CHAPTER XV.

LOST ON THE COL D’HÉRENS—MY SEVENTH ATTEMPT TO ASCEND THE MATTERHORN

We should have started for Zermatt about 7 A.M. on the 18th, had not

Biener asked to be allowed to go to mass at Evolène, a village about

two and a half hours from Abricolla. He received permission, on the

condition that he returned not later than mid-day, but he did not come

back until 2.30 P.M. and we thereby got into a pretty little mess.

The pass which we were about to traverse to Zermatt—the Col d’Hérens—is

one of the few glacier-passes in this district which have been known

almost from time immemorial. It is frequently crossed in the summer

season, and is a very easy route, notwithstanding that the summit of

the pass is 11,417 feet above the level of the sea.

From Abricolla to the summit the way lies chiefly over the flat Glacier

de Ferpècle. The walk is of the most straightforward kind. The glacier

rises in gentle undulations, its crevasses are small and easily

avoided, and all you have to do, after once getting upon the ice, is to

proceed due south in the most direct manner possible. If you do so, in

two hours you should be upon the summit of the pass.

We tied ourselves in line, of course, when we entered upon the glacier,

and placed Biener to lead, as he had frequently crossed the pass,

supposing that his local knowledge might save us some time upon the

other side. We had proceeded, I suppose, about halfway up, when a

little thin cloud dropped down upon us from above, but it was so light,

so gauzy, that we did not for a moment suppose that it would become

embarrassing, and hence I neglected to note at the proper moment the

course which we should steer—that is to say, to observe our precise

situation in regard to the summit of the pass.

For some little time Biener progressed steadily, making a tolerably

straight track, but at length he wavered, and deviated sometimes to the

right and sometimes to the left. Croz rushed forward directly he saw

this, and, taking the poor young man by his shoulders, gave him a good

shaking, told him that he was an imbecile, to untie himself at once,

and go to the rear. Biener looked half frightened, and obeyed without a

murmur. Croz led off briskly, and made a good straight track for a few

minutes, but then, it seemed to me, began to move steadily round to the

left. I looked back, but the mist was now too thick to see our traces,

and so we continued to follow our leader. At last the others (who were

behind, and in a better position to judge) thought the same as I did,

and we pulled up Croz to deliver our opinion. He took our criticism in

good part, but when Biener opened his mouth, that was too much for him

to stand, and he told the young man again, “You are imbecile: I bet you

twenty francs to one that _my_ track is better than _yours;_ twenty

francs, now then, imbecile!”

Almer went to the front. He commenced by returning in the track for a

hundred yards or so, and then started off at a tangent from Croz’s

curve. We kept this course for half an hour, and then were certain that

we were not on the right route, because the snow became decidedly

steep. We bore away more and more to the right to avoid this steep

bank, but at last I rebelled, as we had for some time been going almost

south-west, which was altogether the wrong direction. After a long

discussion we returned some distance in our track, and then steered a

little east of south, but we continually met steep snow-slopes, and to

avoid them went right or left as the case might require.

We were greatly puzzled, and could not in the least tell whether we

were too near the Dent Blanche or too close to the Tête Blanche. The

mists had thickened, and were now as dense as a moderate London fog.

There were no rocks or echoes to direct us, and the guidance of the

compass brought us invariably against these steep snow-banks. The men

were fairly beaten: they had all had a try, or more than one, and at

last gave it up as a bad job, and asked what was to be done. It was

7.30 P.M. and only an hour of daylight was left. We were beginning to

feel used up, for we had wandered about at tiptop speed for the last

three hours and a half; so I said, “This is my advice: let us turn in

our track, and go back as hard as ever we can, not quitting the track

for an instant.” They were well content, but just as we were starting

off the clouds lifted a little, and we thought we saw the col. It was

then to our right, and we went at it with a dash, but before we had

gone a hundred paces down came the mist again. We kept on nevertheless

for twenty minutes, and then, as darkness was perceptibly coming on,

and the snow was yet rising in front, we turned back, and by running

down the entire distance managed to get clear of the Ferpècle glacier

just as it became pitch-dark. We arrived at our cheerless châlet in due

course, and went to bed supper-less, for our food was gone —all very

sulky, not to say savage, agreeing in nothing except in bullying

Biener.

