builders of myths.

The Terraced Walls of Retch Hetehy, seen from granite bar in center of the Valley nearits lower end. Kolana Rock on right and North Dome on left rise more than 2,000 feetabove the meadows and forests of the Valley floor,

Stolid and unimaginative beyond most of their brethren, they saw in theirmountains only homes, sustenance and defense . Superstitions and devil-lore they had in plenty . One of their tales, for example, concerned YosemiteValley, their "Ah-wah-nee," meaning a deep grassy vale . Ah-wah-nee, theytold the whites, was the abode of demons, at whose head was the greatTu-tock-ah-nu-lah, the "Rock Chief," which we have translated into cur-rent usage in the Spanish "El Capitan ." His ominous face could be seenin the side of a vast cliff, threatening invaders of his domain . But onesuspects that this naive legend may have been invented for a timely purpose .

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Giant Sequoias at the Cabin in Mariposa Grove.

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YOSEMITE AND ITS HIGH SIERRA

View South from Kuna Crest, showing Mts. Lyell, McClure and Florence on the distantsky-line, with Potter Point and Parsons Peak in center, beyond Lyell Fork Callon.

The Indian tradition of Yosemite is too much attenuated by the years,and adulterated by the fancies of white writers, to permit the acceptance of

many so-called Indian leg-ends of present-day publica-tion . But even these ascribeto the aborigines here nosuch veneration for the greatpeaks, the wonderful cata-racts, and other superlativeforms of nature as amongprimitive men elsewhereclothed them with powerover human lives, oramounted to worship. Nordoes it appear that theirspeculation undertook seri-ously to explain these phe-nomena by a mythology sucheven as grew up in theNorthwest, where the leg-ends of the "Bridge of theGods" and the "Battle ofthe Winds" on the Colum-bia River, the Puget Sound

White Firs (Abies concolor), on the Eagle Peak Trail.This tree, so named because of its light gray bark,is common throughout the Park at 3,000 to 7,000feet, giving place to the Red Fir, which abounds ataltitudes up to 9,000 feet.

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Mt. Dana (13,050 ft .), seen from Tioga Lake, on its northwest slope .

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folk-tale of the "Miser of Tak-homa," and the like show theIndian's restless mind allyingNature with his daily life, andseeking curiously to unravel herproblems . For the YosemiteIndian, the unknown darknessheld only ghosts and witches.His mountains gave him novision . Yet they supplied himwith a place to live in comfortand aboriginal luxury . Theyprovided him with acorns, nuts,game and other food . They en-abled him to hide in pathlesscanons, where pursuit was im-possible, and from the walls ofwhich he might roll down rocksupon any who should attempt topenetrate his mountain fastness.

It is not surprising, there-fore, that our first native tradi-tion of the Yosemite representsthe Red Man as telling whitetrespassers that Tutockahnulah

would surely punish their intrusion into his Ahwahnee . The white tidewas rolling steadily across the plains to the Pacific . A wave had sweptup the coast from Mexico ; all lowland California was inundated. Themountain Indians had no wish to be "civilized " as their valley cousins hadbeen. Hence even asearly as 1833, longbefore the discoveryof gold and the rushof miners to the foot-hills, Captain JosephWalker, the firstwhite man to layeyes upon the Yo-semite country, wascarefully warned byhis Indian guidesaway from the greatvalleys, and made tokeep his course on

Sugar Pine (Pinus lauibertiana), loaded with cones.This tree, king of all the pines, is noted for itstine cones, twelve to twenty inches long.

Crossing Cold Canon Meadows, on trail between Conness Creekand Virginia Callon . This is a typical filled glacial lake.There are hundreds of such broad, shining upland meadowsin the Park, each a park in itself, carpeted with the finestgrass and brilliant with alpine flowers .

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Oh, the mountain music of the Happy Isles!There cool winds are singing,And crystal waters flinging

Their diamond dancing laughter about the Happy Isles.—Harold Synames .

Cascades at the Head of Happy Isles .

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Looking Down into Yosemite from the Western Slope of Clouds Rest . On the right are seen 'Penay-a Canon, North Dome and the topof Washington Column, with El Capitan in the distance ; on the left, Half Dome and the profile of Glacier Point .

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43

:he divide between the Merced and Tuolumne.And when the gold-hunters came, a notable fig-. .re, if California furnished any notables to the:Al of Indian history, arose on behalf of his

rninished tribe to dispute their advance into-~e beloved canon . Tenaya, the Yosemite chief,

the most memorable and picturesque nativereader in the annals of the state.

The actual discovery of this Indian strong-hold is a matter of some debate . Whether it wasWalker, in '33, or Savage's frontier militia of:1, that first looked down into the vast Yosemite_Jrge may never be established . Each expedi-: :on, however, is part of our story.

History has done scant justice to JosephReddeford Walker . He belonged to that smallcoup of intrepid frontiersmen who did much but--rote little, and whose achievements have been_pored through their own neglect of fame and

- :e claims of more ambitious rivals . Walker's_ilure to publish his discoveries, and the fact thate served under a jealous commander, who was

: .en capable of claiming them for his own, have_ Dmbined to obscure his work. That he led a:arty of Bonneville's men in the first exploration

estward from "the Great Salt Lake ;" that he Yosemite Squaw, with Papooseand Baby Basket.: :sproved the then accepted belief that that lake

.rained into the Pacific ; that he established the existence, extent andcharacter of the Great Basin ; that he charted its rivers and lakes ending as

they begin in the desert ; that he discoveredand was the first to cross the Sierra NevadaRange, entering Alta California through theMono Pass and leaving it the next year, 18 34,by the route since known as Walker's Pass ;—here, surely, was a real "pathfinder," worth a

4 clear and permanent page in Western history!Walker concerns us, not only because he

was the first white visitor to the Yosemiteregion, but especially because the claim is nowmade by his family and others that he "dis-covered and camped in Yosemite Valley ."The evidence available hardly seems to sus-taintain this claim in full.(P . eximium), at 12,000

ft ., near Parker Pass . This

On the stone over Walker 's grave in Al-daring blue perennial seeks thehighest slopes .

hambra Cemetery, at Martinez, Cal ., is this

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YOSEMITE AND ITS HIGH SIERRA

line, said to have been placed there on authority of Captain Walker him-self : "Camped at Yosemite, November 13, 1833 ;" and Munro-Fraser's"History of Contra-Costa County," published in 1882, six years after

Walker's death, con-tains a sketch of theexplorer, quoting hisnephew, with whomhe spent his lastyears, and saying:"His were the firstwhite man's eyes thatever looked u p o nthe Yosemite, which

Above, Mono Pass (el.10,599 ft .), looking west,with Mammoth Moun-tain and Iiuna Crest onleft . Below, BloodyCanon and Walker Lake,with Williams Butte andMono Lake beyond.

he then discovered, al-though the honor hasbeen accorded to someother person at aperiod twenty yearslater."

Thus it isseen that the present claim goes somewhat beyond the testimonyand his nephew. We may accept "Camped at Yosemite," but areranted in assuming that "at" means "in"?

On the contrary, Dr . L. H . Bunnell, who

of Walkerwe war-

COPYRIGHT, J . T. BOYSEN

Happy Hours! Deer are a familiar sight everywhere in the up-land forests and meadows of the Park .

was of the Savage partyvisiting the valley in1851, and who namedit "Yosemite," says inhis well-known book,"Discovery of t h eYosemite" (4th ed .,pp. 38 ' 39) :

I cheerfully concedethe fact * * * that "hiswere the first white man'seyes that ever looked up-on the Yosemite" abovethe valley, and in that

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45sense he was certainly-he original white dis-:overer.

The topography ofThe country over whichThe Mono trail ran, andwhich was followed by'apt. Walker, did notadmit of his seeing the-:alley proper . The de--ression indicating the' .-alley, and its magnifi-

ent surroundings, couldalone have been dis-overed, and in Capt.

Walker's conversationswith me at various-:mes he was manlyenough to say so . Up-_n one occasion I told

.'apt . Walker that Ten-ie-ya had said that "asmall party of whitemen once crossed themountains on the northside, but were so guid-ed as not to see the valley proper ." With a smile the captain said : "That was my:,arty, but I was not deceived, for the lay of the land showed there was a valley below;but we had become nearly barefooted, our animals poor, and ourselves on the verge ofstarvation, so we followed down the ridge to Bull Creek, where, killing a deer, wewent into camp ."

Again, on p . 78, Dr. Bunnell says Walker told him that "his Ute andMono guides gave such a dismal account of the canons of both rivers thathe kept his course near to the divide,"—that is, between the Tuolumneand the Merced . With no other chronicle of this first expedition, Bunnell'squotations from Walker and the Yosemite chief enable us to see the weary

explorers struggling up theher'' ;`` steep defile of Bloody Canon

from the volcanic Monoplain, descending the longwestern slope, half starved,and floundering through theuntracked snow of Novem-ber on the divide, to reachat last the sunshine and com-fort of the provincial capi-tal, Monterey. ProbablyWalker's route was muchthe same as that of the laterTioga Road. The Indianshad kept the secret of theirwarm Yosemite home.

We must conclude, Ithink, that while Walker

Sardine Lake, filling a glacial cirquebelow Mono Pass .

in Bloody Cation.

Mt . Hoffman, from Snow Flat, on the Tioga Road . Thismass of granite ramparts is the crest of the dividebetween Yosemite Valley and the Tuolumne.

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YOSEMITE AND ITS HIGH SIERRA

Eastern End of Yosemite Valley, seen from Yosemite Falls Trail, near foot of the - U pperFall. Beginning with Glacier Point on the right, the sky-line shows successively Mt.Starr King, the Mt . Clark group, Half Dome, and North Dome.

first traversed the Yosemite uplands, and was, in that sense, as Bunnelladmits, "the original white discoverer," the honor of first visiting the floorof the valley and making known the majesty of its walls remained for the

"Mariposa Battalion ." Ofthat second expedition wehave a vivid and trust-worthy report . Dr. Bun-nell's account of it, and ofthe Indian war of 1851, ofwhich it was a part, is afrontier classic, with Tena-ya as its hero . In the oldchief's last stand for themountain fortress of hispeople, we see the Indianat his best.

The gold-seekers andgame-hunters of '49 and '5owere pushing the nativesback into the mountains;the Indians were retaliat-ing as usual with robberies,

Distinguished Visitors to the Grizzly Giant . On Presi-dent Roosevelt's right are Gifford Pinchot and Gov.Pardee; on his left, John Muir, Benjamin Ide Wheeler,etc. Out of this visit grew the recession of YosemiteValley and the Mariposa Grove, and their incorpora-tion in the Yosemite National Park .

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.tern end of Yosemite. with Sentinel Hoek and El Capitan, seen from Union Point, 2,334 feetabove the Valley floor .

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YOSEMITE AND ITS HIGH SIERRA

burnings, and occasional murder . To the reser-vation established by the Indian commissionerson the Fresno, near the site of the present townof Madera, some of the hill tribes had comepeaceably . Others were brought in by the militiacompanies of the new state government . Butfar in the heart of the Sierra, the half-breedscouts reported, near the head of the MercedRiver, was a small tribe that refused to leave itsdeep, rocky valley.

"There," they said, "one Indian is morethan ten white men. Hiding places are many,and the Indians will hurl down rocks upon allwho pursue them . Other tribes dare not makewar on them, for they are lawless, like the griz-zly bear, whose name, Yo-Semite, they haveadopted, and as strong . We fear to go to thisvalley. There are many witches there . "

Messengers sent to the Yosemites failed,but at last their chief came alone. AddressingMajor Savage, a veteran frontiersman who com-manded the Battalion, the grave old Indian said:"My people do not want anything from theGreat Father you tell me about . The GreatSpirit is our father, and has supplied us with allwe need. We want nothing from white men.Our women are able to do our work . Go then;

let us remain in the mountains where we were born, and where the ashesof our fathers have been given to the winds . I have said enough!"

Tenaya Peak (10,200 ft.), on the right, with Tenaya Lake in the distance at its foot.

Indians Acorn Cache ("Chuck-ah"), consisting of a largewicker basket set on posts,and thatched with pinebranches, points down, tokeep out squirrels and mice.

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49

Tenaya was sent to bring in his tribe, but only a part came, mostlythe old and the very young . The aged chief, when charged with decep-tion, promised to go on with his people to the soldiers' camp . MajorSavage, he said, might go to the valley with one of his youths as a guide,

but he would find no one there;the younger men frorn Monoand the Tuolumne who hadmarried into the tribe had goneback to the mountains . "iNIytribe is small," he declared,

In Tenayn Canon . The upper viewlooks back to the half Dome ; thelower one shows the gorge blockedby a huge boulder. The steepsouth wall, swept by avalanchesevery spring from the side ofClouds Rest, is seen in each pic-ture . This cation otters great diffi-culties to the climber.

not large as the white chief has said . The Piutes and Monos are all gone.Young and strong men can find plenty in the mountains ; why should theygo to see the white chiefs, to be yarded like horses and cattle? I amwilling to go, for it is best for my people ."

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Lake Tena)a . at the head of Tetucta Creek Canon. The remarkable domes am' polished granite hillsides surrounding this beautifullake vividly recall its n,ontparsltively recent glacial history .

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Gates of Tenaya Canon in Winter—North and Half Domes, Royal Arches, and Washington Column . In beauty of detail, the photo-graph here reproduced is the finest ever made of these commanding cliffs and peaks . Note the overhang of the arehes, the .valer-etched rock, and the snow-laden trees and chaparral . The vast span of the concentric strata may be inferred from their elevation:the upper arch is 1,500 feet above the Valley . North Dome rises 3,530 feet ; Half Dome, 4,850 feet . Clouds Hest, the snowy slope ofwhich is seen beyond, overtops the Valley by almost 6,000 feet .

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YOSEMITE AND ITS IIIGH SIERRA

South Merced Valley, seen from Lookout Point, on the road from Walt ona to Yosemite.

Sending Tenaya and his band on to the camp, upon the South Forkof the Merced, Savage and his men proceeded across the upland throughdeep snow, and on March 21, 1851, descended to the mysterious valley.There they found only an aged squaw . It was as Tenaya had said ; theyoung men and their women had disappeared, and after a brief surveythe disappointed whites recrossed the hills to their camp.

During this first visit to the valley,Dr. Bunnell proposed naming it Yosemite,after its Indian inhabitants ; and the beau-tiful name was adopted, though not with-out the usual opposition from men whosaw in the Indian merely a savage to bedespoiled of his lands . But the Indianname of the valley, as I have said, wasAh-wah-nee . Its ancient tribe had beenalmost exterminated by disease many yearsbefore, and the valley home abandoned,until Tenaya, son of an Ahwahneecheefather by a Mono mother, had led back thefew survivors of the race, re-enforced byrenegade Monos, Piutes from the Tuolum-ne, and fugitives from the lowland tribes.The mongrel clan of several hundred mem-bers proudly adopted a new name given itA Yosemite Wood-Gatherer .

