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Tous les autres exemplaires originaux sont film^s en commen^ant par la premiere page qui comporte une empreinte d'impression ou d'iliustration et en terminant par la derniire page qui comporte une telle empreinte. Un des symboles suivants apparaTtra sur la dernidre image de cheque microfiche, selon le cas: le symbole — ► signifie "A SUIVRE ", le symbols V signifie "FIN". Les cartes, planches, tableaux, etc., peuvent dtre film^s d des taux de reduction diff Arents. Lorsque le document est trop grand pour dtre reproduit en un seul cliche, il est film* A partir de I'angle supdrieur gauche, de gauche d droite, et de haut en bas. en prenant le nombre d'images ndcessaire. Les diagrammes suivants illustrent la mdthode. 1 2 3 1 2 3 4 5 6 m^r^'-^'^"''^' ttyi THE NORTH FORK V/ LLEY OF THiE WAPTA (BRITISH COLUMBIA) By JEAN HABEL -%i '>.-£.! ''^'^A' w^mn^'v i^ ! c X . 4-1 . MiiMiiiiiiliiii^^ ?f-J^<,-^i'-^f- '^T, <^ i I i. The North Fork of the Wapta. By Jean Habbl. Read January 19, 1898, Travelling westward in the Rocky Mountains on the Canadian Pacific Railroad, and after having passed the Great Divide at Stephen (5296 feet) and the Wapta Lake at Hector (6190 feet), a wild valley is visible to the right, the ent -ice 328 THE NORTH FORK OF THE WAPTA. to which seems to be barred by precipitous, forest-clad moun- tain walls ; its upper terraces are covered by extensive ice-fields. This is the so-called North Fork Valley, — the stream emerging from the same being considered as the right fork of thb Wapta or Kicking Horse Kiver, although from a geographical point of view it seems rather to be one of the different affluents of the latter river, the source of which is formed by the Wapta Lake and a few creeks emptying into it. In the background of this hitherto untrodden valley a high, glacier-clad peak is visible from the railway, and to explore the region to a point as high as possible upon this peak was the purpose of the journey which these pages report. This object was attained only par- tially, the greatest drawback being that, once in the valley, the mountain was lost from sight, and the way leading to its ascent was discovered too late to be made use of. No other name being known to me, I have called the peak " Hidden Mountain." ^ After having passed the North Fork Valley, the station at Field (4050 feet) is soon reached, where the railway company manages a little hotel and tries to make the traveller as com- fortable as possible, — an endeavor which, during my stay, was not always seconded by the persons employed in the house. Making Field my starting point, I left the place on the morn- ing of July 15, 1897, accompanied by Fred Stephens, Ralph Edwards and the cook, Frank Wellman, all three on horseback. Our outfit was carried by four pack-horses, everything having been provided by Mr. T. E. Wilson of Banff, to my great satis- faction. Abstaining from taking a saddie-horse for myself, as the nature of the valley seemed too unfavorable for equestrian exercise, I made the whole trip on foot. After the first day the men had to walk nearly continuously as well. For crossing the rivers, however, one or two saddle-horses are necessary. As the entrance to the North Fork Valley could hardly be worse from the west, by way of Emerald Lake,^ than it appeared ^ This IS the peak mistakenly identified as " Mt. Balfour " in Plates VI. and VIII. of this volume of Appalachia. — Ed. 'if ^ > ^j, 9^ ,? V . . -'^ ' C- . 2 A visit to this lake and the Natural Bridge ; a walk to the western Ottertail bridge, affording a most beautiful view of the Ottertail Range and the mountains north of Emerald Lake, which fitly may be called Emerald Range ; and a walk to an eastern point, opposite the North Fork Valley, or to Hector are three excursions \ X m r- O ^ m zo O z •n O 3 2 3 » O ■0 -^ I H i I "5 m fi) 1 z o- O 3: 3 T3 I > ■D > r > n I < o L:;^a05j / r 1 J FK^ 'i^^yj, '• * . .*J .jC Aiisr, *.'•■•■■ _ •■ ■ _^^^_,_^^ .-yt,.,.,.. , i^^-gj-- ... II 1 ' ■ 1 1| '^^■■■■IMIHM ,.. v^^^^^^^^^^^^ ^^MHM&^k ' jWMH^H^^^ 'V-iyiB ^ ■ . 1 L ii.' 'v^^QGS^^^^^ ;f^**uA 1 L '4^v^P^^^^ *>JL'^JF ■■ ■ k ^m^tt-.-rii^B^^^^^k.' ik^'t^ > •^Jlwfe JSj .T-'-'* '^^^JHf^^ Hi -wlHjj^ ■ ~ * ^^P^<3t l^i. ^B ^v^t^W ■■^L..^..._ a: — ^" "" ^■ B^^^^r 'sBHlfll^P^^ j>^ 1 V' GLAC ibel. H^^'SEni' 1 jL fi^yf^..^^S9^^^^^^^^| < ^ mI Ski^^^^^^^I "4 -> I s ^- ? 4^^ U. o o i. O E ■ ^K^Kmf tM-^^p4^- Jr O 2 ■■ » ■i-'i^^-^v^ LU ^^^^■L A^ '^^^IB^ V/J: --»<*«'■.,• ». . I ll^B^ ^m ''^^^^1 '[^.■->±.