CHAPTER XIX

THE ROCKY MOUNTAINS

BY A. L. MUMM

[Sidenote: General Topography.]

The Rocky Mountains form the backbone of the North-American Continent, and the Canadian Rockies extend from the United States frontier in a north-westerly direction for some hundreds of miles. Of the regions which are of interest to mountaineers, the northern limit is marked by Mount Sir Alexander, a peak which rises a few miles to the west of the continental divide or watershed, a little over 400 miles, as the crow flies (_very_ roughly speaking), from the frontier, and from 60 to 80 miles beyond Mount Robson. The country situated between these two mountains is full of interest for explorers and climbers, but is at present very imperfectly known and mapped. From Mount Robson southward we possess mountaineering knowledge which is extensive, but not quite continuous and far from complete, as far as Mount Assiniboine, a distance in a direct line of about 200 miles (another rough estimate). Till quite recently nothing of alpine or mountaineering interest was known to exist in the main chain of the Canadian Rockies south of Mount Assiniboine, but, in the course of an official survey of the watershed between Kicking Horse Pass and the frontier (1913-16), no less than four groups of mountains, clad in snow fields and glaciers, and containing three peaks of over 11,000 feet, were discovered. No climbing has as yet been attempted on any of them. They extend for about 40 miles beyond the Assiniboine group.[36]

The continental watershed pursues a very tortuous and irregular course, and is probably at least half as long again as the ‘air-line’ length of the range. East of the watershed the mountain region extends for a comparatively short distance and ends with remarkable abruptness. Through much of its length there is a succession of minor groups and ranges situated close to the main chain, but separated from it by the upper valleys of the great rivers, which show a striking tendency to run parallel to it. These possess some extensive snow fields and considerable glaciers, and will probably receive attention from climbers in the near future, but very little is known of them at present. Beyond them is a belt of mountains, not attaining to the snow-level but often rocky and bold in outline, which reaches to the edge of the great central plain, and presents to the traveller approaching it by the railway the appearance of a solid impenetrable wall. There are no snow fields or glaciers in this outer belt so far as I am aware. (It may be as well to say here once for all that this qualification is often unavoidable in dealing with an area so extensive and little known as the mountain region of Canada; it is impossible to give any information at all without putting forward as probable statements which may turn out to be erroneous.) To the west of the watershed, on the other hand, the country is continuously mountainous all the way to the Pacific Coast, three hundred miles away, and there are several ranges, alpine in size and character, standing quite apart from and independent of the main chain. Of these the Selkirks, an immense mountain system, enclosed by the great loops of the Columbia and Kootenay Rivers, are by far the largest and most important.

The outstanding feature of all this region is that till quite modern times it was entirely uninhabited, and for the most part still remains so. Indians in old days came up into the mountains to hunt, and to some extent for purposes of trade, but they did not live among them. Two or three outposts of the Hudson Bay Company, long since abandoned, were the only permanent human habitations. This differentiates mountain travel in Canada in many ways--as soon as the immediate neighbourhood of the railway is left--from mountain travel in the Caucasus or the Himalaya, particularly with respect to food supplies, roads and methods of transport. In the high mountain region the railways have had little or no effect on the character of the country, except within a few miles of the line.

The Rockies are now accessible by two lines of railway. Of these the Grand Trunk Pacific was completed early in 1914. It enters the mountains by the valley of the Athabasca River, and at the point where it leaves the Athabasca to ascend to the Yellowhead Pass (17 miles away) stands Jasper, destined to become a tourist centre, to which we shall return later. The other line, the Canadian Pacific, which has been in existence more than thirty years, crosses the main chain at the Kicking Horse Pass, and then, after descending into the deep trench of the Columbia River, passes through the very heart of the Selkirk Range. Climbing has now been carried on continuously and systematically for nearly thirty years among the mountains adjacent to this railway both in the main chain and in the Selkirks. It will be convenient to deal at once with the region here indicated, which will be referred to as the C.P.R. district. It is the only region where at the present moment conditions prevail at all resembling those of the European Alps, and climbing within its limits is quite a different affair from climbing elsewhere in Canada.

A climber wishing to see something of the mountains of Canada, who has not ample time at his disposal after arriving among them--I should be inclined to say _at the very least_ a month--would be well advised to confine himself to the C.P.R. district, making, perhaps, one short trip of the kind mentioned below. He would find enough, and more than enough, to occupy him.

[Sidenote: The ‘C.P.R.’ District.]

