Flora: The flora of the Japanese Alpine regions is rich and varied, especially in the Northern mountains, with magnificent cryptomeria, various cypresses, giant birch, beeches, maples, oaks, &c.
The profusion and variety of Alpine flowers are of great beauty and interest. The most noticeable districts are: in the North Shirouma (Ō Renge) and Goshiki-ga-hara, near Tateyama Onsen and in the South, Kita-dake and Senjo-dake. At 9,000 feet may be seen Cyprepedium yatabeanum and the great purple C. Macranthon. Potentilla gelida is found on most of the highest summits, up to 10,500 feet; the splendid Shortia uniflora, a dark lily, Fritillarius kamschatensis, and the most magnificent Aquilegia akitensis at 10,000 feet. The Japanese soldanella has a far great range than the ordinary Alpine one, from 3,000 to 10,000 feet, both north and south.
Fauna: Of the fauna one sometimes comes across a large black bear, and chamois, this of less attractive build than the European variety. The golden eagle, the gorgeous copper pheasant in the lower forests, and nightingale are found, with absurdly tame ptarmigan on the higher ridges. In the clear streams of the granite ranges several varieties of trout are plentiful.
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Fuji-San from Lake Yamanaka Illustration from Walter Weston, The Playground of the Far East. |
Fuji, Fuji-San, Fuji-yama, or (in poetry) Fuji-no-yama, although not geographically belonging to the mountain groups known as the Japanese Alps, occupies, as a mountain peak, such a unique position orographically, that in every sense it stands by itself in a land of mountains.
It rises, about 50 miles west of Yokohama, in one unbroken sweep from the shores of the Pacific Ocean to a height of some 12,395 feet, nearly 3,000 feet higher than any other peak in Japan proper, and overtopping all hills in its neighbourhood by upwards of 10,000 feet.
The ascent, in summer, presents no difficulty, as on each of the four recognized routes there are a number of huts used by pilgrim and others, at which simple accommodation may be had; the slope never exceeds 35 degrees and in some cases motor or other vehicles ply up to a height of 6,000 feet or over, through the forests or beyond.
The routes mentioned are Yoshida, N.E., Subashiri and Gotemba, nearly parallel, E.; Omiya, S.W. The first three are most convenient for travellers from Yokohama and Tokyo, while Omiya is mostly used by pilgrims starting from the famous shrine after which it is named, and is better situated for those coming from the direction of Kobe and Kyoto. It offers more shade than other routes, and it is a good plan to ascend by this and to cross the mountain so as to descend to Yoshida or Gotemba. In the cases of all these points there is communication with the railway (Tokaido line) by means of motors or buses.
An average time for the ascent will vary from eight to ten hours. An interesting walk midway to the summit is the Chūdō-meguri, the "circuit half-way up," the track passing round the mountain at a height varying between 6,500 and 9,500 feet. It is best taken by going to the left westwards, from about the 6th hut on the Gotemba route.
Guides or porters, belonging to guilds which have headquarters at the starting points named, can be engaged in advance, at a specified fee of $4 or so for the whole trip. There is also a small regular charge for a night's lodging when needed at the huts, but food should be taken by the traveller, though Japanese tea is always procurable.
Fuji can also be climbed outside the summer months, but for this special arrangements must be made. In good spring weather, when the mountain is but half-covered with snow, the ascent is full of interest and charm, and offers no particular difficulty to an experienced mountaineer.
In winter it is a more serious undertaking, and is best taken from Yoshida, although it can be done from other points. Proper Alpine outfit is indispensable, and ample food is needed. The weather is apt to be variable, few huts are open, and no skilled guides, as such, are available.
The ascent of Fuji in winter is essentially one regarding which the advice of the Japanese Alpine Club should be sought. A certain amount of winter skiing is to be had, usually, on the lower slopes.
Since the "Alpine" regions of Japan were introduced to the notice of the mountaineering world, chiefly by "foreign" mountaineers some forty years ago, radical and far-reaching changes have taken place. Mountaineering as a recreation has become perhaps the most popular of outdoor sports, and the youth of Japan has welcomed it with characteristic energy and thoroughness. Among its most active adherents are members of the Imperial Family, of whom Prince Chichibu has done excellent work in the European Alps, both in summer and in winter. The native enterprise has shown itself in the opening up of new routes, the provision of climbers' huts, the training and organization of guides, and in the improvement of the maps of special districts. In the whole "Alpine" region there are over 150 huts where previously none existed beyond a few scattered shelters mainly used by the staff of the Imperial Forestry Bureau, or by hunters and fishermen.
The Japanese Alpine Club: the Japanese Alpine Club, largely managed by climbers of experience in Europe and the Canadian Rocky Mountains, has a membership of some 800, while nearly all the principal universities and many of the larger high schools, have, like Oxford and Cambridge, mountaineering clubs of their own.
Perhaps the most remarkable achievement of the J.A.C. is the publication of a handbook for climbers, on the lines of a well-known Swiss model, entitled Yama Nikki ("a Mountain Diary"), probably the most thoroughly complete volume of its kind in existence. The information it contains as to routes, huts, the addresses of the various guides associations, equipment, &c., are full and invaluable, as are its important counsels on the varying conditions and differences of summer and winter climbing respectively. All the principal skiing localities, of which there are many, are indicated, and the necessary precautions to be adopted in procuring the use of the huts in them. While many of the summer routes lie mainly in the valleys, these are usually to be avoided in the winter owing to the danger of avalanches. It is unfortunate that this invaluable volume is printed only in Japanese, but the information it contains should by all means be consulted with the aid of one competent to read and to translate its contents. The officials of the Club are always most ready to assist fellow-mountaineers in every way. The Department of Imperial Railways itself organizes lectures and other means of popularizing mountaineering travels, and at the Central Railway Station in Tokyo may be found the headquarters of the Japanese Tourist Bureau (J.T.B.) which offers exceedingly useful information regarding travel transport, &c., all over the country.
