A Tramp Abroad Part 36

Well, I had to go overland--there was no other way. I marched the Expedition down the steep and tedious mule-path and took up as good a position as I could upon the middle of the glacier--because Baedeker said the middle part travels the fastest. As a measure of economy, however, I put some of the heavier baggage on the sh.o.r.eward parts, to go as slow freight.

I waited and waited, but the glacier did not move. Night was coming on, the darkness began to gather--still we did not budge. It occurred to me then, that there might be a time-table in Baedeker; it would be well to find out the hours of starting. I called for the book--it could not be found. Bradshaw would certainly contain a time-table; but no Bradshaw could be found.

Very well, I must make the best of the situation. So I pitched the tents, picketed the animals, milked the cows, had supper, paregoricked the men, established the watch, and went to bed--with orders to call me as soon as we came in sight of Zermatt.

I awoke about half past ten next morning, and looked around. We hadn't budged a peg! At first I could not understand it; then it occurred to me that the old thing must be aground. So I cut down some trees and rigged a spar on the starboard and another on the port side, and fooled away upward of three hours trying to spar her off. But it was no use. She was half a mile wide and fifteen or twenty miles long, and there was no telling just whereabouts she _was_ aground. The men began to show uneasiness, too, and presently they came flying to me with ashy faces, saying she had sprung a leak.

Nothing but my cool behavior at this critical time saved us from another panic. I ordered them to show me the place. They led me to a spot where a huge boulder lay in a deep pool of clear and brilliant water. It did look like a pretty bad leak, but I kept that to myself. I made a pump and set the men to work to pump out the glacier. We made a success of it. I perceived, then, that it was not a leak at all. This boulder had descended from a precipice and stopped on the ice in the middle of the glacier, and the sun had warmed it up, every day, and consequently it had melted its way deeper and deeper into the ice, until at last it reposed, as we had found it, in a deep pool of the clearest and coldest water.

Presently Baedeker was found again, and I hunted eagerly for the time-table. There was none. The book simply said the glacier was moving all the time. This was satisfactory, so I shut up the book and chose a good position to view the scenery as we pa.s.sed along. I stood there some time enjoying the trip, but at last it occurred to me that we did not seem to be gaining any on the scenery. I said to myself, "This confounded old thing's aground again, sure,"--and opened Baedeker to see if I could run across any remedy for these annoying interruptions.

I soon found a sentence which threw a dazzling light upon the matter.

It said, "The Gorner Glacier travels at an average rate of a little less than an inch a day." I have seldom felt so outraged. I have seldom had my confidence so wantonly betrayed. I made a small calculation: One inch a day, say thirty feet a year; estimated distance to Zermatt, three and one-eighteenth miles. Time required to go by glacier, _a little over five hundred years!_ I said to myself, "I can _walk_ it quicker--and before I will patronize such a fraud as this, I will do it."

When I revealed to Harris the fact that the pa.s.senger part of this glacier--the central part--the lightning-express part, so to speak--was not due in Zermatt till the summer of 2378, and that the baggage, coming along the slow edge, would not arrive until some generations later, he burst out with:

"That is European management, all over! An inch a day--think of that!

Five hundred years to go a trifle over three miles! But I am not a bit surprised. It's a Catholic glacier. You can tell by the look of it. And the management."

I said, no, I believed nothing but the extreme end of it was in a Catholic canton.

"Well, then, it's a government glacier," said Harris. "It's all the same. Over here the government runs everything--so everything's slow; slow, and ill-managed. But with us, everything's done by private enterprise--and then there ain't much lolling around, you can depend on it. I wish Tom Scott could get his hands on this torpid old slab once--you'd see it take a different gait from this."

I said I was sure he would increase the speed, if there was trade enough to justify it.

"He'd _make_ trade," said Harris. "That's the difference between governments and individuals. Governments don't care, individuals do. Tom Scott would take all the trade; in two years Gorner stock would go to two hundred, and inside of two more you would see all the other glaciers under the hammer for taxes." After a reflective pause, Harris added, "A little less than an inch a day; a little less than an _inch_, mind you.