Taking the main chain first, the extent of the C.P.R. district may be taken to be the area dealt with in _Baedeker’s Canada_ (1907), which contains about ten pages packed with accurate and highly condensed information. The alpine particulars given are mainly based on chapters i. to ix. of _In the Heart of the Canadian Rockies_, by the Rev. Sir James Outram, who has been over almost the whole district and has supplemented his own experiences by copious extracts from the original narratives of Dr. Collie, Mr. Wilcox, and the members of the Appalachian Mountain Club.[37]

The railway enters the mountains from the east by the valley of the Bow River, the principal constituent of the _South_ Saskatchewan, and soon afterwards arrives at Banff. The excellent C.P.R. Banff Springs Hotel is the most frequented place in the Rockies; but Banff itself is not a mountaineering centre, though Dr. Collie discovered a good rock climb in the neighbourhood on Mount Edith, and doubtless others might be found.[38] It is, however, of interest to climbers as the site of the Club House of the Alpine Club of Canada (of which more anon), and as the starting-point for Mount Assiniboine. This peak is the highest to the south of the railway, and its ascent is a very fine expedition. Given favourable conditions it can be reached and climbed, and the return journey to Banff completed, within six days. This involves travelling with a camp outfit and pack-horses; but it would be well worth while for a climber visiting Canada for the first time to make one such trip (and this one is probably the most repaying), for, besides being pleasant and interesting in itself, it would give him much useful experience in case he contemplated returning another year, and making a more extended journey off the beaten track.

Soon after leaving Banff, the valley of the Bow River runs parallel with the main chain, passing Storm Mountain and Mount Ball, which can be reached via the Vermilion Pass in two days from Banff.[39]

Thirty-five miles beyond Banff is Laggan, where the railway leaves the Bow River, and ascends by Bath Creek to the Kicking Horse Pass. Laggan[40] is the station for Lake Louise, where there is another first-class C.P.R. hotel (3 miles from the railway), the principal centre for the mountains on the south side of the line. Several of these can be climbed from the hotel itself; and there may be a permanent summer camp for the use of climbers in the valley of the Ten Peaks. If not, it is easy to have a tent, provisions, etc., sent there from the hotel.[41] A similar arrangement could be made either at Lake Louise or Field for a camp at Lake O’Hara, and this would bring within easy reach all the other peaks which deserve attention, except those of the Ottertail Range.

The last-mentioned group is best attacked from Field, 16 miles beyond Laggan and 8 miles to the west of the Kicking Horse Pass, where there is another C.P.R. hotel, the Mount Stephen House, the best centre for visiting the mountains on the north side of the railway. Besides the hotel at Field there are a chalet hotel on Emerald Lake and two permanent summer camps, one at the Takakkaw Falls; the other, Camp Warren, I have not been able to locate. It is, of course, also possible to approach the mountains of the Waputik Range by making a short trip up the Bow River, but the Yoho and Emerald Valleys seem to be more attractive. From the climber’s point of view these mountains are distinctly inferior in interest to those on the south side of the line, and the same may be said of Mount Hector, the highest summit between the Bow and Pipestone Valleys. East of the Pipestone the mountains of the Ptarmigan Lake district, just opposite Laggan, should be worth a visit.[42]

The best general map that I can discover of this part of the C.P.R. district is the southern sheet of a map of “The Rocky Mountains between lat. 51° and lat. 53°,” published by the Department of the Interior. Unfortunately, it comes to an end four or five miles short of Mount Assiniboine. The part of it which is material for present purposes is given in a pamphlet issued by the C.P.R. Company, entitled _The Challenge of the Mountains_. The scale is 4 miles to an inch. The large-scale maps accompanying the Report mentioned on p. 572 show the mountains actually forming the watershed (and this includes the Assiniboine group) southward from Vulture Col and Mount Gordon in the Waputik Range.

Coming now to the Selkirks, Glacier House (about 90 miles by rail beyond Field and 3 miles beyond Rogers

Pass, where the line crosses the crest of the range), is probably the best of the centres of the C.P.R. district, in so far that the largest number of expeditions can be carried out from the hotel itself, or with only one night out. In this respect Glacier House has very few rivals even in Switzerland. _Baedeker_ gives a short summary of these expeditions and an excellent little map of the mountains, which literally surround the hotel.

[Sidenote: The Selkirks.]