At 7 A.M. on the 19th we set out, for the third time, for the Col

d’Hérens. It was a fine day, and we gradually recovered our tempers as

we saw the follies which had been committed on the previous evening.

Biener’s wavering track was not so bad, but Croz had swerved from the

right route from the first, and had traced a complete semicircle, so

that when we stopped him we were facing Abricolla, whence we had

started. Almer had commenced with great discretion, but he kept on too

long, and crossed the proper route. When I stopped them (because we

were going south-west) we were a long way up the Tête Blanche! Our last

attempt was in the right direction: we were actually upon the summit of

the pass, and in another ten yards we should have commenced to go down

hill! It is needless to point out that if the compass had been looked

to at the proper moment—that is, immediately the mist came down—we

should have avoided all our troubles. It was of little use afterward,

except to tell us when we were going _wrong._

We arrived at Zermatt in six and a half hours’ walking from Abricolla,

and Seiler’s hospitable reception set us all right again. On the 20th

we crossed the Théodule pass, and diverged from its summit up the

Theodulhorn (11,391) to examine a route which I suggested for the

ascent of the Matterhorn; but before continuing an account of our

proceedings, I must stop for a minute to explain why this new route was

proposed, in place of that up the south-western ridge.

The Matterhorn may be divided into three sections—the first facing the

Z’Muttgletscher, which looks, and is, completely unassailable; the

second facing the east, which seems inaccessibility itself; the third

facing Breuil, which does not look entirely hopeless. It was from this

last direction that all my previous attempts were made. It was by the

southwestern ridge, it will be remembered, that not only I, but Mr.

Hawkins, Professor Tyndall and the chasseurs of Val Tournanche, essayed

to climb the mountain. Why, then, abandon a route which had been shown

to be feasible up to a certain point?

[Illustration: THE MATTERHORN FROM THE RIFFELBERG]

I gave it up for four reasons: 1. On account of my growing

disinclination for arêtes, and preference for snow and rock faces. 2.

Because I was persuaded that meteorological disturbances (by which we

had been baffled several times) might be expected to occur again and

again. 3. Because I found that the east face was a gross imposition: it

looked not far from perpendicular, while its angle was, in fact,

scarcely more than 40°. 4. Because I observed for myself that the

strata of the mountain dipped to the west-south-west. It is not

necessary to say anything more than has been already said upon the

first two of these four points, but upon the latter two a few words are

indispensable. Let us consider, first, why most persons receive such an

exaggerated impression of the steepness of the eastern face.

When one looks at the Matterhorn from Zermatt, the mountain is regarded

(nearly) from the north-east. The face that fronts the east is

consequently neither seen in profile nor in full front, but almost

halfway between the two: it looks, therefore, more steep than it really

is. The majority of those who visit Zermatt go up to the Riffelberg or

to the Görnergrat, and from these places the mountain naturally looks

still more precipitous, because its eastern face (which is almost all

that is seen of it) is viewed more directly in front. From the Riffel

hotel the slope seems to be set at an angle of seventy degrees. If the

tourist continues to go southward, and crosses the Théodule pass, he

gets, at one point, immediately in front of the eastern face, which

then seems to be absolutely perpendicular. Comparatively few persons

correct the erroneous impressions they receive in these quarters by

studying the face in profile, and most go away with a very incorrect

and exaggerated idea of the precipitousness of this side of the

mountain, because they have considered the question from one point of

view alone. Several years passed away before I shook myself clear of my

early and false impressions regarding the steepness of this side of the

Matterhorn. First of all, I noticed that there were places on this

eastern face where snow remained permanently all the year round. I do

not speak of snow in gullies, but of the considerable slopes which are

seen in the accompanying engraving about halfway up the face. Such beds

as these could not continue to remain throughout the summer unless the

snow had been able to accumulate in the winter in large masses; and

snow cannot accumulate and remain in large masses, in a situation such

as this, at angles much exceeding 45°.[49] Hence I was bound to

conclude that the eastern face was many degrees removed from

perpendicularity; and to be sure on this point, I went to the slopes

between the Z’Muttgletscher and the Matterhorngletscher, above the

châlets of Staffel, whence the face could be seen in profile. Its

appearance from this direction would be amazing to one who had seen it

only from the east. It looks so totally different from the apparently

sheer and perfectly unclimbable cliff one sees from the Riffelberg that

it is hard to believe the two slopes are one and the same thing. Its

angle scarcely exceeds 40°.