Well, I'm losing my reverence for glaciers."

I was feeling much the same way myself. I have traveled by ca.n.a.l-boat, ox-wagon, raft, and by the Ephesus and Smyrna railway; but when it comes down to good solid honest slow motion, I bet my money on the glacier. As a means of pa.s.senger transportation, I consider the glacier a failure; but as a vehicle of slow freight, I think she fills the bill. In the matter of putting the fine shades on that line of business, I judge she could teach the Germans something.

I ordered the men to break camp and prepare for the land journey to Zermatt. At this moment a most interesting find was made; a dark object, bedded in the glacial ice, was cut out with the ice-axes, and it proved to be a piece of the undressed skin of some animal--a hair trunk, perhaps; but a close inspection disabled the hair-trunk theory, and further discussion and examination exploded it entirely--that is, in the opinion of all the scientists except the one who had advanced it. This one clung to his theory with affectionate fidelity characteristic of originators of scientific theories, and afterward won many of the first scientists of the age to his view, by a very able pamphlet which he wrote, ent.i.tled, "Evidences going to show that the hair trunk, in a wild state, belonged to the early glacial period, and roamed the wastes of chaos in the company with the cave-bear, primeval man, and the other Ooelitics of the Old Silurian family."

Each of our scientists had a theory of his own, and put forward an animal of his own as a candidate for the skin. I sided with the geologist of the Expedition in the belief that this patch of skin had once helped to cover a Siberian elephant, in some old forgotten age--but we divided there, the geologist believing that this discovery proved that Siberia had formerly been located where Switzerland is now, whereas I held the opinion that it merely proved that the primeval Swiss was not the dull savage he is represented to have been, but was a being of high intellectual development, who liked to go to the menagerie.

We arrived that evening, after many hards.h.i.+ps and adventures, in some fields close to the great ice-arch where the mad Visp boils and surges out from under the foot of the great Gorner Glacier, and here we camped, our perils over and our magnificent undertaking successfully completed.

We marched into Zermatt the next day, and were received with the most lavish honors and applause. A doc.u.ment, signed and sealed by the authorities, was given to me which established and endorsed the fact that I had made the ascent of the Riffelberg. This I wear around my neck, and it will be buried with me when I am no more.

CHAPTER XL

[Piteous Relics at Chamonix]

I am not so ignorant about glacial movement, now, as I was when I took pa.s.sage on the Gorner Glacier. I have "read up" since. I am aware that these vast bodies of ice do not travel at the same rate of speed; while the Gorner Glacier makes less than an inch a day, the Unter-Aar Glacier makes as much as eight; and still other glaciers are said to go twelve, sixteen, and even twenty inches a day. One writer says that the slowest glacier travels twenty-five feet a year, and the fastest four hundred.

What is a glacier? It is easy to say it looks like a frozen river which occupies the bed of a winding gorge or gully between mountains. But that gives no notion of its vastness. For it is sometimes six hundred feet thick, and we are not accustomed to rivers six hundred feet deep; no, our rivers are six feet, twenty feet, and sometimes fifty feet deep; we are not quite able to grasp so large a fact as an ice-river six hundred feet deep.

The glacier's surface is not smooth and level, but has deep swales and swelling elevations, and sometimes has the look of a tossing sea whose turbulent billows were frozen hard in the instant of their most violent motion; the glacier's surface is not a flawless ma.s.s, but is a river with cracks or crevices, some narrow, some gaping wide. Many a man, the victim of a slip or a misstep, has plunged down one of these and met his death. Men have been fished out of them alive; but it was when they did not go to a great depth; the cold of the great depths would quickly stupefy a man, whether he was hurt or unhurt. These cracks do not go straight down; one can seldom see more than twenty to forty feet down them; consequently men who have disappeared in them have been sought for, in the hope that they had stopped within helping distance, whereas their case, in most instances, had really been hopeless from the beginning.