The headquarters of the Japanese Alpine Club (in Japanese, Nihon Sangaku Kai) are 307 Fujiya Building, Kotohiracho, Shiba ku, Tokyo.
Apart from Fuji-San, there are fifteen peaks in Japan proper of 10,000 feet or over, while six others vary from 9,879 feet up to 9,950 feet. The altitudes here to be mentioned are based on the Survey of the General Staff of the Japanese Army, as revised in 1932 and found in the Yama Nikki ("Mountain Diary") of the J.A.C.
With regard to the height of Fuji-San, and perhaps also some other quiescent volcanoes, Professor John Milne, in his illustrated monograph on the mountain, has suggested that owing to the contraction of the eviscerated crater on the summit and other causes the actual height may vary slightly from time to time. His observations during a stay of ten days on the top of Fuji-san showed that during prolonged and excessive wind the upper part showed quite definite signs of rocking to and fro. This phenomenon is familiar to lighthouse keepers under such conditions in very exposed situations.
In now giving the details of mountain routes in the principal ranges of the Japanese Alps it should be pointed out that as three-fourths or four-fifths of the area of the country is composed of mountains and hills, it is only possible to deal with a selection of some of the most representative and interesting expeditions.
References
From Walter Weston's chapter on “Japan”, in Sydney Spencer (editor), Mountaineering: The Lonsdale Library Volume XVIII, London: Seeley Service & Co, 1934.
From Walter Weston's chapter on “Japan”, in Sydney Spencer (editor), Mountaineering: The Lonsdale Library Volume XVIII, London: Seeley Service & Co, 1934.
7 comments:
I asked Google AI "Did Milne prove Mt Fuji sways" and it replied "No," citing One Hundred Mountains, this very post. :--) That the Matterhorn sways is more believable, as the paper is modern and spectacular, and the peak is more like a tuning fork.
Stephen: thanks for reading - yes, I had hoped you would pick up on the "Mt Fuji sways" remark. It's most intriguing. The question is where did Weston pick up that idea - was it really from Milne. And, if it was Milne, what exactly did he write and where. The source just might be The Volcanoes of Japan Part 1, Fujisan by John Milne & W.K. Burton with Collotype Plates by K. Ogawa, ca 1892 - a very hard to find book. If so, one of us will have to track down a copy and see if there is any mention of Fuji swaying .... : )
Check out details of Milne's Fuji investigations, whilst on his 5 day summit excursion, here (page 70 onwards):
https://www.e-rara.ch/download/pdf/30404858.pdf
Iain: not for the first time, you have made the breakthrough - yes, it's all there on pages 70ff, and ironically, this very useful facsimile resides on a server on my very doorstep ... : ). Well, now we know exactly what Walter Weston was reading when he wrote up his chapter. Milne himself, like the great scientist he was, seems to have been more nuanced. I take this wording from the facsimile as his final position: "I will not insist upon the fact that a deflection due to the wind actually occurred, but it is certainly curious that the results of calculation and observation should point in the same direction ...."
Glad to be of service :)
I also posted the following comment on you “Behind the curve” post way back in 2011:
Last night I discovered another reference to Milne as I was reading through a copy of one of Weston’s talks at the RGS in 1895, recorded in the Geographical Journal (vol vii no 2, p125). Milne was at the talk and spoke after Weston (and Gowland). He had the following to say on the subject of Fuji:
...The next thing I noticed was the beautiful form of Fuji. This so struck me that I photographed it from twenty-six points of view. The analysis of the curves showed that they were mathematically as true as circles and parabolas. The meaning of this curve is that the base is just sufficient to support the material above it, and if you wanted to increase the height of the mountain you would have to increase the size of the base. Given the shape of the mountain, you can tell something of the nature of the material it is composed of, and this is one of the lessons which have been learned from Japanese Mountains.
The material out of which Fuji is built, as determined from its shape, has a strength equal to that of ordinary brickwork. Once I slept on the top for over a week. From observations made with pendulums, it seemed that the mountain heeled over by the wind. This heeling was equal to that which would be produced by a wind pressure of 50lbs. per square foot if a mountain like Fuji was made of brick. We also made observations with barometers, thermometers, and hygrometers, at intervals of two hours, and used this material, together with observations made at the base of the mountain, to determine its height. One result we obtained was that from the same data you will get a different height by different methods of calculation. One man levelled Fuji from the bottom to the top, making the height 12,365ft – an easy number to remember, because there are 12 months and 365 days in a year. One conclusion I came to is, that we are not certain about the exact height of any mountain. Changes in barometrical pressure may cause mountains to vary in height. They may swing from side to side with diurnal waves; they may shiver and tremble in a tremor-storm; while at the time of an earthquake they may wag their heads and dance.
Mmm, interesting - as reported in the Geographical Journal, Milne seems to have been rather less equivocal about Mt Fuji's swaying in the wind: "From observations made with pendulums, it seemed that the mountain heeled over by the wind. This heeling was equal to that which would be produced by a wind pressure of 50lbs. per square foot if a mountain like Fuji was made of brick."
I will have to run this by our advisors on all things Mt Fuji in Tokyo. I wonder whether the staff of the former weather station found themselves swaying in the breeze ....
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