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Mirror Lake, at mouth of Tenaya Canon, with reflection of Mt. Watkins, rising more than4,000 feet above its surface . Perfect reflections such as this are seen only in the earlymorning interval between the downward currents of the night and the warm windsthat draw up the Sierra slope as soon as the sun strikes it.

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YOSEMITE AND ITS HIGH SIERRA

by others, Yosemite,or Grizzly Bear, forthe animal which theIndians most fearedand emulated.

Savage never gothis captives to theFresno reservation.When nearly there,alarmed by runnersfrom the hostileChowchillas on theSouth Fork, andtaking advantage ofthe relaxed vigilanceof their guards, theyfled in the night, andwere not again to betempted away fromtheir valley. In-ducements successfulwith other tribeswere rejected with

contempt . Gaudy clothing and cheap presents Tenaya declared no recom-pense for loss of freedom in their mountain home . Even the offered beefwas refused ; the Indians preferred horse-flesh . Hence, after the Chow-chillas had been subdued, and the other tribes had made treaties, Savage senta second expedition, under Captain Boling, to bring in the stubborn Yo-semites . Bunnell again was of the party, which expected to have littledifficulty in persuading Tenaya to surrender . But on reaching the valleyin May, Boling found only deserted wigwams and smoking ash-heaps tellingofhastyflight . Threeof the chief's sonswere captured at thefoot of the greatrock then named, inmemory of the cap-ture, "Three Broth-ers." One of theseyouths was killed intrying to escape, andshortly afterwardsTenaya himself wascaught by Boling'sIndian scouts on a "Umbrella Tree," a snow-flattened pine at bead of Nevada Fall.

Yosemite Indian Basket-Maker, weaving a burden basket. Thelarge basket to the left is for cooking .

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high bench east ofthe "Big Falls,"whence he had beenwatching his enemiesbelow . When hesaw the body of hisson, his grief foundvent only in a lookof hatred that Bol-ing well understood.No word could becoaxed from him inreply to the cap-tain's regrets for theyouth's death . Aday or two later, hemade an unsuccess-ful attempt to escapeacross the swollenMerced. Then atlast his grief andrage poured out incharacteristic speech.

"Kill me, Cap-tain," he cried, "asyou killed my son;as you would kill mypeople, if they wereto come to you . Youhave made my lifedark . But wait alittle. When I amdead, my spirit willmake trouble foryou and your people . I will follow in your footsteps, and be among therocks and waterfalls, and in the rivers and winds . You will not see me,but you shall fear the spirit of the old chief, and grow cold ."

Tenaya's appeal to the unknown was as futile as eloquence generallyis . The white conquest paid no heed to his threats. Steadily rounding upthe savages, Boling's party captured the last of their band at a rancheriaor village a few miles above the valley, on a beautiful lake walled by pol-ished granite cliffs and domes, which they at once named Lake Tenaya."But it already has a name," Tenaya protested,—" Ty-we-ack,' Lake ofthe Shining Rocks ." The naming of a lake in his honor seemed to him apoor equivalent for the loss of his territory. Another chance was given him.

Wild Flowers beneath the Royal Arches .

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The "Forest Queen," in theMariposa Grove, — an ex-ceptionally straight trunk,without the usual but-tresses at the base .

Taken at last to the Fresno, he soon begged forleave to quit the heat and dust of the reserva-tion ; and on his pledge of their good behavior,he led back his people once more to the coolspaces of the Yosemite . The aged sachem him-self kept faith, but he could not control hisyoung men . The killing of prospectors in thevalley the next summer quickly brought a thirdvisit from the soldiers, and the final dispersionof the Yosemites. It hardly detracts from thepathos of Tenaya's losing fight for his wildhome that he and his last handful of followerswere killed by Mono swhose hospitality theyhad repaid by stealingtheir horses. The Indi-an's code did not recog-nize other people's rightsin livestock.

Present-day visitorsto Yosemite are oftendisappointed that theirfirst impression of t h eheight of the valley wallsfalls short of publishedaccounts. Yosemite mag-nitudes are not quicklyrealized. Even Dr. Bun-nell was ridiculed by Cap-tain Boling and otherswhen he estimated thesuperb granite cliff opposite their camp as atleast fifteen hundred feet high . Some guessedfive hundred, others eight hundred. Not evenBunnell himself dreamed that El Capitan actu-ally towered more than three-fifths of a mileabove the silent Merced.

Its Indian inhabitants gone, Yosemite sooncame into public notice . As early as 1855, thefirst tourist parties visited the valley . Trailswere quickly opened, rude inns established, and,in 1864, John Conness, a senator from California,introduced and Congress passed an act grant-ing to the state "the `cleft' or `gorge' in the gran-ite peak of the Sierra Nevada Mountains . .

,:OVYHiOni, J . T. BOVSEN

"Watch Me!"

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known as the Yosemite Val-ley, with its branches orspurs, in estimated lengthfifteen miles, and in averagewidth one mile back fromthe main edge of the preci-pice, on each side of thevalley, with the stipulation,nevertheless, . . . that thepremises shall be held forpublic use, resort, and rec-reation ." To this grant wasadded the " `Mariposa BigTree Grove, ' not to exceedthe area of four sections ."In 189o, Congress createdthe Yosemite NationalPark, subject to the grant of1864 . Its lines have sincebeen modified considerablyby acts of 1905 and 1906,excluding the head basins ofthe north and middle forksof the San Joaquin, and em-bracing more completely thewatersheds of the Tuolumneand Merced Rivers . Itsarea, as already noted, isnow 1,124 square miles.

The dual administra-tion established by the creation of the National Park surrounding the StatePark was soon found impracticable and disastrous . The state commis-

sioners did the best they could with the tenor fifteen thousand dollars annually votedby the legislature, but these inadequate ap-propriations were largely consumed in thesalaries of park guardians and the travelingexpenses of the commissioners ; little wasleft for needed improvements . Much ofYosemite Valley was fenced in, and let toprivate contractors . Conflicts occurred be-tween the state and federal authorities . Aforest fire, for example, was sometimes leftto burn while the officers debated as to

Blue Jay, in Merced Canon belowVernal Fall.

which jurisdiction was responsible!

,OPYhIUnl, PILUEURY

On the Overhanging Rock at Glacier Point, with eighifeet of snow .

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John Muir was one of the firstand most active in pointing out theimportance of ending this imperiumin imperio . His opportunity camein 1903, when he was invited byPresident Roosevelt to accompanyhim on his visit to Yosemite . Gov-ernor Pardee, President BenjaminIde Wheeler of the State Universi-ty, and other well-known men werein the party, which received Mr.Muir's arguments for the recessionof the valley and Big Tree grovewith unanimous approval.

A vigorous state-wide cam-paign was started by the SierraClub, the strong California societyof mountain-lovers of which Muirwas president. The plan won gen-erous support from the newspapersof the state, as well as from the

Native Sons and other large organizations ; and was eventually successful,though its advocates had to overcome bitter opposition, both at Sacramentoand at Washington, from certain politicians and favored concessionnaireswhose private interests conflicted with the public advantage.

The recession has been justified by its results . Better order has beenestablished, and in every way the rights and convenience of the public havebeen promoted . The federal management, while sometimes open to criti-cism, has devoted annualappropriations exceeding$5o,000, besides an in-creased income from con-cessions, mainly to im-provements that would stillbe lacking under the clumsydual system. Several hun-dred thousand dollars havebeen spent in buildinggood roads and perman-ent bridges, and in leadingtrails into all parts of thePark. No one who viewsthe matter impartially cannow be found to advocate:a return to the old regime.

John Muir in Retch Hetehy. The tree shownhere is a fine example of Yellow Pine.

Ready for the Trails .

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*.'rnaya Canon, from Glacier Point (3,250 feet), with the late Galen Clark at the age of 94 on "Pho-tographer& Rock ." The perpendicular cleavage of the Half Dome by weathering is well shownin this view. Mirror Lake lies below in the canon, and beyond rise Mt . Watkins on the left,Clouds Rest on the right, and Tenaya Peak in the distance at the head of the canon .

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Ball-Dome in the Alpen-Glow.

Now . while a farewell gleam of evening lightIs fondly lingering on thy shattered front,Do thou, in turn, be paramount ; and ruleOver the pomp and beauty of a sceneWhose mountains, torrents, lake and wood uniteTo pay thee homage .

—Wordsworth.

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Diereed River and the Forest in Yosemite, with Half Dome in distance.

IL

THE CANON OF YOSEMITE.

"Of the grandest sights I have enjoyed,—Rome from the dome of St. Peter's, the

Alps from lake Conio, Mont Blanc and its glaciers from Chamouni, Niagara, and

Yosemite .—I judge the last named the most unique and stupendous ."— Horace Greeley.

The only spot I have ever found that came up to the brag ."—Ralph Waldo Emerson.

FARLY visitors to Yosemite paid well for its pleasures . To reach thevalley by any of the old routes meant a hot and dusty ride of two orthree days, in a primitive vehicle, over the roughest of mountain roads.

In common with thousands of others, I painfully recall my first trip . Wequit the train from San Francisco at Raymond, to endure a day of misery ina crowded "stage," which jolted us up from the low country into the noblevalley of the South Fork atWawona . That ride madethe friendly little inn there,when we finally reached it,seem more luxurious thananymetropolitan hotel . Thenext day was spent amongthe Mariposa Big Trees.The third carried us acrossthe broad Wawona ridge toInspiration Point and thehard-won vision of Yosem-ite itself . We were bruisedand happy.

Hundreds of touristsLost Arrow Trail, east side of Yosemite Creek, leading

still come and go by the

to Camp Lost Arrow .

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YOSEMITE AND ITS HIGH SIERRA

Wawona route, leaving or return-ing to the railway at Madera orRaymond . Automobiles, goodroads, and improved hotel servicehave robbed the trip of its terrors.The traveler is able to enjoy fullythe increasing interest of a wonder-ful ride, as his motor climbs swiftlyback among the great, forested hillsof Wawona. It is a country which,even without Yosemite or the Mari-posa Grove, might well draw himto its own splendid outlooks, deepvalleys, and fine waterfalls andlakes,—a sportsman's paradise thatshould form part of any extendedYosemite outing.

The Wawona route, like theBig Oak Flat road north of theMerced, is recommended by the factthat it gives the incoming visitorhis introduction to Yosemite Valleyfrom the heights . Few things in

Chilnunlua Falls, near Wawona ; one of the this world can exceed the surprisemost beautiful series of cataracts and ens- and pleasure of that view . Nearingin the Park .

gthe rim of the plateau, the road sud-

denly leaves the forest for a turn far out on a rocky promontory . Nearlytwo thousand feet below, the river lies, a white thread, at the bottom of itsgorge. The foreground is wild and unformed,—an abyss fringed by pro-jecting crags and pinnacles, and barren save for a few rugged and adven-turous pines clutching the ledges . But eastward opens the famous valley,always more impres-sive than imagina-tion has conceivedit. Its nearest cliffstower as far aboveas the river lies be-low, while, milesbeyond, the greatpicture closes withdomes and peakslightly silhouettedagainst the softestblues and whites ofthe Sierran sky .

"New England Bridge," at Wawona, built by Galen Clark in 1870 .

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Bridal Veil Meadow, on the route of the ancient Pohono Glacier . Such sunny glacialflats, large and small, telling of old lakes long since transformed by stream-wash,are come upon everywhere below timber line, on forest trails or among the uplandgranite domes . Homes of flowers and deer, musical with the song of birds, they areone of the surprises of the Park.

It is a picture one can not afford to miss, and if he comes to Yosemiteby rail, as most visitors now do, he will lose much of its beauty if he fails tosee the valley from Wawona road . I do not wonder that every artist wantsto paint his interpretation of Yo-semite's message from the sublimeoutlooks on or near this road, asit rises out of the canon ; or thatthe scene inspires such admirablework as we have in Mr . Jorgen-sen's Bohemian Club painting.But all nature-lovers will indorseMr. Chase's protest against thecheap, bromidic names given theseview-points . It does not add tothe inspiration of the scene to betold, "This is Inspiration Point !"There is both good humor andgood sense in what Chase says:

Inspiration, in any case, is a timidbird, which appears without advertise-ment, delights not in sign-boards, and On Wawona Road, near Inspiration Point .

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YOSEMITE AND ITS HIGH SIERRA

the louder it is whistled for is the more apt to refuse to come . I have heard thespot spoken of by warm and jocular young gentlemen as Perspiration Point ; andalthough that species of witticism is, generally speaking, distasteful to me, I find thatI suffer no pang when it is practiced at the expense of this piece of pedantry .—Yosemite Trails, p . ~8.

The Merced River, three miles above El Portal . The sharp V-shape of the gorge indicatesthat it was probably eut by stream erosion, rather than by the glacier which carved theU-shaped canon of Yosemite above. Along this wild trough, filled with boulders fromthe cliffs . an excellent automobile road has been built at great cost.

The majority of Yosemite visitors to-day prefer the quicker serviceof the railway, even to automobiles on the roads into the Park which haverecently been opened to those vehicles . Leaving the Southern Pacific orSanta Fe system at the pleasant town of Merced, their through cars fromSan Francisco or Los Angeles carry them over the Yosemite Valley Railroadto El Portal, its terminus, just outside the Park boundary . This road is anoteworthy piece of railway building . A few miles above Merced, it en-ters the Merced River gorge, which it follows for the rest of its seventy-eight miles, as the canon sinks deeper into the range . For most of thislength it was blasted out of the granite or cleated upon the wall of thegorge. Below it the Merced winds in a narrow, tortuous channel, whichis dammed here and there to supply power for quartz and lumber mills.Gold mining is in progress at many points .

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At El Portal, the rail-way maintains an excellenthotel . From here automo-bile stages run not only toYosemite, but also to theMerced and Tuolumne BigTree Groves . These smallareas contain many finetrees, and the journey tothem is one of great interest.The road, as it climbs thehills, unfolds magnificentviews of Yosemite and thelower Merced valley. Evenif there were no Giant Se-quoias in prospect, the ridewould be well worth while,for the forests of fir, pineand cedar through which itpasses are among the mostinteresting in the state.