~^' ■ r Tjiii V' H- ^^^^^^L '^Im^^^IP' ^^ -"■ ^^^H^^^^R/ ^^ J^^^^^Ki 'fBtr "'^^ef ^ *%& '( ^^^Bj^^^fg ' ''l9^H^^^B^^^^^ft^SK^i^I^3V^.^^Ki£^ ' ^ IjH^K^'^^V^^^^^^^^^^^^^^^^^^^^^^^I ^ > I^^^^K '^B@)p ' > ty ^^v ^K^flKKHP^^Bmk?fl^B^H|^^^^^^^Hn^|^^^^^^^^^^^^^^^^^^| J o > m "^ ' JMf^^p@^p^^^^^| < I (J < ^■^T m^^^h¥ ' r *i ^^^ ' 4 .^hIb^^^^^^^^^^^I _i ^^^K^' .^^^^^^^^^^^H t aqj t .'■■■ A- *i^mi9vi^^^^^^^^^^^^^^^i < ^^^^^K^ ^^^^^^^^^^^^^^^^^^Kt j^M^^ga^MU^^ri ^^^^^B^^^^^BII^B^^^^^^^^^^^^^^^^^^^I CL Q. ^^^^* ^^^^^^^^^^^I^K'C^^^^^^^^^^^H^nfjJ^^^^^^^^HBI^^^^^^^^^^^^^I < -^'^lIHMIi^' ■ - - " i r 1 THE NORTH FORK OF THE WAPTA, 320 O 3 - o a. LlJ I O E O .2 X I- to be from the south, I decided to attempt it first from that side. In one hour from Field the " Natural Bridge " is reached, where a bar of eambrian slate stretches from one side of the Wapta to the other, with an outflow for the stream in the centre, but easily traversed by homo Hapiens. The railway com- pany had a bridge built this year over the bar, and our horses were the first to cross it. From the Natural Bridge to the creek flowing from the lake, where another bridge would be con- venient, requires another hour, and then, after a third hour's walk from Field on a good trail, leading through a fine forest. Emerald Lake (about 4220 feet i) is reachetl. Our outfit was shipped on board the little craft stationed there, and rowed over by Fred to the northern shore, where we pitched our tents, the horses having been driven around the western side. The lake had a temperature of 55° F. ; the numerous little springs rising near its shore and emptying into it, of 42°. The next morning was a very damp one. To beguile the weary hours I made myself waterproof and entered the narrow valley, which opens to the northwest of the lake. Two hours' walk brought me over the debris of an avalanche to its upper end, a precipitous cirque, with high tilted strata to the west and a hanging glacier to the north, the right side of the latter de- scending in a narrow ribbon pretty far down. On my way back I met a porcupine on its way up, which passed within a yard of my feet. The morning of July 17 was also damp and cold (5 A. m. 38° F.) With Fred and Ralph I left the camp at eight o'clock to ascertain whether it would be possible to take our horses to a higher camp and find there the necessary feed for them. We traversed the little plain behind Emerald Lake to the northeast, crossed the creeks without difficulty, and moved up the iinwooded slopes of the Emerald Range, skirting its perpendicular walls. Coming into forest again, we tui*ned further north and found, after three hours' walk from our ivhich may be easily made and which will give great satisfaction to any visitor at Field. ^ This and the following heights have been determined by two aneroids, con- trolled by the boiling point of the water. The little sketch map, attached to the paper, has been compiled by aid of numerous bearings, taken on the road. It will no doubt be found incorrect and can ouly be considered as a finger-post for the reader. 330 THE NORTH FORK OF THE WAPTA. camp 1, a good camping ground with two or three days' feed for our horses and water about twenty minutes higher up. Ascend- ing the Emerald Range still fui ';her and turning to our right towards tlie North Fork Valley, we reached in one hour a point (7110 feet) from which a good part of the latter valley could be overlooked. We were here standing on the rim of the extensive hanging glaciers, which cover the northern Hanks of Emerald Range. In tlie background of North Fork Valley a so-called " valley glacier " was visible, descending into it in a fine ice-fall. The torrent from the hanging glaciers, which cover the eastern terraces of the valley, descended directly opposite to us in a very powerful waterfall. Rushing from imder the ice at about the height of our standpoint, this fall plunges over a nearly perpendicular wall down to the very level of the valley bottom in beauty and grandeur hardly to be excelled by any other on our globe. An entire view of the fall can only be got from a point like that at which we stood, and not from the lower parts of the valley. The difference between the height of our standpoint and the foot of the fall is over 2100 feet. From this figure much must be deducted as not of the fall proper, yet it seems no exaggeration to say that the fall is one of the highest in the world, although it certainly does not go down in so vertical a leap as the Yosemite Fall in California. The latter, the