[49] I prefer to be on the safe side. My impression is that snow

cannot accumulate in large masses _at_ 45°.

A great step was made when this was learned. This knowledge alone would

not, however, have caused me to try an ascent by the eastern face

instead of by the south-west ridge. Forty degrees may not seem a

formidable inclination to the reader, nor is it for only a small cliff.

But it is very unusual to find so steep a gradient maintained

continuously as the general angle of a great mountain-slope, and very

few instances can be quoted from the High Alps of such an angle being

preserved over a rise of three thousand feet.

1 do not think that the steepness or the height of this cliff would

have deterred climbers from attempting to ascend it, if it had not, in

addition, looked so repulsively smooth. Men despaired of finding

anything to grasp. Now, some of the difficulties of the south-west

ridge came from the smoothness of the rocks, although that ridge, even

from a distance, seemed to be well broken up. How much greater, then,

might not have been the difficulty of climbing a face which looked

smooth and unbroken close at hand?

A more serious hindrance to mounting the south-west ridge is found in

the dip of its rocks to the west-south-west. The great mass of the

Matterhorn, it is now well ascertained, is composed of regularly

stratified rocks, which rise toward the east. It has been mentioned in

the text, more than once, that the rocks on some portions of the ridge

leading from the Col du Lion to the summit dip outward, and that

fractured edges overhang. This is shown very clearly in the annexed

diagram, Fig. 1. It will be readily understood that such an arrangement

is not favorable for climbers, and that the degree of facility with

which rocks can be ascended that are so disposed must depend very much

upon the frequency or paucity of fissures and joints. The rocks of the

south-west ridge are sufficiently provided with cracks, but if it were

otherwise, their texture and arrangement would render them

unassailable.[50]

[50] Weathered granite is an admirable rock to climb; its gritty

texture giving excellent hold to the nails in one’s boots. But upon

such metamorphic schists as compose the mass of the great peak of the

Matterhorn, the texture of the rock itself is of no value.

[Illustration: Fig. 1.]

It is not possible to go a single time upon the rocks of the south-west

ridge, from the Col du Lion to the foot of the Great Tower, without

observing the prevalence of their outward dip, and that their fractured

edges have a tendency to overhang; nor can one fail to notice that it

is upon this account the débris which is rent off by frost does not

remain _in situ_, but pours down in showers over the surrounding

cliffs. Each day’s work, so to speak, is cleared away—the ridge is

swept clean: there is scarcely anything seen but firm rock.[51]

[51] I refer here only to that portion of the ridge which is between

the Col du Lion and the Great Tower. The remarks would not apply to

the rocks higher up (see p. 118); higher still the rocks are firm

again; yet higher (upon the “Shoulder”) they are much disintegrated;

and then, upon the final peak, they are again firm.

The fact that the mountain is composed of a series of stratified beds

was pointed out long ago. De Saussure remarked it, and recorded

explicitly in his _Travels_ (§ 2243) that they “rose to the north-east

at an angle of about forty-five degrees.” Forbes noticed it also, but

gave it as his opinion that the beds were “less inclined, or nearly

horizontal.” He added, “De Saussure is no doubt correct.” The truth, I

think, lies between the two.

I was acquainted with both of the above-quoted passages, but did not

turn the knowledge to any practical account until I re-observed the

same fact for myself. It was not until after my repulse in 1863 that I

referred the peculiar difficulties of the south-west ridge to the dip

of the strata, but when once persuaded that structure and not texture

was the real impediment, it was reasonable to infer that the opposite

side—that is to say, the eastern face—might be comparatively easy; in

brief, that an arrangement should be found like Fig. 2, instead of like

Fig. 1. This trivial deduction was the key to the ascent of the

Matterhorn.

[Illustration: Fig. 2.]

The point was, Did the strata continue with a similar dip throughout

the mountain? If they did, then this great eastern face, instead of

being hopelessly impracticable, should be quite the reverse. In fact,

it should be a great natural staircase, with steps inclining inward;

and if it were so, its smooth aspect might be of no account, for the

smallest steps, inclined in this fashion, would afford good footing.