But much more than _Baedeker_ is available. Besides Mr. Palmer’s exhaustive book (of which more presently), no visitor to the Selkirks should omit to secure a copy of Mr. A. O. Wheeler’s _Selkirk Range_ and the accompanying map in four large sheets, which covers a large portion of the range on a scale of practically 1 mile to an inch. The topographical information secured by Mr. Wheeler during his survey is embodied in the form of a Climbers’ Guide in chapter ii. of _The Selkirk Mountains, a Guide for Mountain Pilgrims and Climbers_, where very full particulars are given as to the number of days and nights required for each expedition, whether pack-horses are available, etc. Huts or cabins are mentioned at Rogers Pass and the Caves of Cheops. There seem to be no huts or summer camps south of the railway, and it must be borne in mind that pack-horses cannot be taken southward into the mountains direct from Glacier House.[43]

The limits in the Selkirks of the C.P.R. district can be easily grasped by examining together the map in _Baedeker_ and that in the Climbers’ Guide (difficult to read, but useful as showing at a glance the area comprised in Mr. Wheeler’s large maps). It will be seen at once that the latter covers a wider area, and in particular has a large extension to the west and south-west, reaching even beyond the Columbia River to the Gold Range--a quite independent group. This extension seems to come well within the C.P.R. district: one or two of the expeditions in it can be taken from Glacier House; the remainder are treated in chapter vi. of the Guide in connection with Revelstoke, which accordingly must be added to the list of C.P.R. centres. Since the publication of the Guide fine climbing has been accomplished on Mount Moloch and other peaks reached by the north branch of the Illecillewaet River.[44] The extension of Mr. Wheeler’s map to the north is unimportant; the notices in the Guide of Mountain Creek and Mount Pearce are not encouraging, and, so far as Glacier House is concerned, the crest of the Hermit Range forms the limit of ordinary mountaineering in this direction. To the south, on the other hand, both maps extend to regions which can only be reached by a journey of some days, and several of the expeditions described in the Guide clearly lie outside the category now under consideration. No hard-and-fast line can be drawn, and the traveller must use his own judgment; only, if he is at all tied as to time, let him bear in mind that estimates of a journey’s length by little-trodden trails are necessarily very rough, and that what is called a week’s trip may easily turn out to require two or three days less _or more_.

[Sidenote: Guides and Equipment.]

Swiss guides, to the number of six or eight, are imported every summer by the C.P.R. Company, and endeavours are being made to induce some of them to settle permanently at Edelweiss, near Golden, on the Columbia. They are distributed during the season among the four or five centres which have been mentioned. Anyone desiring their services, the charge for which is (or used to be) $5 per day, should communicate as early as possible with the hotel from which he intends to climb. A mountaineer arriving in the C.P.R. district with his ordinary Swiss outfit could thus enjoy plenty of climbing without any special preparations. Even ropes and ice-axes are supplied at Glacier House, and, probably, at the other centres also. The Hudson Bay Company’s excellent blankets can be procured at Banff, and for a single odd night out bedding could probably be borrowed.

There is also plenty of scope for guideless climbing. Some of the expeditions are undoubtedly difficult, and only suitable for an exceptionally strong unguided party; but three reasonably experienced amateurs could accomplish a great deal. As compared with the main chain, the Selkirks offer more snow and ice work and less rock work, and there seem to be more climbs of only moderate difficulty than in the Rockies on the south side of the railway. (For a general comparison of the Selkirks with the Rockies, see Palmer, op. cit. pp. 3-10.)

[Sidenote: The Northern Selkirks.]

Turning now to remoter and less known ground in the Selkirks, to the north of the railway, beyond the Hermit and Clach na Cooden Ranges, a very considerable mountain area is enclosed in the Great Bend of the Columbia River. Pack-horses cannot be used in it effectively, and the conditions of travel are exceptional and extremely difficult; but a large part of it, probably the most interesting part, was explored with extraordinary perseverance by Mr. Howard Palmer’s party from 1908 to 1912. Only in the latter year, on their fifth visit, did they succeed in attaining the summit of Mount Sir Sandford, the monarch of the region. For further information the reader is referred to part iii. of Mr. Palmer’s _Mountaineering and Exploration in the Selkirks_. Part ii. of this fascinating book is equally valuable as a guide to the mountains immediately south of Glacier House, which have already been noticed. Beyond these a still more extensive region remains to be dealt with.

It will have been noticed that Mr. Wheeler’s map, breaking off abruptly along most of its southern margin in the very middle of untrodden snow fields, is itself a challenge to further exploration. His work has been carried a short distance further by the ascents of Mount Beaver and Mount Duncan, and some climbs in the Battle Range, but the regions beyond are still, so far as I am aware, a _terra incognita_, and I am quite unable to say how much further the southern portion of the Selkirks proper continues its alpine character.

[Sidenote: The Purcell Range.]

Between this southern portion and the main chain of the Rockies is another large mountainous tract forming part of the Selkirks system and known as the Purcell Range, comprising the Dogtooth, Spillimacheen and South Purcell Ranges. A rough idea of its extent and situation may be obtained from the sketch map accompanying Dr. Longstaff’s paper in the _Canadian Alpine Journal_,[45] bearing in mind that Mounts Beaver and Duncan rise close to the watershed between the two rivers which also bear those names.

The Dogtooth Range appears to be sub-alpine, and is disposed of in