In 1864 a party of tourists was descending Mont Blanc, and while picking their way over one of the mighty glaciers of that lofty region, roped together, as was proper, a young porter disengaged himself from the line and started across an ice-bridge which spanned a crevice. It broke under him with a crash, and he disappeared. The others could not see how deep he had gone, so it might be worthwhile to try and rescue him. A brave young guide named Michel Payot volunteered.

Two ropes were made fast to his leather belt and he bore the end of a third one in his hand to tie to the victim in case he found him. He was lowered into the crevice, he descended deeper and deeper between the clear blue walls of solid ice, he approached a bend in the crack and disappeared under it. Down, and still down, he went, into this profound grave; when he had reached a depth of eighty feet he pa.s.sed under another bend in the crack, and thence descended eighty feet lower, as between perpendicular precipices. Arrived at this stage of one hundred and sixty feet below the surface of the glacier, he peered through the twilight dimness and perceived that the chasm took another turn and stretched away at a steep slant to unknown deeps, for its course was lost in darkness. What a place that was to be in--especially if that leather belt should break! The compression of the belt threatened to suffocate the intrepid fellow; he called to his friends to draw him up, but could not make them hear. They still lowered him, deeper and deeper.

Then he jerked his third cord as vigorously as he could; his friends understood, and dragged him out of those icy jaws of death.

Then they attached a bottle to a cord and sent it down two hundred feet, but it found no bottom. It came up covered with congelations--evidence enough that even if the poor porter reached the bottom with unbroken bones, a swift death from cold was sure, anyway.

A glacier is a stupendous, ever-progressing, resistless plow. It pushes ahead of it ma.s.ses of boulders which are packed together, and they stretch across the gorge, right in front of it, like a long grave or a long, sharp roof. This is called a moraine. It also shoves out a moraine along each side of its course.

Imposing as the modern glaciers are, they are not so huge as were some that once existed. For instance, Mr. Whymper says:

"At some very remote period the Valley of Aosta was occupied by a vast glacier, which flowed down its entire length from Mont Blanc to the plain of Piedmont, remained stationary, or nearly so, at its mouth for many centuries, and deposited there enormous ma.s.ses of debris. The length of this glacier exceeded _eighty miles_, and it drained a basin twenty-five to thirty-five miles across, bounded by the highest mountains in the Alps.

"The great peaks rose several thousand feet above the glaciers, and then, as now, shattered by sun and frost, poured down their showers of rocks and stones, in witness of which there are the immense piles of angular fragments that const.i.tute the moraines of Ivrea.

"The moraines around Ivrea are of extraordinary dimensions. That which was on the left bank of the glacier is about _thirteen miles_ long, and in some places rises to a height of _two thousand one hundred and thirty feet_ above the floor of the valley! The terminal moraines (those which are pushed in front of the glaciers) cover something like twenty square miles of country. At the mouth of the Valley of Aosta, the thickness of the glacier must have been at least _two thousand_ feet, and its width, at that part, _five miles and a quarter._"

It is not easy to get at a comprehension of a ma.s.s of ice like that. If one could cleave off the b.u.t.t end of such a glacier--an oblong block two or three miles wide by five and a quarter long and two thousand feet thick--he could completely hide the city of New York under it, and Trinity steeple would only stick up into it relatively as far as a s.h.i.+ngle-nail would stick up into the bottom of a Saratoga trunk.

"The boulders from Mont Blanc, upon the plain below Ivrea, a.s.sure us that the glacier which transported them existed for a prodigious length of time. Their present distance from the cliffs from which they were derived is about 420,000 feet, and if we a.s.sume that they traveled at the rate of 400 feet per annum, their journey must have occupied them no less than 1,055 years! In all probability they did not travel so fast."

Glaciers are sometimes hurried out of their characteristic snail-pace.