A ride of twelve milesover a good automobileroad of easy grades bringsthe visitor to Yosemite Vil-lage, at the center of Yosem-ite Valley . This highwayis one of the most pictur-esque mountain roads inAmerica. From El Portalto the very gates of the val-ley, it had to be cut out ofthe granite hillsides . Allabout it is a scene of colossaldisorder, the work of ava-lanche and earthquake, fill-ing the canon with mightyboulders from the cliffsabove, over which the river foams in continuous cascades . One greatwaterfall is passed before we reach Yosemite, though among the multitudeof cataracts hereabout it is so inconspicuous that the automobile driver mayrush by it without calling his passengers' attention to its beauty . This isCascade Falls, seen on the left, where Cascade Creek pours from the northwall of the canon, five hundred feet, in a deep recess close to the road.So fine a sight should not be overlooked . It prepares one for the

Cascade Falls, four miles west of El Capitan .

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Bridal Veil Fall, seen in early Winter from thesouth-side road.

that he may well deem it thefamous waterfalls.

Here, too, at the very gates of the valley, we find an invaluable keyto the problem of its origin . As we followed up the Merced, we have thusfar seen it everywhere a turbulentcanon stream . But at the baseof Cathedral Rocks its characterchanges. For seven miles abovethat point, it is the most peacefulof meadow-bordered rivers, withonly a few feet of fall as it me-anders indolently down the levelvalley floor from Happy Isles. Alittle easy investigation, for want ofwhich, however, some eminent sci-entists have gone far astray, ex-plains the change.

At the place just mentioned,where El Capitan bridge formerly

greater magnificence of Bridal VeilFall ahead.

Soon, quitting the narrow, clut-tered wildness of the lower river,the newcomer is face to face withthe ordered peace and glory of Yo-semite itself . Gratefully, silently, hebreathes the very magic of the En-chanted Valley. For here, fullyspread before him, is that combina-tion of sylvan charm with stupen-dous natural phenomena whichmakes Yosemite unique amongEarth's great pictures . He sees thecanon's level floor, telling of an an-cient glacial lake that has givenplace to wide, grassy meadows;fields of glad mountain flowers;forests of many greens and laven-ders ; the fascination of the wind-ing Merced, River of Mercy ; and,gleaming high above this world ofgentle loveliness, the amazing grayface of El Capitan, while Pohonodrops from a "hanging valley" su-perbly sculptured, and so beautiful

noblest setting Nature has given to any of her

Winter Sports in -Y osemite . Skiing andsnow-shoeing draw many parties to thegalley each winter .

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El Capitan and Three Brothers, seen from the moraine at the foot of Cathedral Rocks.Tourists of the class that finds its chief out-door interest in discovering zoological re-semblances in natural objects have dubbed El Capitan "the Crouching Lion of Yosem-ite." This is a misnomer, as the splendid huge rock is obviously an elephant:

stood, and where its piers may yet be seen, a broad ridge of glacial debris,now covered with young forest, and notched by the river channel, stretchesfrom the talus slope below Cathedral Rocks a quarter of a mile across tothe rock slide, or earthquake talus, west of El Capitan . It is largely buriedin silt and river gravel, but about twenty feet of its height is visible on theupper side, and twice as much below . So solid and level an embankment ofsoil and boulders,some of which havebeen freighteddown from the sea-beach strata still re-maining back onthe highest peaks,is unmistakably aglacier's record.Had Prof. J. D.Whitney seen itwhen, as state geol-ogist, he conductedhis famous Yosem-ite survey, fiftyyears ago, he would

A Glimpse of North Dome . from one of the beautiful forest roadsin Yosemite Valley .

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Yosemite Village .

Merced River.

Royal Arches .

Tenaya Canon.North Wall of the Valley, seen from the talus back of Yosemite Village . The trail to the top of Yosemite Falls and Yosemite Point

climbs out of the Valley over the wooded earthquake talus seen in this view below Eagle Peak, follows the second bench eastwardto the foot of the upper fall, and then, by many zigzags, ascends the small glacial canon west of that cataract.

Tenaya Canon .

Half Dome. Mt . Broderick. Liberty Cap. Vernal and Nevada Falls .

Mt . Starr King.

Panoramic View East from Washburn Point, above Glacier Point.

El Capitan . Eagle Peak_ Yosemite Falls . Yosemite Point .

Indian Callon. North Dome . Half Dome.

Mt . Watkins.

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Ca hedral Roeks and Spires, from the Mereed River near Rocky Point.

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not have made theblunder of his lifeby denying that thevalley was due toglacial action, orsaid : "There are be-low the valley noremains of the mo-raines which such anoperation could notfail to have formed ."For in fact this ridgeis simply a terminalmoraine, depositedby the great valleyglacier at the pointwhere the last of itsrepeated advancesstopped, and fromwhich its final slowretreat began.

The line of themoraine, geologiststell us, practicallycoincides with, andcovers, a granite bar,or sill, which formedthe dam of the an-cient Yosemite Lake.This body of water

had the same history as hundreds of other canon lakes still to be foundin the High Sierra, occupying the depressed treads of the huge glacial stair-ways. Deep basins were quarried by the glaciers wherever inflowingbranch glaciers greatly augmented their mass and weight, with a correspond-ing increase in digging power . Glaciers alone produce these rock-basins.Lakes such as Merced and Tenaya, above Yosemite Valley, and filledlake-beds such as Yosemite and Hecch Hetchy Valleys, are found only inthe tracks of the vanished ice-streams . River erosion never cuts suchhollowed steps in water-channels . It requires the long scouring of incal-culable moving ice-masses, armed with vast rocks plucked from their beds,to prepare the canons for the lakes and level valleys of the later time.

Thus the sudden change in the Merced River, from a quiet meadowstream to a brawling mountain torrent, recalls vividly to the modernstudent that distant day when the receding glacier left behind it a beauti-ful lake, seven miles in length and probably four or five hundred feet deep.

The "Back Road," on the south side of Yosemite. The treesshown are chiefly California Black Oaks (Quercus kelloggii),a deciduous species that does much to beautify Yosemite andRetch Hetchy . Its acorns supply bread to the Indians, andare prized by squirrels and woodpeckers .

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losemite Falls, seen front trail through the beautiful oak and pine forest that skirts the northwall of the Valley . The upper fall, beginning 2,365 feet above the Valley floor, drops 1,430feet ; the lower fall, 320 feet, with several smaller falls between. Yosemite Point, 2,9755feet, is on the right, and the tall granite spire in front of it is the "Lost Arrow" of Indianlegend.

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walled by perpendicular cliffs rising morethan three thousand feet, and dammed bya rocky moraine overlying a granite dike.Where the lake ended, the Merced cut apass for itself through the moraine . Thisis also used by the road to-day . The lakeitself, probably within the last two orthree hundred years, if we may judge bythe trees growing where once was onlywater, has filled up with rich alluvial soil,brought down mainly by spring freshetsfrom near-by heights, rather than by thelarger river, and giving us the fertile val-ley floor, with an inestimable part of thebeauty of Yosemite.

That Yosemite Valley is due mainlyto glacial action, which deepened andwidened a river gorge existing before theglacial epoch or epochs, is now generallyaccepted by the geologists : they differ onlyas to the length of the main Yosemite gla-cier, some believingthat it extended lit-tle below El Capi-tan, while others find

reached the foothills.Government geologists are now making a minute ex-amination of the region, and the publication of theirwork will throw light on many such minor problems.But the main question is no longer disputed.

Such agreement, however, is of comparativelyrecent date. There have been many theories as to themaking of the great canon . The most interesting ofthese, because of the eminence of its author, and theviolence with which he mistakenly denounced the gla-cial hypothesis, was the famous fault-block contentionof Prof. Whitney. Said he:

A more absurd theory was never advanced than that bywhich it was sought to ascribe to glaciers the sawing out ofthese vertical walls and the rounding of the domes . Nothingmore unlike the real work of ice, as exhibited in the Alps,could be found . Besides, there is no reason to suppose, or atleast no proof, that glaciers have ever occupied the valley, orany portion of it, so that this theory, based on entire ignoranceof the whole subject, may be dropped without wasting anymore time on it . . . . We conceive that, during the upheavalof the Sierra, or, possibly, at some time after that had takenplace, there was at the Yosemite a subsidence of a limited

Cliff at Head of Yosemite Falls,showing the vertical cleavagejoints which have guided the gla-cial sculpturing and made possiblethe sheer walls of A osemite, HetchHetchy and similar cations.

evidence that convinces them it

Leopard Lily (L . par-dalinum), a gorgeousorange - and - purplemember of the Lilyfamily, which fre-quents the lowervalleys of the Park.-

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Evening Primroses and the Half Dome . These beautiful luminous yellow flowers are a familiardecoration of Yosemite, Heteh Hetehy and other valleys in the Park during July, when theirbuds "pop" open noisily at sunset for a single night of fragrant revelry .

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area, marked by lines of "fault" orfissures crossing each other some-what nearly at right angles. Inother and more simple language,the bottom of the valley sankdown to an unknown depth, owingto its support being withdrawnfrom underneath . —The YosemiteGuide Book, 73, 74.

Had Whitney's examin-ation of the valley beenthorough enough to take noteof the old moraine belowEl Capitan, it is probable hewould not have written thosewords. And yet he had otherevidence that should haveprevented his error. El Cap-itan Moraine and the old Yo-semite Lake which it helps us

lee Cone at the Foot of Upper Yo-semite Fall . This volcano-likehill rises each winter to a heightof four or five hundred feet,formed by the freezing spray andby blocks of ice fallen from theface of the cliff . The mouth ofthe cone is about 200 feet indiameter, says Muir, who haslooked down into it from theledge seen ou the right in theupper picture. The two smallspecks on the side of the conein the lower view are the lateGalen Clark and a companion,who climbed it to get a look intothe "crater ."

to reconstruct are far from be-ing the only reminders of thevalley's glacial history. Moststriking of all, the hangingvalleys on its walls are noless clearly of glacial origin .

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cerhanging Rock at Glacier Point, the most famous and important viewpoint on the rim of Yo-semite. From it the spectator looks down 3,230 feet sheer to the Merced, winding among theforests and meadows of the valley floor, and across to the beautiful Yosemite Fall, droppinghalf a mile out of its own hanging valley.

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As we pass Bridal VeilFall, we note that it drops,not from a flat plateauabove, nor from a narrowcleft in the wall, but out ofa high side-valley, which inturn is framed by lofty cliffs.The U-shape of this broadvalley is so clear that we atonce perceive that it, too,must have been scoured outby a glacier, rather than byPohono Creek, which couldhave cut only a V-shapedgorge. Its sculptor, in fact,was a minor glacier, mightyenough to dig a splendidwild valley, more than fif-teen hundred feet deep, butnot powerful enough to sinkit to the bed of the mainvalley . Hence, as the larger

Glacier Point . jutting into Yosem-ite Valley at its junction withthe Merced-Illilouette Cafion.Seen either from the Valleyfloor or from the trail to VernalFall, this massive cliff is thestateliest headland of the southwall . Its precipitous faces aredue to glacial quarrying alongvertical joint-planes.

glacier shrank in bulk, andceased to fill the great canonof Yosemite, the Pohonoglacier was left "hanging"on the side; to drop its ice androck in avalanches upon thetrunk glacier below . Final-ly, both glaciers vanished,

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Vernal Fall.

1- springs are in the cloud, thy stream=egins to move and murmur first

r ._ ere ice-peaks feel the noonday beam,=r rain-storms on the glacier burst,

—Bryant.

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111ilouette Fall, viewed from its canon below. This fine waterfall has a drop of 370 feet.It is a hard climb up Illilouette Canon from the Merced River to the foot of the fall,which may be seen more easily from above, on the Long Trail to Glacier Point .

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79

with increasing mean temperature and decreasing snowfall . Of theircanons one was occupied by the typical glacier-made lake of Yosemite,nearly four thousand feet above sea ; while the other, for want of icebergsto drop into the .Iake, just as plainly declared its origin by flinging out a,lacial banner, the most graceful and musical, though far from the largest,

of the Yosemite waterfalls.Other famous cata-

racts hung high on the val-ley walls repeat the storyof Bridal Veil. YosemiteFalls, at the center of thenorth wall, and Illilouette,on the south wall at thehead of the valley, are themost important in volumeand length of season, tell-ing by their well-definedhanging valleys and fan-,

amphitheaters, set deepin the highlands, that they,

The Merced at Happy Isles—two beautifully woodedislets at the upper end ofthe Valley, where theriver rushes out of itsnarrow canon below Iliil-ouette and Vernal Falls.

too, are glacier-born.No more enjoyable oc-cupation can be foundfor part of a Yosemitevacation than to trace their old glaciers to their sources in the Hoffman andMerced spurs of the main Sierra.

If one follows up Yosemite Creek, above its falls, and beyond the oldTioga Road, he discovers a fine cluster of glacial cirques, stretching aroundfrom the north side of Mt. Hoffman, along the southern slope of theMerced-Tuolumne divide, and forming a mountain-walled basin, almost

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YOSEMITE AND ITS HIGH SIERRA

circular, and five orsix miles in diam-eter. In outline itis like the spreadingcrown of one of thecanon live-oaks thatbeautify the uplandroads and trails.This characteristicabandoned home ofa minor glacier nolonger holds its per-manent neve. It isto-day merely a tem-porary reservoir.There the annualsnows are held untilit pleases their par-ent, the Sun, totransform them

again into summer floods, and send them, singing, down the valley to jointhe Yosemite chorus . Yosemite Creek now flows to its fall amidst a wildpanorama of gray, barren domes and fir-covered moraines . But here forcenturies a shallow glacier, fifteen miles in length and several miles wide,crept slowly from the Mt . Hoffman Range to meet the great ice-streamof the Merced ; and when the larger glacier sank low in its vast canon, thenorth-side feeder dug back its section of the wall until it had quarried adeep branch canon, in which Yosemite Upper Fall now thunders its own

The "Fallen Monarch," with troop of cavalry. This great Sequoia, standing, was one of thelargest in the Mariposa Grove.

Le Conte Memorial, at the foot of Glacier Point ; erected by theSierra Club in honor of the late Prof . Joseph Le Conte, thefamous geologist and author, of the University of California,and maintained as the Club's Yosemite headquarters . Herea library of out-door literature is accessible to the public .

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vernal Fall, from Clark's Point, on the horse trail . This famous cataract is eighty feet wide, andhas a drop of 317 feet . Although the most conventional of the great falls in Yosemite, Vernaloffers a magnificent picture, both in its setting and in its wealth of color . The golden greens andblues of the steadily falling stream, its shooting "comets," clouds of spray, and circular rain-bows . make it an ideal study, well worth many visits .

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YOSEMITE AND ITS HIGH SIERRA

chapter of the glacial story, king of all thewaterfalls in height and stateliness.

How easily the Yosemite cliffs wereundercut and torn away by the blows ofavalanches from the glacier above may beguessed from the picture on page 72, show-ing the wall so deeply fissured by verticaland intersecting cleavage planes that it ismerely a standing pile of huge rectangulargranite blocks, ready to be tumbled overby any power that can.