height of which is given at 2600 feet, has a first vertical descent of 1500 feet ; of the remainder, 600 feet are cascades, and then comes a final plunge of 400 feet. But it is fed by temporary snow-fields, and while in spring it carrier a large volume of water, it is greatly reduced in sumpier, after the snow has melted away. So, too, the fall which is sometimes quoted as the highest in Europe descends for over 1400 feet from the glaciers on the Pic du Marborc into the Cirque de Gavarnie, near the French village of the same name in the Dcpartement des Hautes Pyrenees ; but its volume is so slight that it reaches the bottom only in spray. The fall in the North Fork Valley, draining parts of the extensive glacier-fields on the western slope of the ridge stretching south from Mt. Bal- four, will always have a large supply of water. On the way back to camp I shot a very fine mountain « THE NORTH FORK OF THE WAPTA. :}:]i goat, which, after the fatal wound, following the peculiar habit of its race, went down over a precipice ; wo found it quite near to our intended camp 2. The meat of this very lusavy buck, which the united force of our six arms was unable to lift, proved later on to be very good indeed, in taste like beef. It enjiblud us to remain longer in the valley than we had iinticipated. As the weather was uncertain, I stopped another day at camp 1, and then, on the 19th, we achieved the difKcult task of get- ting the horses and outfit up to camp 2. The i nst diffiart of the Rockies is said to stretch far to the north, and in this direction perpendicular ridges of rock, several hundred feet in height, emerge froni the same. We turned to the western part of the basin, which perhaps sends down another valley glacier (292°), towards the so-called North Branch of the Kicking Horse River, and halted there at 1.15 p. M. (8840 feet), lunching, observing, photographing. Fine, 1 July 25, four p. M. Temperature of the air, 8° C. (46.4° F.). 334 THE NORTH FORK OF THE WAPTA. glacier-slad mountains stood near to us, two to the south (164° and 207°), one to the northwest (308|°), united to a rocky wall ; and to the east stretched the three peaks which border the left bunk of the Wapta Glacier, the highest (100°) more to the north, the eastern part of the great glacier basin descending between them into the main stream. To the southeast the chain of the Rockies south of the Kicking Horse River was visible : the Ottertail peaks of Mt. Goodsir (141|°-140°), Mt. Stephen (134°), Cathedral, Biddle, Hungabee, Huber, Victoria, and Lefroy, a most wonderful view, which reminded me of the Dolomites in the Alps. At 3.30 we retraced our steps, reach- ing camp at 6.45 p. m. The next day was spent in the environs of our camp, and on the 28th the eastern slope of the valley was ascended. A steep climb of an hour and a half brought us to a point (7170 ft.) where the whole western side of the North Fork Valley was visible, includingj Hidden Mountain. The ascent to the latter would perhaps be easily achieved through the side valley, the entrance of which we passed on our way to the glacier basin. This mountain and its glacier-clad neighbors is drained by the stream which forms the above-mentioned Twin Fall and the little picturesque fall we passed before camp 5. We had a very fine view of the former from here, and above it part of another fall formed by the same torrent was visible. To the south of tills " Waterfall Valley " the whole northern side of Emerald Range, Mt. Wapta, and the Mt. Stephen group were visible. To the east, not far from us, stood the perpendicular walls '^f Mt. Balfour and, separated from it by a small glacier, a characteristic mountain, to all appearance quite inaccessible from this side, resembling somewhat a well known mountain in the Norwegian valley of Romsdalen, and which I therefore called " Trolltinder." Ascending further east, we got in two hours to the highest point (9370 feet) of the ridge which here borders the southern part of the great glacier basin at the foot of Mt. Balfour. Tlie weather, in the morning cloudy and rainy, had cleared up, and we could even see, to the right of the Ottertails, something of the distant Selkirk Range. A descent of two hours brought us back to the camp. The evening was a most glorious one. At sunset Mt. Stephen appeared from fm6^ysy ^y,y/kPJ. Sketch Map op- rwE Valley o^ the morth fobk of th Wa,pta River B.C &y Jk>m4 HAa«L, I897 lost OP v SCAL* OP Mn.«S £'/9r^4P^?.-*'*i. A'f/^AT > > > o I < o ^^rr\. H Punchc«rd.Tra*vi«nt- 6ld'