They did so, so far as one could judge from a distance. When snow fell

in the summer-time, it brought out long terraced lines upon the

mountain, rudely parallel to each other; and the eastern face on those

occasions was often whitened almost completely over; while the other

sides, with the exception of the powdered terraces, remained black, for

the snow could not rest upon them.

The very outline of the mountain, too, confirmed the conjecture that

its structure would assist an ascent on the eastern face, although it

opposed one on all other sides. Look at any photograph of the peak from

the north-east, and you will see that upon the right-hand side (that

facing the Z’Muttgletscher) there is an incessant repetition of

overhanging cliffs and of slopes, all trending downward; in short, that

the character of the whole of that side is similar to Fig. 1; and that

upon the left hand (or south-east) ridge the forms, so far as they go,

are suggestive of the structure shown by Fig. 2, above. There is no

doubt that the contours of the mountain, seen from this direction, have

been largely influenced by the direction of its beds.

It was not therefore from a freak that I invited Mr. Reilly to join in

an attack upon the eastern face, but from a gradually-acquired

conviction that it would prove to give the easiest path to the summit;

and if we had not been obliged to part the mountain would doubtless

have been ascended in 1864.

My guides readily admitted that they had been greatly deceived as to

the steepness of the eastern face, when they were halted to look at it

in profile as we came down the Z’Muttgletscher on our way to Zermatt,

but they were far from being satisfied that it would turn out to be

easy to climb, and Almer and Biener expressed themselves decidedly

averse to making an attempt upon it. I gave way temporarily before

their evident reluctance, and we made the ascent of the Théodulhorn to

examine an alternative route, which I expected would commend itself to

them in preference to the other, as a great part of it led over snow.

There is an immense gully in the Matterhorn which leads up from the

Glacier du Mont Cervin to a point high up on the south-eastern ridge. I

proposed to ascend this to its head, and to cross over the south-east

ridge on to the eastern face. This would have brought us on a level

with the bottom of the great snow-slope shown upon the centre of the

eastern face in the engraving. This snow-slope was to be crossed

diagonally, with the view of arriving at the snow upon the north-east

ridge, which is shown upon the same engraving about half an inch from

the summit. The remainder of the ascent was to be made by the broken

rocks, mixed with snow, upon the north side of the mountain. Croz

caught the idea immediately, and thought the plan feasible: details

were settled, and we descended to Breuil. Luc Meynet the hunchback was

summoned, and expressed himself delighted to resume his old vocation of

tent-bearer; and Favre’s kitchen was soon in commotion preparing three

days’ rations, for I intended to take that amount of time over the

affair—to sleep on the first night upon the rocks at the top of the

gully, to make a push for the summit, and to return to the tent on the

second day; and upon the third to come back to Breuil.

We started at 5.45 A.M. on June 21, and followed the route of the

Breuiljoch for three hours. We were then in full view of our gully, and

turned off at right angles for it. The closer we approached the more

favorable did it look. There was a good deal of snow in it, which was

evidently at a small angle, and it seemed as if one-third of the

ascent, at least, would be a very simple matter. Some suspicious marks

in the snow at its base suggested that it was not free from falling

stones, and as a measure of precaution we turned off on one side,

worked up under cover of the cliffs, and waited to see if anything

should descend. Nothing fell, so we proceeded up its right or northern

side, sometimes cutting steps up the snow, and sometimes mounting by

the rocks. Shortly before 10 A.M. we arrived at a convenient place for

a halt, and stopped to rest upon some rocks close to the snow which

commanded an excellent view of the gully.