The Illilouette watershed is larger,and even more interesting, as rimmed byhigher mountains . From the "Long Trail"approaching Glacier Point, we get a good

jview of its deep lower valley, encirclingMt. Starr King, and inviting us back to itsfountain basins sunk in the west flank ofthe Merced Range. There Mt . Clark, andGray, Red and Merced Peaks, accent asnoble a ring of cirques as we shall findbelow the very crest of the Sierra . Thiswatershed, once occupied by a broad riverof ice, is now a land of sunny meadows,shining domes, and densely forested con-

verging moraines, the whole walled by snowy mountains that rise to eleva-tions of eleven thousand feet . Some idea of it may be had from theillustration on page 22. But its wonderand beauty are beyond the power of pho-tography. The best general view is to behad from Mt . Clark or the east slope ofMt. Starr King, whence one carries awaya lasting picture of what a glacier can doas a landscape architect.

Differing from these three importantcataracts in their manner of birth, butnone the less proclaiming a glacial origin,Vernal and Nevada Falls, at the head ofthe valley, are the largest in volume of allthe Yosemite group . Instead of fallingfrom their own hanging valleys, backedby independent basins, they are part of theMerced itself, and drop from giant stepsin the river's glacial stairway . Thesesteps, like the outstanding sheer cliffs of

Vernal Fall in Winter, when theMerced's fountains in the HighSierra are frozen, and curious lee-forms are built by the spray at thefoot of the shrunken fall.

At the Head of Nevada Fall . Here aprojecting ledge, guarded by aniron rail, enables visitors to studythe wild Rood at close range .

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83

Yosemite, owe their remark-able height and perpendic-ular faces to the alternationof practically solid graniteridges, lying across the pathof the ancient Merced gla-cier, with areas of looserrock, vertically jointed, andtherefore readily disinte-grated by the ice.

Glacial canon steps ashigh as these are exceeding-ly rare . Hence canon water-falls of the height of Vernaland Nevada are elsewherealmost unknown, while cliffcataracts of even greaterfall, dropping from hang-ing valleys on the sides oftrunk-glacier canons, are afamiliar feature of everyimportant alpine district.But the two renowned fallsof the Merced stand quitealone among canon cata-racts in their union of largevolume with great altitude,Vernal falling 317 feet, andNevada 594 feet . Not only are they thus exceptional in magnitude, but theglacier used the local rock formations to make them different . Each hasits own special character . Vernal meets all the requirements of an idealcataract,—a solid sheet of clear water bending easily from the brink of a

Little Yosemite, with its bare granite slopes, seen from summit of Liberty Cap, with HalfDome on the left . Here, too, a Jeffrey Pine, more symmetrical than that on SentinelDome, has established itself. Mt. Clark is is distance (left).

The "Cataract of Diamonds," between vernal andNevada Falls .

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YOSEMIT'1 AND ITS HIGH SIERRA

broad, level graniteplatform, and offeringall the colors of its owndelightful rainbows, asthe flood changes swift-ly from golden greenat its brow to brokengrays and flashingsnows in the sunnycanon below. Nevadapresents a strikingcontrast to such con-ventional, if surpass-ing, beauty. Alreadychurned to foam in a

Nevada Fall (384 ft.), seenfrom. the (anon below andfrom Zig-Zrag Trail, half-way to the top . In dis-play of power, this greatfall ranks first among theTosemite cataracts.

steep, crooked trough,it shoots far out fromits narrow cleft, a pas-sionate cloud, seeming-ly made up of millionsof distinct, pearl-likedrops ; and midway inits descent it strikes thesloping cliff, spreadinginto a wide "apron" of

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THE CANON OF YOSEMITE

85

Little Yosemite, with Clouds Rest in the distance.

still more dazzling whiteness . So splendid are the children of the glaciers.The record of these waterfalls is corroborated by the rock-basins which

the glacier scoured out ontheir plateaus, just as it hol-lowed the basin of YosemiteLake itself . Emerald Pool,the little tarn immediatelyabove Vernal Fall, is hardlya stone's throw across, butunmistakable . River erosioncould never have fashionedso perfect a bowl . A milehigher up, beyond NevadaFall, the basin was threemiles long, holding a lakethat has now given place tothe charming vale of LittleYosemite . Here bare cliffsand domes frame anotherlevel valley of meadow, for-est and lazy river, all onabout one-half the scale ofthe greater Yosemite below.Other yosemites lie beyond,until we reach the splendidglacial lakes, Merced and Sugar-Loaf Dome, a he head of Little Yosemite.

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YOSEMITE AND ITS HIGH SIERRA

Washburn, far up the canon . These, too, in time will fill with detritus fromthe hills, and become delightful valleys . Nature abhors barren waters.

Glacial history isalso written plain on thetwo "domes" that risejust north of NevadaFall, called the Cap ofLiberty and Mt . Brod-erick. These are simplymasses of unfissuredgranite, too large andsolid for the glacier toplane away, though itgouged out the vast bedsof jointed rock in which

Climbing the Half Dome . Thisfeat was first performed in1S75 by George Andersonwho drilled holes and seteye-bolts in the northeastslope, the only practicableroute . The ascent is nowmade by occasional adven-turers, aided by Anderson'sspikes and a rope. Thelower view here shows aclimber making his way upacross the projecting lay-ers of granite.

they lay ; and as it sweptover them, it shaved

down their east slopes so that one may easily scale them, and find glacierboulders on their tops that have traveled far .

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THE CANON OF YOSEMITE

87

As Merced Canon forms thesoutheast branch of Yosemite Val-ley, so the still deeper canon ofTenava Creek is its northeasternarm. Here the glacial story is lessplain, and on first sight, from theheights on either side, it might beoverlooked . For above the canon'slower two miles,—that is, beyondthe foot of Mt . Watkins,—it crowdsto a narrow box-canon between thatgreat cliff and the steep incline ofClouds Rest . This might seem tobe a V-shaped, stream-cut gorge,rather than to have the broaderbottom commonly left by a glacier.But a little exploration discoversglacial footprints in the terminalmoraines and the lakes and filledlake-beds, with fine connectingwaterfalls, that mark a glacier'sdescent from the Cathedral PeakRange, south of the Tuolumne . Wehave hardly entered the canon, in-deed, before we are reminded ofEl Capitan moraine and the enclosed Yosemite Lake . A similar boulderridge, thrown across the canon here, is traversed by the road as it carries

visitors on their early morning trips tosee the sunrise reflections in MirrorLake. This lakelet evidently occupiesthe lowermost of the glacial steps . Itis a mere reminder of its former size,the delta of Tenaya Creek having stolena mile from its upper end . Fartherup the canon, below and above Mt.Watkins, stream sediment has alreadyturned similar lakes into meadows . Buteight miles east of Yosemite, at thehead of the canon, Tenaya Lake notonly presents one of the most fascinat-ing views in the whole Park, but alsorecalls, in its polished granite pave-ments, walls and domes, a very differ-ent scene,—a picture of the old Tuol-umne glacier, split against the east front

Overhang at Summit of the Half Dome, nearlya mile above the Valley floor and TenayaCanton . El Capitan is seen in the distance.

Phlox (P . douglasii), on the GlacierPoint Trail .

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YOSEMITE AND ITS HIGH SIERRA

Half Yâ ome at Sunrise, seen from Glacier Point.

of Mt. Hoffman, and sending part of its immense ice-stream over the lowdivide into Tenaya basin, to form the main ice supply of Tenaya glacier,and the rest down Tuolumne Canon to Hetch Hetchy.

Thus Tenaya Canon forms no exception . Its narrowness betweenClouds Rest and Mt . Watkins, well shown in Prof . Le Conte's pictures on

page 49, is seen to be due to thesolidity of the huge inclined strataof the former, and the fact that thelatter is a single block of massivegranite, rising as high, as sheer andas unbroken as El Capitan, whichit greatly resembles . The strikingcontrast which Tenaya Canon thuspresents to Yosemite Valley islucidly set forth by Mr. Matthes,the well-known expert of the Geo-logical Survey :

The Yosemite Valley evidently wascarved from prevailingly fissured materialsin which the ice was able to quarry togreat depth and width . Tenaya Canon,on the other hand, was laid along a rathernarrow zone of fissuring, flanked byclose-set, solid masses ; and the glacierthat flowed through it, while permittedto carve deeply—more deeply even thanthe mightier Yosemite glacier,—was im-peded in its lateral excavating, and has

on the "Short Trail , to Glacier Point . This

been able to produce only a narrow,

trail commands splendid views of Sentinel

gorge-like trough . — Sketch of YosemiteRock, Yosemite Falls and the Valley floor . National Park.

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Lake Merced, one of the finest mountain-walled glacial lakes of the Sierra, in the upper Merced Cation, four miles above Little Yosemite .

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YOSEMITE AND ITS HIGH SIERRA

Yosemite offersmany other convinc-ing particulars of thelife of its great val-ley glacier . Thebeauty of its cliffsis no more obviousthan is their testi-mony regardingtheir origin, outlineand sculpturing.Their perpendicularfronts and project-ing angles, narrow-ing the valley here,or overtowering itsdeeper recesses there,tell unmistakably ofthe glacier's work asa giant sapper andminer . But thatwork was made pos-sible by the extrememingling of zonesof jointed and un-jointed granites . Itwas carried on firstby the ice, and later

by all the agencies of weathering,—water, frost and snow . Where thevalley contracts, we find unfissured masses that resisted the stresses of thecooling earth, and inthe glacial age wereable equally to with-stand the action ofice . Here El Capi-tan and CathedralRocks, rising oppo-site each other atthe valley's narrow-est part, were undi-vided blocks too vastfor the glacier to re-move. So YosemiteP O l n t c O n f r on t s Sentinel Dome, on the plateau above S osemite Valley, south of

Sentinel Rock. On the summit is seen the lone Jeffrey PineUnion Point, and

which is shown at large on the opposite page.

A Characteristic Dome Landscape ; view north from GlacierPoint, looking across Yosemite Valley to North Dome, BasketDome, and Mt. Hoffman . In the foreground, note the deepfissure separating Washington Column from the Royal Arches .

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Jeffrey Pine on Sentinel Dome. Such outposts of the forest are found on nearly all the bare granite bosses that stud the Yosemiteuplands . Starting life where no life would seem possible, they bore down into the cleavage joints, and draw moisture from therock itself. Above, they grow slowly, turning their few stocky limbs eastward with the prevailing winds . The heroic tree shownhere is doubtless several hundred years old, though hardly more than twenty feet high .

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YOSEMITE AND ITS HIGH SIERRA

--` : may: E

the splendid prowitrR of Glacier Point the

projecting pedestalof the Half Dome.In the areas of abun-dantly fissured rockseparating each ofthese pairs of oppos-ing cliffs from thenext, the glacier tookadvantage of thevertical and hori-zontal jointing to un-dermine and cutbackthe valley walls.Their varying cleav-age planes, with theoccurrence of small-er unjointed masses,were set out in aninfinite variety ofgables, pinnacles andspires . Where thejointing was vertical,the ice left the sheerfaces of Glacier andYosemite Points andthe Sentinel . Whereit inclined, the Three

Brothers, with their sloping steps, resulted . A succession of fissured andmassive granites gave us the deeply trenched Cathedral Rocks . Purelylocal solidity surrounded by a fissile structure is represented in CathedralSpires and the Lost Arrow, as well as in such clefts as The Fissures andthe gap separating Washington Column from the Royal Arches. Muchof this detailed sculpture, of course, has been the result of weatheringsince the retreat of the glacier . To that agency must also be ascribed thesplitting off of flat plates from the front of Half Dome, as well as the ex-foliation of concentric layers from the top of that and other domes, which,rather than any glacial grinding, is responsible for their rounded form.

Half Dome, the Indian Tis-sa-ack, dominates the upper end of the valleyeven more finely than El Capitan, Tu-tock-ah-nu-lah, commands the lower.These superb cliffs, perhaps the noblest rocks in the world, withstood the iceas they now endure the storms . Serene and distinguished, they express Yo-semite's majesty . "The Colorado Grand Canon," writes John Burroughs,"is more unearthly, apochryphal ; but one could live with Yosemite ."

Aspen Forest at Lake Merced . The finest grove of Aspens inCalifornia . The large trunk at the right shows scratchesfrom the claws of mountain lions, AYhich delight in climbingthese trees. The Aspen (Populus tremuloides) is the mostwidely distributed of American trees, ranging from the ArcticCircle to _Mexico ; and with the Black Willow (Salii nigra)it monopolizes the distinction of being common to both theAtlantic and the Pacific Coast .

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Triple Divide Peak (11,613 ft .), seen from meadows at the foot of Foerster Peak. So calledbecause its snow-fields feed the San Joaquin and two forks of Merced River.

ON THE CALIFORNIA SKY-LINE

I ramble to the summit of Mt . Hoffman, eleven thousand feet high, the highestpoint in life's journey my feet have yet touched . And what glorious landscapes areabout me, new plants, new animals, new crystals, and multitudes of new mountains,far higher than Hoffman, towering in glorious array along the axis of the range, serene,majestic, snow-laden, sun-drenched, vast domes and ridges shining below them, forests,lakes, and meadows in the hollows, the pure blue bell-flower sky brooding them all,—a glory day of admission into a new realm of wonders as if Nature had wooinglywhispered, "Come higher ."—John Muir : "My First Summer in the Sierra ."

THE best way to see Yosemite is from the heights . The wonder andpleasure of this experience draws thousands of visitors each summer toYosemite Point, overlooking Yosem-

ite Falls, and thence to the still higherelevations of El Capitan, Three Brothers(Eagle Peak) and the North Dome ; or, onthe south side, to Glacier Point, SentinelDome and the great outlooks offered by theLong trail and Pohono trail . These com-paratively easy ascents should be made onfoot by everybody who commands goodwind and a fair pair of legs. Others areadvised to take horses . It is not well tounderestimate either the labor required orthe rewards to be obtained . As one risesfrom the valley, the view develops unex-pected surprises ; the opposite cliffs rise Climbing Mt. Clark .

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YOSEMITE AND ITS HIGH SIERRA

with him ; new rock forms are discovered, colossal and unique ; near-byproportions and distant perspective alike change with increasing altitude;until, at last, from the summits he beholds at his feet a vaster andmore beautiful Yo-semite than he hasever dreamed of.