A marvelous spectacle is presented then. Mr. Whymper refers to a case which occurred in Iceland in 1721:

"It seems that in the neighborhood of the mountain Kotlugja, large bodies of water formed underneath, or within the glaciers (either on account of the interior heat of the earth, or from other causes), and at length acquired irresistible power, tore the glaciers from their mooring on the land, and swept them over every obstacle into the sea. Prodigious ma.s.ses of ice were thus borne for a distance of about ten miles over land in the s.p.a.ce of a few hours; and their bulk was so enormous that they covered the sea for seven miles from the sh.o.r.e, and remained aground in six hundred feet of water! The denudation of the land was upon a grand scale. All superficial acc.u.mulations were swept away, and the bedrock was exposed. It was described, in graphic language, how all irregularities and depressions were obliterated, and a smooth surface of several miles' area laid bare, and that this area had the appearance of having been _planed by a plane_."

The account translated from the Icelandic says that the mountainlike ruins of this majestic glacier so covered the sea that as far as the eye could reach no open water was discoverable, even from the highest peaks.

A monster wall or barrier of ice was built across a considerable stretch of land, too, by this strange irruption:

"One can form some idea of the alt.i.tude of this barrier of ice when it is mentioned that from Hofdabrekka farm, which lies high up on a fjeld, one could not see Hjorleifshofdi opposite, which is a fell six hundred and forty feet in height; but in order to do so had to clamber up a mountain slope east of Hofdabrekka twelve hundred feet high."

These things will help the reader to understand why it is that a man who keeps company with glaciers comes to feel tolerably insignificant by and by. The Alps and the glaciers together are able to take every bit of conceit out of a man and reduce his self-importance to zero if he will only remain within the influence of their sublime presence long enough to give it a fair and reasonable chance to do its work.

The Alpine glaciers move--that is granted, now, by everybody. But there was a time when people scoffed at the idea; they said you might as well expect leagues of solid rock to crawl along the ground as expect leagues of ice to do it. But proof after proof was furnished, and the finally the world had to believe.

The wise men not only said the glacier moved, but they timed its movement. They ciphered out a glacier's gait, and then said confidently that it would travel just so far in so many years. There is record of a striking and curious example of the accuracy which may be attained in these reckonings.

In 1820 the ascent of Mont Blanc was attempted by a Russian and two Englishmen, with seven guides. They had reached a prodigious alt.i.tude, and were approaching the summit, when an avalanche swept several of the party down a sharp slope of two hundred feet and hurled five of them (all guides) into one of the crevices of a glacier. The life of one of the five was saved by a long barometer which was strapped to his back--it bridged the crevice and suspended him until help came. The alpenstock or baton of another saved its owner in a similar way. Three men were lost--Pierre Balmat, Pierre Carrier, and Auguste Tairraz. They had been hurled down into the fathomless great deeps of the crevice.

Dr. Forbes, the English geologist, had made frequent visits to the Mont Blanc region, and had given much attention to the disputed question of the movement of glaciers. During one of these visits he completed his estimates of the rate of movement of the glacier which had swallowed up the three guides, and uttered the prediction that the glacier would deliver up its dead at the foot of the mountain thirty-five years from the time of the accident, or possibly forty.

A dull, slow journey--a movement imperceptible to any eye--but it was proceeding, nevertheless, and without cessation. It was a journey which a rolling stone would make in a few seconds--the lofty point of departure was visible from the village below in the valley.

The prediction cut curiously close to the truth; forty-one years after the catastrophe, the remains were cast forth at the foot of the glacier.

I find an interesting account of the matter in the _Histoire Du Mont Blanc_, by Stephen d'Arve. I will condense this account, as follows:

On the 12th of August, 1861, at the hour of the close of ma.s.s, a guide arrived out of breath at the mairie of Chamonix, and bearing on his shoulders a very lugubrious burden. It was a sack filled with human remains which he had gathered from the orifice of a crevice in the Glacier des Bossons. He conjectured that these were remains of the victims of the catastrophe of 1820, and a minute inquest, immediately inst.i.tuted by the local authorities, soon demonstrated the correctness of his supposition. The contents of the sack were spread upon a long table, and officially inventoried, as follows:

Portions of three human skulls. Several tufts of black and blonde hair.