While the men were unpacking the food I went to a little promontory to

examine our proposed route more narrowly, and to admire our noble

couloir, which led straight up into the heart of the mountain for fully

one thousand feet. It then bent toward the north, and ran up to the

crest of the south-eastern ridge. My curiosity was piqued to know what

was round this corner, and whilst I was gazing up at it, and following

with the eye the exquisitely drawn curves which wandered down the snow

in the gully, all converging to a large rut in its centre, I saw a few

little stones skidding down. I consoled myself with thinking that they

would not interfere with us if we adhered to the side. But then a

larger one came down, a solitary fellow, rushing at the rate of sixty

miles an hour—and another—and another. I was unwilling to raise the

fears of the men unnecessarily, and said nothing to them. They did not

hear the stones. Almer was seated on a rock, carving large slices from

a leg of mutton, the others were chatting, and the first intimation

they had of danger was from a crash, a sudden roar, which reverberated

awfully amongst the cliffs; and looking up they saw rocks, boulders and

stones, big and little, dart round the corner eight hundred feet or so

above us, fly with fearful fury against the opposite cliffs, rebound

from them against the walls on our side, and descend; some ricochetting

from side to side in a frantic manner, some bounding down in leaps of a

hundred feet or more over the snow, and more trailing down in a

jumbled, confused mass, mixed with snow and ice, deepening the grooves

which a moment before had excited my admiration.

The men looked wildly around for protection, and, dropping the food,

dashed under cover in all directions. The precious mutton was pitched

on one side, the wine-bag was let fall, and its contents gushed out

from the unclosed neck, while all four cowered under defending rocks,

endeavoring to make themselves as small as possible. Let it not be

supposed that their fright was unreasonable or that I was free from it.

I took good care to make myself safe, and went and cringed in a cleft

until the storm had passed. But their scramble to get under shelter was

indescribably ludicrous. Such a panic I have never witnessed, before or

since, upon a mountain-side.

This ricochet practice was a novelty to me. It arose, of course, from

the couloir being bent, and from the falling rocks having acquired

great pace before they passed the angle. In straight gullies it will

probably never be experienced. The rule is, as I have already remarked,

that falling stones keep down the centres of gullies, and you are out

of harm’s way if you follow the sides.

[Illustration: MY TENT-BEARER—THE HUNCHBACK.]

There would have been singularly little amusement and very great risk

in mounting this gully, and we turned our backs upon it with perfect

unanimity. The question then arose, “What is to be done?” I suggested

climbing the rocks above us, but this was voted impossible. I thought

the men were right, but would not give in without being assured of the

fact, and clambered up to settle the question. In a few minutes I was

brought to a halt. My forces were scattered: the little hunchback alone

was closely following me, with a broad grin upon his face and the tent

upon his shoulder; Croz, more behind, was still keeping an eye upon his

_Monsieur;_ Almer, a hundred feet below, sat on a rock with his face

buried in his hands; Biener was nowhere, out of sight. “Come down, come

down,” shouted Croz, “it is useless;” and I turned at length, convinced

that it was even as he said. Thus my little plan was knocked on the

head, and we were thrown back upon the original scheme.

We at once made a straight track for Mr. Morshead’s Breuiljoch (which

was the most direct route to take in order to get to the Hörnli, where

we intended to sleep, preparatory to attacking the eastern face), and

arrived upon its summit at 12.30 P.M. We were then unexpectedly

checked. The pass, as one, had vanished! and we found ourselves cut off

from the Furggengletscher by a small but precipitous wall of rock: the

glacier had shrunk so much that descent was impracticable. During the

last hour clouds had been coming up from the south: they now surrounded

us, and il began to blow hard. The men clustered together, and

advocated leaving the mountain alone. Almer asked, with more point than

politeness, “Why don’t you try to go up a mountain which _can_ be

ascended?” “It is impossible,” chimed in Biener. “Sir,” said Croz, “if

we cross to the other side we shall lose three days, and very likely

shall not succeed. You want to make ascents in the chain of Mont Blanc,

and I believe they can be made. But I shall not be able to make them

with you if I spend these days here, for I must be at Chamounix on the

27th.” There was force in what he said, and his words made me hesitate.

I relied upon his strong arms for some work which it was expected would

be unusually difficult. Snow began to fall: that settled the matter,

and I gave the word to retreat. We went back to Breuil, and on to Val

Tournanche, where we slept; and the next day proceeded to Chatillon,

and thence up the valley of Aosto to Cormayeur.

I cannot but regret that the counsels of the guides prevailed. If Croz

had not uttered his well-intentioned words he might still have been

living. He parted from us at Chamounix at the appointed time, but by a

strange chance we met again at Zermatt three weeks later; and two days

afterward he perished before my eyes on the very mountain from which we

turned away, at his advice on the 21st of June.

Scrambles Amongst the Alps in the Years 1860-69 · 第 15 / 22 章