These uplandtrails are the keys

-0604that unlock, not onlythe secrets of Yo-

--

ke ,semite Valley, with

-tea- .

its cliff sculptures,waterfalls and gla-

cial story, but also the greater mysteries of the higher mountains . No onecan climb the valley walls, under the clear Sierran sky, and behold thepanorama which they unfold of the far-away California sky-line, withouthearing the call of those snowy peaks and sunny ranges rising in the east.Splendid views of the High Sierra may be had from Glacier Point or NorthDome, and still granderones from Clouds Rest, eastof Half Dome and easilyreached by trail from Ne-vada Fall,—the highestpoint on the rim of the val-ley. But distant views area poor substitute for thereal enjoyment of days andnights spent amongthe loftypasses and fascinating alpinemeadows nearer the back-bone of the range, with suchascents as may be within

Tuolumne Pass,—upperview looking south;lower view, north . Be-low is seen a snow-field on the slope ofMt . Vogelsang, withadvance of Sierra Clubpack-train coming in-to view. Beyond areRafferty Creek Cationand Rafferty and John-son Peaks.

On Lake Washburn at Sunset .

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Vogelsang Pass (left) and Vogelsang Peak (1 .1,511 ft.) . In the foreground is Vogelsang Lake (frozen), and on the right Fletcher CreekCanon . This Kew looks south from Tuolumne Pass .

(A..

View South from Vogelsang Pass, looking down the Me(lure Fork of the Merced to Mt . (lark and the Merced Range .

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YOSEMITE AND ITS HIGH SIERRA

one's time and inclination.Hence the most importantthing about the trails out ofthe valley is that they in-vite one on and on, to thegrander Yosemite of the farheights.

Visiting the YosemiteSierra has till recentlymeantreal exploration, but withthe good trails now openedto many parts of the Park,one can hardly go anywherebelow timber line without

Summer Snow-fields in t6reSierra . Upperpicture showsparty enteringPark via Don-ohue Pass andeast shoulderof Lyell . Mid-dle, a viewsouth, near

finding sign-boards pointinghim to lake or peak or val-ley . All this is in disregardof the professional climber'sfear that his favorite wildswill be rushed by the "mob."The Park administrationwisely aims to make thisgreat national playgroundfully accessible to the gen-eral public, as well as to themountain enthusiast . The"mob," of course, will notfollow ; but mountain par-

Foerster Pass,across frozenLake Harriet.Lower, coast-ing on snowslope nearFoerster Pass.with MercedCation and Mt.Clark in dis-tance beyond .

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Cathedral Peak (10,933 ft .), from unnamed lake at its foot, on the northwest side, at summit of Cathedral Pass.

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YOSEMITE AND ITS HIGH SIERRA

Looking up Lyell Fork of the Tuolumne, with Kuna Crest on the extreme left, PotterPoint in the center, and Parsons Peak at the end of the ridge beyond.

ties become larger and more numerous every year, and with the establish-ment of the Sierra Club's lodge and camp at Soda Springs next summer,and the chalets which the government is about to erect at Lake Merced,Tuolumne Meadows and some of the intervening passes, the number of suchcompanies taking the long trails will, happily, soon be multiplied.

There is variety enough in the moun-tain trails and the districts to which theylead to fill many summers with enjoyment.No season would be long enough to coverall the trails at anything less than a sprint-er's gait . Hence it is best to undertakesome definite section of the Park, knowingthat unforeseen calls are likely to be madeon one's interest and time.

Except the old Tioga road, all high-ways entering the Park lead to YosemiteVillage, and end there ; travel to the up-lands, save for persons relying upon theirknapsacks, must be by the horse-trails . TheTioga road is not really an exception . Builtmany years ago on easy grades to reach theTioga Mine, it follows up the Merced-Tuolumne divide, and crosses Tioga Pass.East of the Park, it is maintained as a stateroad ; but the western end, long unused andnow impassable for vehicles, is simply aPack Train at Vogelsang Pass . Mt.

Clark is seen in the distance .

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ON THE CALIFORNIA SKY-LINE

99

Huna Crest, seen from meadows near Mono Pass.

well-marked, though very rocky, trail through the central zone of the Parkto Tenaya Lake and Tuolumne Meadows . It is necessarily traversed inpart by those who go north from the val-ley, whether to the upper Tuolumne or toHetch Hetchy.

This road could be put in good shape,and connected by a branch road from AspenValley with the Big Oak Flat road, at com-paratively small cost . When this is done,we shall have a practicable highway, asnearly direct as is now possible, from Yo-semite to Tenaya Lake and the Tuolumnecountry, and forming part of a transcon-tinental automobile highway . Such a roadwould be very much used . Next to morehotels, it is the greatest present need of thePark. The government project of a roadfrom Yosemite to Nevada Fall and LittleYosemite, and thence across one of thepasses east of Clouds Rest, promises in timeto give the Park a magnificent highway bythe upper Merced to Soda Springs . But itwill probably cost four or five times as muchas the other, and, in view of Congressional Mountain Hemlocks (T.saga merten-

siana) on east slope of Mat-indifference to "mere scenery," is not likely

terhorn Cason, where there is a

to be built within a decade .

remarkable forest of this mostgraceful of alpine trees .

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YOSEMITE AND ITS HIGH SIERRA

Outing parties visiting the High Sierra may now leave YosemiteVillage, where camp equipment and supplies, horses and guides are to be

had, by one of severaltrails . The most popu-lar are those by NevadaFall, Little Yosemiteand Lake Merced, in theMerced Canon, and byLake Tenaya and theTioga road to SodaSprings and TuolumneMeadows . There is also

In Alpine California . Above,Mt . Gana Glacier, seen fromthe summit, with camerapointing sharply downwardto the 'moraines and snow-cov ered ice cascades . Be-low, an arctic pool, not atthe North Pole, but in BloodyCallon.

a good trail from GlacierPoint south, across thewooded uplands, to thelake country north of Wawona ; and, on the north side, a new route con-tinuing the Yosemite Falls trail has been opened to Hetch Hetchy.

The pierced route, besides its branch trails to Clouds Rest, Mt . Clarkand the Illilouette head-basin, connects with other well-blazed trails crossing

the divide to the Tuolumne through Cathedraland Tuolumne Passes ; and also offers access tothe entire upper watershed of the Merced River.In this basin, the Merced's branches flow downfrom cirques and snowfields which form a greathorse-shoe stretching from the Merced Rangeand Triple Divide Peak, on the south, along thecrest of the Sierra to the Cathedral Peak Range.Its principal peaks, reaching elevations of twelveand thirteen thousand feet, are Long, Foerster,Electra, Rodgers, Lyell, McClure, Florence,Parsons, and Vogelsang,—a splendid line ofsnow-fountains, forming a vast amphitheaterlaced with canons, and ridged by great morainesof the old Merced glacier . In this wild region,

Cutting Steps up the Snow-Finger on alt. I.yeu .

Mr. Muir counted sixty-seven glacier lakes, not

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Luncheon on the Lee Side of Lyell Summit . View looking across North Fork of the San Joaquin.

I t

Sierra Club Climbing the North Slope of Mt . Lyell . Donohue Pass is seen below on the left, leading down to the Rush Creek country .

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YOSEMITE AND ITS HIGH SIERRA

Rodgers, Electra and Davis Peaks, seen from near Island Pass.

to mention scores of others across in the Illilouette basin and on the southside of the Park, in the watershed of the MVlerced's South Fork.

This whole southeastern section is a favorite haunt of sportsmen, sinceits lakes and streams are abundantlystocked with trout,—as, indeed, arethe waters of the entire Park. Manythousands of young trout have beensuccessfully planted in nearly everystream and larger lake, up to nineor ten thousand feet . Nowhere inAmerica is there better fishing.

Down in Yosemite Valley, theMerced shelters many an educatedtrout that exhibits only indifferenceto the lures of the fly-book. Butback in the streams and lakes of thehigher altitudes, as well as in theless fished waters of Hetch Hetchy,during July and August, even anovice may fill his creel with glitter-ing beauties . The native Rainbowtrout (Salmo ivideus) is widespreadin the Sierra . The Eastern Brooktrout (Salvelinus fontinalis) , intro-duced here from the hatchery nearWawona has multiplied extensively'on the upper Merced, especially in

A Convenient Crack. Such chance fissures -frequently offer the only possible trailsacross the glacier-polished granite slopes .

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S mmit of Mt. Lye11 (13,090 ft .) . Made in the mountain spring (July), this picture shows the fine north-side glacier still too deeplycovered with snow to disclose its characteristic crevasses,

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YOSEMITE AND ITS HIGI-I SIERRA

The "llergschrund" of Lyell Glacier . This German word ("mountain rift") is applied tothe great crevasse stretching across the head of every active glacier at the point whereits motion begins, and the ice-stream pulls away from the summit snowfield . To theweathering of the slope exposed in such crevasses, through daily thawing and freez-ing in summer, is chiefly due the head-wall cutting that digs the "cirque" or glacialhead-basin far hack into the heart of the mountain, and opens passes through the range.This is now recognized as the prime factor in the sculpturing of high mountain dis-tricts . The upper rim of a bergschrund often overhangs, as here, in a "°snow-cornice."

Merced and Washburn Lakes, and also in the Tuolumne basin . A fewTahoe trout (Salmo mykiss henshaw'i) are also to be taken in the Merced,and an occasional Loch Levin, or hybrids of it with native species, rewardsthe angler. On the other hand, the wonderfully brilliant and gamy Golden

trout of high altitudes inthe Mt. Whitney region isnot found here. It is to becaught only in the lakes andstreams of the southernSierra, notably in the Cot-

"i tonwood Lakes, where it isknown scientifically asSalmoagua-bonita, and in VolcanicCreek (Salmo roosevelti).

For those who mixmountain climbing withtheir fishing, or vice versa,The Uplands in July . View of Echo Peak from Unicorn

Peak, with alt. Holfmau iu the distance .

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ON THE CALIFORNIA SKY-LINE

IOj

the snow-peaks that sentinel the Merced amphitheater offer fascinatingascents ; and the climber is rewarded with far-reaching views, both of thatwatershed and of the upper San Joaquin. But the best mountain climbingin the Park is doubt-less to be had fromTuolumne Meadowsas a base. The waythither from theMerced, by eitherCathedral or Tuol-umne Pass, is a day'seasy march acrosshigh country of

Above, Mt . Dana (13,050ft.), seen from Gibbs. Be-low, Gibbs Mountain (12,-700 ft .), from the Dana-Gibbs saddle.

broad, snowy cols andsunny, wind-sweptplateaus, dotted withpeaks of curious gla-cial architecture andshining granite bosses,

all burnished by the recent ice . It is country of immense interest, becauseit is astonishingly new,—so new, indeed, that the rapid disintegration com-mon to altitudes of nine and ten thousand feet under daily interchange of

The Craters of Mono County . This unique volcanic range, which lies in the desert ofEastern California, below Mono Pass, ri es 2 .500 feet above the near-by Mono Lake.The picture is a winter view from Pumice Valley .

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sun and frost has not yet tarnished the landscape . Glacier-polished slopesand benches are common enough on the uplands adjacent to Yosemite andHetch Hetchy. Here, on the edge of the snowfields, they are everywhere;but hundreds, perhapsthousands, of yearsyounger. How hard itis to take Nature's wordfor it, that this land ofsunshine and gentlestmountain airs, with joy-ous flowers in every hol-low that holds a spoonfulof soil, was yesterday asea of sullen ice!

Sununit of Mt. Conness (12,556ft.) . The cliff shown below isthe top of a 2,000-foot wall,part of the rim of an ancientglacial cirque.

Yosemite visitors whohave the time will find atrip to Soda Springs fromthe Merced, across one ofthe high passes, as fine anexperience as the Park cangive. But the Tuolumnemay be reached more

directly from the valley, either by the Yosemite Point trail or by the newSnow-Creek trail out of Tenaya Canon . Each of these trails soon bringsone to the Tioga road, which he follows to Tenaya Lake, and thence north-ward past Mt. Hoffman and Fairview Dome. This is the region traversedby the south branch of the Tuolumne glacier, on its way to Tenaya Canonand Yosemite . The cleanness of the country is amazing, and we realizehow the mighty ice-stream stripped the whole region bare of its overlyingsedimentary rock, and left only the hardest granites .

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Cathedral Peak Range, seen from the Tuolumne Meadows. View from junction of the Dana and Lyeli Forks of Tuolumne River, show-ing Fairview Dome on extreme right, with Cathedral Peak beyond . Unicorn Peak is the high mountain on the left .

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Ten:lyn Lake, keen front the old Tioga Rona . built Tunn years at_'o across the Sierra by the owners of the once iiinlous Tioga 1iine.East of Tioga Pass this road is maintained by California as a State hig9ncay, but vest of the suainnit it is still privately- tinned,though non within the National Park . This portion has long been unused, but there is a gro n-i ug demand that it be purchased bythe Government and improved.

Lambert Dome and Tuolumne Jleado la's, with Mt . Dana in the dista nee. The easy slope on the east or up-stream side of this and otherdomes, will. their sheer nest faces, indicates the direel ion in which the :nlrient 'i' ,olummlit. Glacier Honed . Fairview Domc, south ofthe Olen d,, .•w, wh,r ~~w n wln,llnr In,•Ilnr .

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109

Matterhorn Callon . seen front its east slope . Matterhorn Peak (12,272 ft .), is on the sky-line at right, and the Saw-Tooth Range in the distance on left of center.

The trails radiating from Tuolumne Meadows bring a score of im-portant peaks, with their glaciers and snowfields, within easy reach of theclimber . The story of actual ascents must be left to our illustrations show-ing some of the adventures of California's great Sierra Club.

Of all high mountain scenes, the glacial head-basins are the most inter-esting. For they hold the secret of the glacier's method . The fundamentalimportance of such cirques as makers ofmountain landscape was not recognized,even by leading geologists, till the lastdecade. Much less was it understood thatthe tool with which the work is done is the"bergschrund," or crevasse across the headof every living glacier, separating the mov-ing ice from the snowfield above (See page104) . That the bergschrund, through itsexposure of the head-wall to daily thawingand drenching, and to nightly freezin7.plucks huge rocks from the mountain, andso drives the cirque deeper and fartherback, till great peaks are undermined andoverthrown, and broad passes are cutwhere two glaciers head together, — thisworld-old romance of the silent, icy heightsis one of the newest nature-stories told by

The Hammond Fly-Cateher .

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YOSEMITE AND ITS HIGH SIERRA

View East from Benson Pass (10.130 ft .) . In the foreground, Wilson Creek Canon leadsdown to the Matterhorn Canon . Eight miles east, Conness Mountain rises at center ofthe sky-line,

twentieth-century science . So little were these things known a few years ago,indeed, that the famous Scotch geologist, Professor Geikie, could describethe "corries" or cirques of the Scotch Highlands as mainly excavated by

" convergent torrents, " dropping overtheir rims! But if Geikie's theorybegged the question, it remained for ourdistinguished American scientist, Dr.Gannett, president of the National Geo-graphic Society, writing as late as 1898,to ascribe the cirque to the avalancheswhich its steep walls induce:

Glaciers commonly head in amphithea-ters or cirques—basins lying under the shadowof the summit cliffs . An amphitheater is sur-rounded on three sides by vertical walls orsteep slopes, down which the ice and snowslide in avalanches . The effect is preciselylike that of a waterfall . The falling snow andice dig a hollow or depression at the foot ofthe steep descent, just as water does . Suchamphitheaters are found at the heads of allglacial gorges in the high mountains .—Na-tional Geographic Magazine, vol . 9, p . 419.

Dr. Gannett assumed the existenceof the "vertical walls" and "steep de-scent"—the very things his theory pro-fessed to account for! But field workby Johnson and Matthes discovered thereal cause. It is the bergschrund thatdigs the cirques and levels the peaks.

Snow Plant (Sareodes sanguinea),—themost curious and brilliant decorationof the Yellow Pine belt, where itsscaly stems and fleshy blood-redflowers closely follow the retreat ofthe snowbanks.

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I know a mountain thrilling to the stars,

Mt . Leell and its Glaeier.Peerless and pure, and pinnacled with snow;

Glimpsing the golden (lawn o'er coral bars,Flaunting the vanisht sunset's garnet glow;

Proudly patrician, passionless, serene;Virgin and vestal,—O, a very queen!—Robert W. Service.

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Banner Peak (12,957 ft .), Mt. Ritter (13,156 ft .), and the Minarets (12,000 ft .), seen from Shadow Lake (8,700 ft.), east of therange. 'These peaks are about file miles east of the Yosemite National Park, from which they are separated by the basinof the North Fork of San Joaquin River .

The Minarets . Mt. Ritter . Banner Peak.

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California's mountains crown allher diversified wealth of scenery andclimate. The story of her old glaciersis as fascinating as the new life of treeand flower which they have made pos-sible . Under the gentle and unfailingsunshine of the highlands, on one oftheir broadest alpine meadows, thosedauntless explorers, the members ofthe Sierra Club, led by America'sgreatest mountaineer, their president,have discovered the very Fountain ofEternal Youth, and proved it no fable,but a fact of the Yosemite Sierra.And what a leader is John Muir! Asone talks with him, or reads his books,George Sterling's lines on anothergreat Californian come to mind:

Of all he said, I best recall:"He knows the sky who knows the sod;And he who loves a flower loves God ."

Sky, flower and sod, he loved them all.

The Sierrans testify their love ofthe mountains by spending a montheach summer among them. This is thesanest and most joyous of sport. Itwas my privilege for the first time tojoin the club's large party last July attheir camp in Tuolumne Meadows, and there learn how two hundred andfifty men and women, drawn from all the professions, lawyers, teachers andstudents, doctors, preachers and business men, were able, after a day's climbing,to gather about a huge campfire, and jest away their weariness in club songs:

In the mountains of California,We're hitting the trail and shov-

ing our feet along.

Or, still more pathetically:There are rocks in the cradle

where I sleep,And roots and cones embed-

ded deep;Aslant I lie upon my bed,

My feet are higher than myhead.

I know I shall not hear the"call"

My camp is farthest off of all;And so I dare not go to sleep,

While ants and lizards o'er mecreep.

Group of 250-foot Sequoias, showing char-acteristic dome shape of crown whenunbroken. The sharp-pointed trees atsides are White Firs (Abies eoneolor).

'40004

t Woof

Nearing the Summit of Mt . Lyell.

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YOSEMITE AND ITS HIGH SIERRA

Piute Mountain, and Lakelet near the head ofSeavey Pass.

trout. "We estimate the age of a tree," saidgrowth rings . We estimate the ageof a horse by its teeth . We esti-mate the age of a woman by count-ing ten, and then asking . Weestimate the age of a fish by notingthe circles in its ear-bones ." Nowonder those "serious" campfiresdrew crowds of tired trampers!

This inspiring society is one ofthe most useful of California organ-izations . Its intelligent efforts tomake the mountain districts of thestate better known and more widelyenjoyed should have the support ofmany thousands of Californians,expressed by the payment of itsmodest membership fee . We com-plain that the East goes to Europeto see mountains . This will be trueuntil we make our mountains asaccessible as are the Alps, and aswell known . The Sierra Club is A Typical Glacial Cirque on Duna Crest . Such

a horse-shoe-shaped head-basin is dug byhard at work on that task .

each glacier, using the bergsehrund as a tool.

Ah! those mountainfiresides, after the longmarches over the snow-fields, or across the passes,or down the canons! Wewere not always frivolous.One evening, a brilliant col-lege philosopher put intocrisp English Plato's legacyto modern life. Again, areturned diplomat outlinedAmerica's relations with theOrient, and a well-knownHebrew scholar, turningfrom philology, very de-lightfully described the birdsof Yosemite . Anothernight, a distinguished sci-entist from California ' sgreat university explainedhow he told the years of a

the solemn professor, "by its

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-Upper Hetrh Hetchy . view-m-1 from Rancheria Trail on north side of Le Conte Point.North Dome is seen on the right, Kolana Rock in center, and Smith Peak on the left,4,200 feet above the floor of the Valley .

IV.

TUOLUMNE GRAND CAS±ON AND HETCH HETCHY

I see an eagle sweepAthwart the blue ; a gleaming river bindIn gorgeous braid the valleys golden gown;A cataract plunge o'er its distant steep,And flutter like a ribbon in the wind.

—Herbert Bash ford.

THE Sierra Club discovered the Fountain of Youth, which men havesought for centuries ; and having taken possession of it, now plansto guard the treasure well, sharing it, however, with all who may

come to drink its sparkling waters and breathe its mountain air . In thehomelier language of to-day, this coveted fountain is the "Soda Springs ."It is on the north rim of Tuolumne Meadows, a dozen miles by Tioga roadfrom Tenaya Lake, andtwice as far from YosemiteVillage.

No finer spot could befound for a mountaineers'rendezvous in the HighSierra . The great valleyknown as Tuolumne Mead-ows—a filled-up lake basinat the junction of the Danaand Lyell Forks of the Tuol-umne River—is about tenmiles long and two in width . Coasting on the Polished Granite, at the Waterwheels .

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YOSEMITE AND ITS HIGH SIERRA

Lower End of Tuolumne Meadows, with Cathedral Peak on the sky-line . The Tioga Roadskirts the south side of the Valley, which is also reached by many trails, making itthe most accessible point in the northeastern part of the Park, while the importantmountains surrounding it make it a favorite starting point for exploration . In the cen-ter of this picture is seen the Soda Springs tract of the Sierra Club, 160 acres, includ-ing the Springs themselves, at the edge of the wooded moraine north of the river bend.Tine Club will erect a lodge here . This view is from the summit of Lambert Dome.

On all its sides, the highest mountains of the central Sierra stand guard.Conness, Dana, Mammoth and Lyell peaks are upon the north and east.

The unique Cathedral Range overlooks itimmediately on the south . Lambert Domerises from its floor, and, still more beautiful,Fairview Dome towers over its lower end,where the river, leaving its quiet meadowreaches, plunges down the vast Tuolumnecanon on its boisterous way to Hetch Hetchy.

Upon this capital site, the club hasbought the old Lambert, or Lembert, home-stead, a quarter-section in the heart of theMeadows, which was preempted by JohnBaptist Lembert, a stockman, in 1885, be-fore the creation of the National Park. Thetract embraces several fine mineral springs,and with one exception is the only privateholding in the eastern section of the Park.The land is part meadow and part hillsidefacing the mountains on the south . Its cen-tral location, with the Tioga road runningsouth and east, and trails radiating to allparts of the Tuolumne watershed, makes it

Cathedral Creek Falls, the fine cas-cade by which Cathedral Creekdrops into Tuolumne Canon.

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TUOLUMNE GRAND CANON AND HETCH HETCHY

I17

the natural starting point, either formountain climbing, or for explora-

'''tion of Tuolumne Canon and thealluring region north of it. From itone goes with equal directness acrossthe passes to Mono Lake or west toHetch Hetchy.

Three or four times, at inter-vals of three years, the club hasmade Tuolumne Meadows a basefor its summer explorations ; andnow, on the one hundred and sixtyacres which good fortune has en-abled it to acquire, it proposesduring the coming summer to erecta lodge and establish a camp, thusmaking Soda Springs its permanentTuolumne headquarters . Here willbe provided simple entertainment,not only for members of the SierraClub, but also for those of similarassociations who may visit theMeadows, and for such others asthere may be room to accommodate.It will be named "Parsons Memorial Lodge," in honor of the late Edward T.Parsons, long a director of the club, and one of its most active mountaineers.Arrangement for accommodations should be made at LeConte Lodge inYosemite. As the Panama-Pacific Exposition will doubtless bring a host ofmountaineers to California, the new camp on the Tuolumne should aidmany in exploring the Park.

It is a day's good walk from Soda Springs to the summit of Mt . Danaand back. The Tioga road and Dana Fork are followed to the foot of

the mountain, whence the trail climbsthe pass between Dana and Gibbs.The ascent from the saddle is shortand easy . The summit of Dana com-mands a view of more snow-peaks,probably, than one can see with solittle labor anywhere else on the con-tinent, while a mile down on the eastside lie Mono Lake, rimmed with finemountains, and, south of it, a grayand grim line of volcanic peaks.

From the Dana-Gibbs saddle oneday last July,—the only stormy day

Glen Tulin and Wildeat Point, near the up-per end of Tuolumne Grand Canon.

Spermophiles at Connes Creek .

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Tuolumne Falls, at the Head of the Grand (anon of the Tuolumne ;—first and most im-portant of the cascades by which tills nobly turbulent river, dropping 5,600 feet intwenty-five miles, comes to tie quiet waters and lovely wild gardens of He-tell Hetchy .

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Grand Carson of the Tuolumne, seen from its north wall, looking across to the deeplyeroded side of Falls Ridge. This vast cutting by glacier and stream extends from Tuol-umne Meadows to Hetch Hetchy, twenty-five miles in length and from 3,000 feet to amile in depth .

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Largest of the "Waterwheels," Tuolumne Canon.

of the Sierra Club outing,—I beheld a scene that can never be forgotten.In Tuolumne Meadows, westward, it was raining lightly ; but below us, onthe east, a wild thunder-storm swept the Mono Lake basin with lightning andrain. All the great amphitheater seemed filled with the black, solid mass of

the tempest ; but as flash upon flash pierced thedarkness, we saw, vivid as day, the breakers beat-ing the shore of the lake, and the trees upon theislands that dot its breast . While this stormblackened the Mono basin at our feet, beyond,stretching far into Nevada, range after range rolledaway, waves of a sea of mountains, flashing in thesame sunshine that bathed our lofty outlook.

Other peaks are reached from the Tuolumnebase with almost equal ease . The trail to Mt. Lyelland its neighbors follows up Lyell Fork, and un-folds a succession of splendid mountain pictures . Inother directions, trails lead north to Conness Moun-tain, remarkable for the sheer walls of great glacialhead-basins, and to beautiful Matterhorn Canonand the Benson Pass country . Those who like stillharder climbing may go with the Tuolumne downthe whole length of its rough canon to HetchHetchy. The Sierra Club parties commonly divide,

A Fair Iinapsacker, readyfor Tuolumne Canon trip . as did that of last summer, part taking the trails

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N t i le, . . I . .•cl I .11 s, In 1he 'Iunlo . . .11e 1,raod I'n no . . . Ilene the river, s h uuli ..g•ilolvn a smooth granite thine, strikes several bowl-shapeddo pre aala ua larun• .1 b . 1144 rrnsluu ul .•uu .pn rnll .rl~ soil suits In the ruck, and is hurled far aloft, thirty to forty feet at high water,la Me .4 no, . hubl . ` . . hrr Is" sI .u . .n iiione .

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across the uplands, the rest choosing the pathless river gorge . The formerroute offers the inspiration of wide views from the heights ; the latter, thezest of a long scramble across huge boulders and polished benches, aroundfrequent cascades, and over the walls of such impassable box-canons asMuir Gorge . The cation of the Tuolumne is one of the deepest and wildest

glacier-troughs in the world.Its walls rise to heights of amile above the mad river,with constantly changing in-terest in their sculpture.

The falls of the Tuol-umne are nowhere compara-

Benson Lake, one of tJoe most Die -tlu•esilne of the Park's alpinelakes . The inlet is seen above;the outlet below.

ble in altitude with Vernal orNevada Falls, but they havethe fascination of infinite va-rietyand the impressive power of repetition, while their setting, at the bot-tom of this truly grand canon, is far more stupendous and wonderful thanthat of the great Merced cataracts . For twenty-five miles of cascades,rapids, sheer falls of considerable drop, and delightful glacial tarns, thewild river plunges down a path so narrow and difficult that to follow ittwo or three miles is sometimes a day's work for a party of experiencedclimbers . Even these climb over and around Muir Gorge, rather than risktheir lives in its deep flume.

Camping at Conness Creek basin,

Cookstoves on the march. Part of the SierraClub's comuiissar3 in motion .

below the splendid Tuolumne Falls,and at the foot of the noble WhiteCascade, most of the Sierra Clubparty in July went down the canonas far as the Waterwheel Falls.These surprising water forms arefound where the turbulent river,shooting down smooth inclines atfurious speed, drops into spoon-shaped depressions caused by theerosion of soft rock . The water ishurled aloft, twenty to forty feet atdifferent stages of the stream, and

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Rodgers Lake . View looking down from the trail to Benson Pass. This fine alpine lake is a fat orite camping spot of the Sierra Cluband other parties exploring the north side .

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YOSEMITE AND ITS HIGH SIERRA

the backward action of the spray gives a good imitation of a wheel revolv-ing with great velocity.

Returning to Conness Creek, we took the high trail up the fine ColdCreek Meadows, and across Virginia Canon, thence climbing an unnamedpass to reach Miller Lake, and late in the day descended through a note-worthy forest of mountain hem-locks to our night's camp in Mat-terhorn Canon. MatterhornPeak and the canon are worthseeing, but the next day, after wehad climbed the long trough ofWilson Creek to Benson Pass,and then ascended the hills over-looking the pass at an elevation

In the Heart of the Tuolumne Grand(anon. The lower siew shoes theentrance to Muir Gorge.

of about Io,Soo feet, a wonder-ful array of mountains, canons,valleys and lakes swept majestic-ally from Conness on the eastaround the circle to RancheriaMountain and the blue deeps of

Tuolumne Canon in the southwest . Everywhere the vast amphitheater toldof its ancient inhabitants, the glaciers, now long vanished, but proclaimedin the clean-cut cirques, deep-set glacial lakes, and silvery waterfalls drop-ping from hanging valleys high on distant canon rims.

Descending from Benson Pass, the trail wound round Volunteer Peak,past Smedberg Lake, and in the sunny afternoon brought us to camp on

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COPY RIGHT, F . M . FULTZ

Muir Gorge . View from its lower end, looking' up the Tuolumne . Half a mile above thispoint the river contracts into a race-like stream, hemmed in by the precipitous wallsof a box canon, impassable save at lowest water . Only a few daring climbers haveever made the trip .

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YOSEMITE AND ITS HIGH SIERRA

Rodgers Lake, the queen of allthe lakes, on the north side ofthe Park. Leaving this campthe next morning, abandoningthe delightful lake shore wasa hard parting . But the daybrought new wonders in thegreat views it gave us of Tuol-umne Canon, as the trail skirtedits north wall. Camp at nightat Pleasant Valley in PiuteCanon was followed by the longascent of Rancheria Mountain,the next day, through forests ofred fir (dbies magniica) thatwere a joy to see. These statelytrees justify Chase's enthusiasm :"If I were called upon to choosethe one among the conifers thatI would live and die by, I shouldchoose the red silver fir, with nofear of ever wearying of itssublime companionship ."

Reaching camp on Ranch-eria early in the afternoon, wehad more glimpses down intothe Tuolumne abyss, and still

more the following morning, when the trail led us westward to RancheriaCreek . The descent into its canon brought us to its charming falls, and finallyto the Mecca of our pilgrimage, lovely, famous, fought-over Hetch Hetchy.

This book is not a brief for or against the San Francisco power andwater dam. Enough has already been said on both sides of that controversythat were better left unsaid ; and although I have been heartily with those whoopposed the commercializ-ing of any of our too fewnational parks ; who deemedHetch Hetchy, properlydrained and made access-ible, infinitely more valu-able, even to California, asa park than it can ever be asa reservoir for water that isobtainable elsewhere ; andwho saw behind the call for

Weighing the Dunnage. This ceremony precedes eachincreased water supply a

day's march on a Sierra Club outing.

Little Ketch Hetchy, a mile above the main Val-ley; Kolana Rock in the distance.

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Waterfalls and Cascades in the Tuolumne Grand Cation.

River, Meadow and Forest in Hetch Hetchy . Here the peaceful Tuolumne presents a striking contrast to its turbulence in the cationabove. The trees are mainly black oaks and yellow pines,

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YOSEMITE AND ITS HIGH SIERRA

vast municipal power project, andquestioned the propriety of Con-gress endowing such an undertakingwith public property worth manymillions ; nevertheless I recognizethat many conservative and disinter-ested Californians, both in and outof San Francisco, hold the oppositeview, believing that the conversion isnecessary, and that it need not closethe Tuolumne watershed, or precludethe establishment of sanitary campsand hotels for visitors who may wishto explore the Tuolumne highlands.The issue has been fought in goodfaith, and to a finish . Congress hasacted sincerely in the belief that thenecessities of this case transcend thedanger of a possibly troublesomeprecedent . Its action, unless re-pealed, settles the question so far asthe country at large is concerned ; thematter now rests with the courts andpeople of California . I have roomonly to point out the fact that thosewho would know Hetch Hetchy mustsee it before it ceases to be the unique

and glorious vale it is to-day . The Yosemite Park contains many lakes asfine as this will be ; it has only one Hetch Hetchy.

If there were no Yosemite, Hetch Hetchy would doubtless be themost celebrated valley in America . But it is misleading, though easy, todescribe it as merely a minor edition of the more magnificent canon . Theresemblances, of course, arestartling. Sheer gray wallsof granite, marked with"royal arches," crownedwith domes, and hung withsplendid waterfalls, rim asimilar level valley floor.This records the filling of anancient glacial lake, whichis still more plainly recalledin the rock sill at its lowerend. Here the Tuolumne,

Unnamed Lake in Eleanor Canon, at the foot of theoverhanging rock shown on page 134.

Sunrise in Hetch Hetchy.

after flowing lazily for

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"The Tvcins," a splendid double tree in the Tuolumne Grove .

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In Mariposa Grove.

Thy giant brood, . .Children of elder time, in whose devotionThe chainless winds still come and ever cameTo hear an old and solemn harmony.

—Shelley .

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TLOLLNINE GRAND CANON AND HETCH HETCHY

1 3 1

three miles amidst mead-ows and forests, is cut-ting a narrow box canon,too shallow as yet tosave the valley from an-nual inundation byspring floods . Freedthus from unwonted re-straint, the impatientstream resumes its roleas a canon torrent, andbounds wildly away tojoin the San Joaquin.

But Hetch Hetchyhas a character and at-mosphere all its own . Itlies five hundred feetlower than Yosemite ; itis only half as long andwide, with walls two-thirds as high . Thesmaller canon is warmer, sunnier, more gracious . Its beauty is less appalling,but so much more intimate and lovable that save for the formal resemblance

Lake Eleanor, five miles northwest of Hetch Hetchy . This beautiful mountain-walledlake, enlarged by a dam at its outlet, will form part of the San Francisco water system.

Fix e-Finger Falls, in Raneheria Creek, Heteh Hetehy.

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Central I-Ietch Hetchy, the Yosemite of the Tuolumne. View from Surprise Point on the south trail. At the middle of the south wall(right), Kolana Rock rises approximately 2,04111 feet . Opposite are two flue water falls, Tueealala and Wapama, with the RetellHetehy El Capital( (1,900 ft.) between them . Beyond is North Home (2,400 ft .) . The likeness of this famous but little known cationto the still grander -Yosemite of the Merced is seen in its sheer walls, with their cataracts, "royal arches" and domes ; its level,filled-lake floor, and its vvinding river, bordered with flowery meadows and groves of splendid pines and oaks,

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Upper Retch Iletehy', seen front the bench of the north wall . The foreground shows the alley at its least width . Its elevation abovesea let el is 3,660 feet. On the left, beyond the foot of North Dome, it widens to meet the callous of Till Till and Raucheria Creeks;Rancheria Mountain forms the distant sky-line. Retch Hetchy ends where he Conte Point, the conical mountain in the middle dis-tance, cuts off Little Retch I-letchy beyond, crowding the Tuolumne River against the foot of Smith Peak, the long slope of whichrises east of Kolana Rock on the right .

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YOSEMITE AND ITS HIGH SIERRA

and contiguity of the two valleys, a readerof mountain character would hardly comparethe gentler graces of Hetch Hetchy with thestupendous grandeurs of Yosemite.

The walls of Hetch Hetchy, imposingin their height and sculptured forms, willmake a very splendid frame for the restoredlake . Its two great waterfalls, with the cas-cades in thebranch canons ofRancheria a n dTill-Till Creeks,so far as notburied by therising waters,will alwaysbe among themost beautifulin the Park. Butits valley floor,with all thesplendor ofmountain flowersand stately for-ests, will be over-whelmed . Nolake can evercompare withsuch a valley, ormake up the lossof such grovesof pines andoaks . Black oaksdominate thisvalley floor, justas the yellowpines are su-preme on the floor of Yosemite . Taller thanthe live oaks, with vast crowns of brightdeciduous foliage, they form here the noblestoak groves I have ever seen ; and I advise myreaders who love beautiful trees to see thesegreat oaks, and walk among them, and bathein the cool Tuolumne beneath their spread-ing shade, before it is too late.Yellow Pines (Plains ponderosa) .

Overhanging Rock at EleanorCanon. This little knowncliff rises two thousand feetor more above one of themost beautiful lakes in theNational Park.

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Lower Hetch Hetchy, seen from the Lake Eleanor Trail . The dam which will impound the Tuolumne for San Francisco's water andpower supply is to be erected at the end of the meadows, where the bills come together, forming a boa cation less than a hundredfeet wide. It will have a height of 377,0 feet, throwing the waters back for seven miles, and flooding both Ileteh Hetchy and LittleHeteh Hetchy Valleys . Around the lake thus formed, it is proposed to build a fine automobile road .

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A Contemporary of Noah . The famous "Grizzly Giant," patriarch of the Mariposa Grove,has watched the career of man upon the earth for at least forty centuries . It is oneof a few very ancient trees found in the several groves, and believed to be survivorsof a former generation of Sequoias,—doubtless the oldest of all living things. Thisvenerable Big Tree is thirty feet in diameter ; its largest limb is six feet thick. Itsheight, 204 feet, however, is less than that of ninny younger trees, the storms havingdestroyed much of its crown. It shows few signs of senility, and may live many cen-turies more,

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Cavalrymen at the Cabin in Mariposa Grove. For many years the National Park hasbeen policed by a detail of United States cavalry, and its Superintendent has been anArmy officer. This system, however, has been changed by the present Federal admin-istration to one of civilian supervision,

V.

THE "KING OF THE FOREST"

In terraced emerald they standAgainst the sky,

Each elder tree a kingwhose fame the wordless billows magnify.

—George Sterling : "An Altar of the West ."

HE crowning glory of the Yosemite country is its forests . Of these

T the three groves of Big Trees (Sequoia gigantea), especially the greatMariposa Grove, reached by way of Wawona, represent the climax

of plant life . To leave the Park without seeing them is unthinkable,The Yosemite forests begin with the magnificent yellow pines and

incense cedars (Lib-ocedrus decurrens),as well as black andmaul oaks, which doso much to softenand adorn the deep,wide valleys on theMerced and Tuol-umne . Whether welook down on thesenotable forests fromthe valley walls, orwalk among their A Fish Story from Laurel Lake. One day's catch of a party

of sportsmen.

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YOSEMITE AND ITS HIGH SIERRA

fine trees, we quickly recognize that, unparalleled as is their setting, theyare worthy of it.

Quitting the valleys for the uplands, we soon find the yellow pineyielding in number to the great sugar pine of California and southern Ore-gon . On the plateaus above, first place is taken by white fir (Abies con-color), and held up to about 7,500 feet, where the still more imposing redfir (Abies magnifica) supplants it . Each of these typical Sierran treesforms large and delightful forests in many parts of the Park . Along with

Wawona Meadows and the South Merced Valley . seen from Wawona Point, near theMariposa Grove.

red fir, Jeffrey and mountain pines are found, to the nine thousand footlevel and beyond, where the graceful mountain hemlocks dwell, and thetamarack or lodgepole pine (Pines contorta murrayana) takes up its taskof covering the thinnest soils with gaunt forests that seem to belong to thestern, new landscapes. On the highest ridges, outposts of stunted white-bark pine (Pinus albicaulis) march with the hardiest alpine flowers to thevery snow-line. But it is the Sequoia which, in interest and importance, risesimmeasurably above the Park's other forest wealth, peerless among allgrowing creatures of the soil in age and size, and equally preeminent inbeauty and distinction .

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THE "KING OF THE FOREST "

1 39

Would you know what the famousBig Tree really is, how it outlives allits forest comrades, enduring by thepluck that meets calamity with a laugh?A volume of botanical data would tellless of its habits, its virility, than onemay learn by seeing a single example ofSequoia well-doing . Let us visit thelittle Tuolumne Grove, on the westboundary of the Park . This containsonly thirty trees, among them some ofcolossal size and perfect proportion.But we have come to see a burnt andshattered stump that sets forth the vir-tues of its clan more bravely than any

of its comelierpeers. It is theso-called "Kingof the Forest ."

Among myboyhood friendswas a worthy butbroken old man.In earlier yearshe had servedhis communitywell . Then mis-fortune and i l lhealth dealt hima cruel slap, andhis kindly hearttook on a veneerof eccentricity.He became a vil-lage "character ."His neighbors,loving him butknowing thetwist, put himgently by as anegligible "backnumber ." Butwhen a test camethat tried thesoul of our town,

Red Fir (Abies magnif-lea), on RaneheriaMountain .

"Alabama," in the Mariposa Grove . Itstypical dome-shaped crown indicatesthat it has been exceptional in thusfar escaping damage by storm .

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1 40

YOSEMITE AND ITS HIGH SIERRA

it was "Old Ben," the super-annuate, whose fiber andcourage saved the day.

The forest life, too, hasits crises ; it provides testsof the hardest. And ashuman wrecks often regaintheir footing and makegood, so a tree that by allsigns is down and out, likean obsolete and seedy poli-tician, or king discrowned,—may not it "come back"?

Originally our tatter-demalion "King of the For-est" was one of the noblestBig Trees. It had a circum-ference of nearly a hundredfeet . Its height was doubt-less three hundred . Itscrown was worthy of amonarch of giants . Aroundit the tides of ordinary treelife rose and fell . Pines andfirs, the sturdy commoners

of the forest, spanning out their little generation of three or four centuries,came and went. But His Sequoia Majesty ruled on . Fortwo thousand years, or even three, it was the pride ofits stately grove.

Then came disaster that would have wiped out anyother tree . Fire destroyed one side of it, and ate awayits heart. Of the huge bole there remained hardly a halfcylinder of sound wood and thick cinnamon-colored bark.The crown fell, but this charred fragment stood, ninetyfeet of hollowed stalk, still flaunting two or three scorchedand ragged little limbs. It seemed merely a lopsided andludicrous monument to departed grandeur . Surely evena forest king, in such plight, might yield without dis-honor, and returning to the soil await reincarnation inanother age of Big Tree life . But not the unconquerableSequoia . Blood will tell ! So long as a sound root re-rnained, and sap still flowed, this "King" would be noless than kingly.

Mustering its diminished resources, the strickenmonarch held its ground . It is the Sequoia way, if a tree

Maul Oak (Quereus chrysolepls), on SYawona Road.This familiar tree, also known as "Canon Live Oak,""Gold-Cup Oak," etc., is common on hillsides andcanon walls in the lower half of the Park, andcovers the talus and rock ledges of Yosemite andHeteh Hetehy with low-spreading evergreen foliage.

Mariposa Lily (Ca l-ochortasveuustus) .

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THE "KING OF THE FOREST "I4I

be weakened by fire, to clutchthe soil more broadly than be-fore . Thus, here, the few re-maining roots were sent fartherout, and new stores of nour-ishment drawn upon . But itmust do more than feed . Itis a tree's office to be beautiful.It is a king's right to wear acrown. So now the surviving

"King of the Forest." a mere shell,left by fire, of what was once themonarch of the Tuolumne Grove;now making an heroic effort to re-build its crown, and get a new startin life. The three figures at its baseshow that its diameter was aboutthirty feet. The fine tree in theforeground below is a six-foot RedFir (Abies naagnifica),

branchlets are cheerily turningupward,—also after the habitof the species when, crushed bylightning or storm, it quickly

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142

YOSEMITE AND ITS HIGH SIERRA

rebuilds its top ; and one of them has already taken shape there, far aloft,as a symmetrical young tree, undaunted by adversity, and fighting for itsshare of air and sunshine . Thus would the living skeleton hide its shameby grace of new foliage. Here's wishing it luck! Royal endurance meritshomage. Long may so kingly a forest "character" play a part in the treeworld! An eminent expert, famous for his knowledge of mankind, once

Three Veterans,—the "Haverford" and "Ohio" trees in the Mariposa Grove, and GalenClark at the age of 93 . This is said to be the last picture of the celebrated "Guar-dian of Yosemite," who died a year later, in 1910. The "Haverford," named for thecollege in Pennsylvania . illustrates the Indian practice of using Big Trees as back-logs for fires . Although its core was burnt away, leaving a cavern that is reputed tohave sheltered seventeen horses and their riders, its remaining roots have reachedout the more stoutly for nourishment, and are supplying ample sap to stalk and crown.

declared : "Skin for skin, yea, all that a man hath will he give for his life ."This Sequoia King, more than human in its tenacity, is a veritable Job ofthe forest . Its faith forbids death . Better to keep on growing againstodds, better to live even as a misshapen cripple, showing what humblebeauty it may, than to stand a black and rotting shell where once it reignedSovereign of the Woods! Truly, it is not alone in the Forest of Ardenthat we

Find tongues in trees, books in the running brooks,Sermons in stones .

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NOTESTransportation, Hotels, Camps, Guides, etc .—Yosemite Valley is about 150 miles due

east of San Francisco . It is reached by either the Southern Pacific or the Santa Fe Rail-way to Merced, 145 miles by rail from San Francisco and 330 from Los Angeles ; by theYosemite Valley Railroad from Merced, 78 miles, to El Portal, just outside the NationalPark boundary, and by automobile stages from El Portal to Yosemite village, 12 miles.Round-trip tickets from San Francisco to Yosemite, $22 .35 ; from Los Angeles, $31.20.Sleeping-car berths, $2 .50 each way.

Del Portal, the Yosemite Valley Railroad's hotel at El Portal, is more than a stop-ping place on the way to Yosemite, as it offers excellent accommodations for sportsmenhunting or fishing in the near-by mountains, or tourists visiting the Merced and TuolumneSequoia Groves . Hotel Rates, $4 .00 per day, or $22 .50 per week, upwards . Automobileround trip to the Big Trees, made in one day, $7 .50.

Tourist accommodations in Yosemite are provided at present by the Sentinel Hoteland three large permanent camps . While a larger and modern hotel is promised by thePark administration for the season of 1915, the Sentinel Hotel, opposite Yosemite Falls,W. M. Sell, Jr ., manager, gives good service at the prices charged, $3 .50 to $5 .00 a day,or $23 to $30 a week ; for two persons in a room, $3 .00 to $4 .00 a day, or $20 to $25 aweek . Camp Ahwahnee is situated at the foot of Sentinel Rock . It is well managed byW . Al . Sell, and offers an excellent table with clean, roomy floored tents at $3 .00 to $3 .75a day, or $17 .50 to $22 .75 a week. Camp Lost Arrow, near the foot of Yosemite Falls,W. M. Sell, Jr ., manager, is a popular resort at $2 .50 a day or $15 a week.

Camp Curry, D. A. Curry, proprietor, at the upper end of the valley, is the largestand best known of the camps. Its structures include offices, dining rooms, steamlaundry, bakery, bath house, swimming pool, etc . Comfortable tents are provided for1,000 guests . Rates, $2.50 a day, or $15 weekly. At Glacier Point, overlookingYosemite and Little Yosemite, W . M. Sell, Jr ., conducts a hotel and camp . Rates, $2 .50to $4 .00 a day.

Free sites are designated by the Superintendent in different parts of the valley forparties wishing to establish temporary private camps . Cut firewood may be bought fromthe Superintendent. Tents, camp outfits, groceries and other supplies, as well as outfits

Del Portal, the Yosemite Valley Railway Company's attractive hotel nt El Portal .

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1 44

NOTES

for High Sierra trips, are obtainable from the well-stocked general store of W . D.Thornton in Yosemite . Thornton's store is also the post office . A bakery and confec-tioner's shop, meat market, laundry, telegraph and express office , with several photo-graphic and art studios, will be found in the village.

Carriages from the hotel and camps to all parts of the valley, and horses and guidesfor the trails, are supplied byJ. W. Coffman, under regula-tion of the Superintendent, atwhose office the authorizedrates may be obtained. Ar-rangements and prices shouldbe made in advance throughthe hotel or camp management.

Camp (lorry . delightfully situ-ated among the pines at thefoot of Glacier Point one milefrom Happy Isles. This is thelargest of the tourist camps inYosemite Valley. The littleDouglas squirrels are commonthroughout the Park.

Wawona and the MariposaTtilaNNINKt"Grove . — Transportation fr em

Yosemite to Wawona, 26 miles, and thence to the Mariposa Big Tree Grove, is by theautomobile stages of the Yosemite Stage and Turnpike Company. Rates, Yosemite toWawona, $6 .50, round trip, $13 ; Yosemite to Mariposa Grove, $7 .50, round trip, $15.Transportation Yosemite to Glacier Point by stage, via Inspiration Point and Chinquapin,$6 .50 each way. At Wawona, the Wawona Hotel is one of the best kept mountain inns inAmerica; rates from $3.50 to $4 .50 a day.

Automobiles .—Automcbiles are now admitted to the Park . Good roads from Stock-ton, Modesto and Merced, in the San Joaquin Valley , lead to the west boundary of thePark, connecting with the Coulterville and Big Oak Flat roads . Automobiles are per-mitted to enter the Park over either of these roads, but east of the Merced Grove theyare limited to the Coulterville road as far as Big Meadows, whence they may either pro-ceed directly to Yosemite, or take the new road via El Portal . A fee of $5 .00 is chargedfor permit . Garage and automobile-camp sites are provided in the valley . For regula-tions apply to the Superintendent.

Literature .—The useful pamphlet, General Information Regarding Yosemite National

Park, may be had gratis at the office of the Superintendent in Yosemite Village, or bymail from the Department of the Interior, Washington, D . C. It contains brief notes onthe Park and its administration ; altitudes, distances, trails, etc . ; size of Big Trees inMariposa Grove ; rules and authorized rates of transportation ; hotels, camps, and camp-

Page 144: YOSEMITE AND ITS HIGH SIERRA BY JOHN H WILLIAMS

NOTES

Iq-S

ing outfits ; automobile regulations ; and a bibliography of books and important magazinearticles . Two other government pamphlets are for sale at the Superintendent's office:Sketch of Yosemite National Park, a popular account of Yosemite geology by F . E . Matthes,of the U. S. Geological Survey, price 10 cents ; and The Secret of the Big Trees, by Ells-worth Huntington, price 5 cents . Foley's Yosemite Souvenir, a handy pocket guide, may bepurchased at J . D. Foley's studio in the village.

Of the earlier books, Dr . L . H . Bunnell's Discovery of Yosemite, 1880, 4th ed ., 1911, isthe best account of the Indian war of 1851 and the visits of the Mariposa Battalion . Thelast edition is handsomely illustrated from photographs by Boysen . In the Heart of the

Sierras, by J . M. Hutchings, 1886, is a history of the valley by one of its earliest residents.Prof . J . D. Whitney's The Yosemite Guide-Book, 1871, despite its obsolete theory of thevalley's origin, is a very readable and informing essay . Mountaineering in the Sierra Nevada,

1871, by Clarence King, who was Whitney's associate in the geological survey of Cali-fornia , is one of the best books inspired by the mountains of the West.

Three booklets, Indians of Yosemite Valley, 1904 ; The Big Trees of California, 1907;and The Yosemite Valley, 1910, by Galen Clark, discoverer of the Mariposa Grove andlong the guardian of Yosemite under the state regime, contain much first-hand informa-tion. The fullest and most valuable description of the Park, with its glaciers, past andpresent ; its forests, flowers, birds and animals, is of course, John Muir's Yosemite, 1912.Muir's other books, My First Summer in the Sierra, 1911 ; The Mountains of California, en-larged ed ., 1913 ; and Our National Parks, 1909, are also full of Yosemite . Naturalist andgeologist as he is, Mr . Muir, rather than Joaquin Miller, has been the real poet of theSierra, though he writes in prose . His books are after all not so much treatises on itsnatural history as delightful interpretations of its spirit . Yosemite Trails, 1911, by J.Smeaton Chase, is an enjoyable account of the Yosemite uplands, especially useful ontheir trees and flowers . Mr. Chase's little manual, Cone-Bearing Trees of the California

Mountains, 1911, will also be found of service.The standard handbook on the botany of the Park is A Yosemite Flora, 1912, by

Prof . Harvey M. Hall and Carlotta C . Hall . Untechnical in style and excellently illus-trated, with keys for identifying the trees and flowers, this accurate manual is invaluable

for field work . Prof . Willis Linn Jepson's The Trees

of California, 1909, is well planned for laymen's use,and capitally illustrated. It is not to be confusedwith his monumental and technical Silva of California,

published by the University of California . Supple-menting these popular handbooks, Sudworth's Forest

Trees of the Pacific Slope, 1908, published by the U . S.Forest Service, covers the Sierra forests with thesame thoroughness given to the rest of its subject.

The nine volumes of the Sierra Club Bulletin con-tain a store of papers by experts, covering not onlythe Yosemite country, but also the great mountainsof the Kings and Kern River basins . These admirablyedited publications, with a considerable library ofother mountain literature, may be consulted at theSierra Club's headquarters, the LeConte MemorialLodge, near Camp Curry . In the general periodicalsof this country and Europe, Yosemite and HetchHetchy Valleys have received more attention thanany other American scenic district, and many note-worthy articles may be found through the periodicalindexes and magazine files at the public libraries.

Hatching the Sunrise at MirrorLake.

Page 145: YOSEMITE AND ITS HIGH SIERRA BY JOHN H WILLIAMS

FROM YOSEMITE V :ILLEY TO WAWONA AND THE MARIPOSA GROVE.

1. Mt. Raymond (El. S .54S ft.).2. Signal Peak, or Devil Peal. (7,079),3. Wawona Point.4. Mariposa Grove.5. Wawona.6. Fish Hatchery.

Eight Mile.S . Eleven Mile.9. Chinquapin.

10. Grouse Creek.1Y . Fort Monroe.12. Inspiration Point,13. Artist Point.14. Old Inspiration Point.15. Stanford Point.16. Crocker Point.

PRESS OFTHE BLAIF-MUR DOCK COMPANY

SAN FRANCISCO

17. Dewey Point.1S . Cathedral Rocks.19. Cathedral Spires.20. Taft Point.21. Sentinel Rock.22. Sentinel Dome.23. Union Point.24. Glacier Point.25. Sentinel Hotel, Yosemite Village.26. Lost Arrow Camp.27. Three Brothers.2S. Camp Ahwahnee.29. El Capitan.30. Lookout Point,31. Ostrander Lake,32. Crescent Lake .

Page 146: YOSEMITE AND ITS HIGH SIERRA BY JOHN H WILLIAMS

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The following maps, at the prices given, may be obtained from the Director of the U. S . Geological Survey,Washington, D . C ., or at the office of the Superintendent of the Park in Yosemite Village:

Map of Yosemite National Park, 283 x 27 inches, scale z miles to the inch . Price, 5o cents a copy flat ; 55 centsa copy folded and bound between covers.

Map of Yosemite Valley, 35 x 15% inches, scale 2,000 feet to the inch. Price, 20 cents.Panoramic view of Yosemite National Park, 183/. x 18 inches, scale 3 miles to the inch . Price, 25 cents .

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Page 147: YOSEMITE AND ITS HIGH SIERRA BY JOHN H WILLIAMS

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Key to Outline Map of Yosemite Valley and Adjacent Peaks, with Elevations of Principal Landmarks.NOTE : The elevations given below are from the maps of the United States Geological Survey . These maps do not always agree one with another, and even in

the same map slight differences between the legend and bench-mark figures are sometimes found . Such variations, however, are inconsiderable,—never more than a fewfeet . Where they occur, the authority of the latest map, the " Panoramic View of the Yosemite National Park," has as far as possible been followed.

The figures indicate height above sea-level . For height above the floor of Yosemite Valley, deduct 3,960 feet, the elevation of the pier near the Sentinel Hotel.In the case of waterfalls, the height, or "drop," of each is given, as well as its elevation above sea-level.

1. Artist Point, 4,701 feet.2. Inspiration Point, 5,391.3. Old Inspiration Point, 6,603.

1. Stanford Point, 6,659.5. Crocker Point, 7,090.6. Dewey Point, 7,316.7. Bridal Veil Fall, top, 4,787 ; drop, 620.S. Cathedral Rocks, 6,638.9. Cathedral Spires, 6,114.

10. Taft Point, 7,503.11. The Fissures.12. Sentinel Rock, 7,046.13. Union Point, 6,314.14. Glacier Point, 7,214.15. Sentinel Dome, 8,117.16. Glacier Point Hotel.

17. Vernal Fall, top, 5,049 ; drop, 317.18. Panorama Cliff, 6,224.19. Illilouette Fall, top, 5,816 ; drop, 370.20. Nevada Fall, top, 5,910 ; drop, 594.21. Mt . Broderick, 6,705.22. Liberty Cap, 7,072.23. Little Yosemite, 6,150.24. Mt . Starr King, 9,181.25. Mt. Clark, 11,500.26. Foerster Peak, 12,062.27. Electra Peak, 12,462.28. Rodgers Peak, 13,006.29. Mt. Lyell, 13,090.30. Mt. McClure.31. Mt . Florence, 12,507.32. Half Dome, 8,852 .

33. Clouds Rest, 9,924.34. Parker Peak, 12,850.35. Gibbs Mountain, 12,700.36. Tenaya Peak, 10,200.37. Mt. Watkins, 8,235.38. Indian Rock, 8.526.39. Basket Dome, 7,602.40. Leaning Tower, 5,863.41. North Dome, 7,531.42. Washington Column, 5,912.43. Mirror Lake, 4,096.44. Camp Curry.45. Kennyville.46. Royal Arches, 5,500.47. Indian Camp.48. Camp Lost Arrow.

49. Camp Yosemite (Military).50. Yosemite Point, 6,935.51 . Yosemite Falls : Top of Upper Fall,

6,525 ; drop, 1,430 . Top of Lower Fall,4,420 ; drop, 320.

52. Lost Arrow.53. Three Brothers, 7,773 (Eagle Peak).54. El Capitan : Brow, 7,042 : summit, 7,564.55. Ribbon Fall, top, 7,008 ; drop, 1,612.56. Sentinel Hotel, Yosemite Village, 3,964.57. Camp Ahwahnee.58. Garage.59. Lake Tenaya, 8,146.60. Dana Mountain, 13,050 .

Page 148: YOSEMITE AND ITS HIGH SIERRA BY JOHN H WILLIAMS

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