CHAPTER III

AVALANCHES

Many of the most terrible accidents in the Alps have been due to

avalanches, and perhaps, as avalanches take place from different

causes and have various characteristics, according to whether they are

of ice, snow, or _débris_, some account of them may not be out of

place.

We may briefly classify them as follows:--

1. Ice avalanches, only met with on or near glaciers.

2. Dust avalanches, composed of very light, powdery snow.

3. Compact avalanches (_Grund_ or ground avalanches, as the

Germans call them), consisting of snow, earth, stones,

trees, and anything which the avalanche finds in its path.

These take place only in winter and spring, while the two

other kinds happen on the mountains at any season.

An ice avalanche is easily understood when it is borne in mind that a

glacier is always moving. When this river of ice comes to the edge of

a precipice, or tries to crawl down a very steep cliff, it splits

across and forms tottering crags of ice, which lean over more and more

till they lose their balance and go crashing down the slope. Some of

the ice is crushed to powder by its fall, yet many blocks generally

survive, and are occasionally heaped up in such huge masses below that

they form another glacier on a small scale. If a party of mountaineers

passes under a place overhung by threatening ice, they are in great

danger, though at early morning, before the sun has loosened the

frozen masses, the peril is less. Sometimes, too, if the distance to

be traversed is very short and the going quite easy, it is safe enough

to dash quickly across.

[Illustration: A TUNNEL 300 FEET LONG THROUGH AN AVALANCHE.

Tree trunks, etc., can be seen embedded in it.]

[Illustration: AN AVALANCHE NEAR BOUVERET, LAKE OF GENEVA.]

Dust avalanches occur when a heavy fall of light, powdery snow takes

place on frozen hillsides or ice-slopes, and so long as there is no

wind or disturbance, all remains quiet, and inexperienced people would

think there was no danger. But in reality dust avalanches are the most

to be feared of any, for they fall irregularly in unexpected places,

and their power is tremendous. While all seems calm and peaceful,

suddenly a puff of wind or the passage of an animal disturbs the

delicately-balanced masses, and then woe betide whoever is within

reach of this frightful engine of destruction. First, the snow begins

to slide gently down, then it gathers pace and volume, and even miles

away the thunder of its fall can be heard as it leaps from ledge to

ledge. Covered with a cloud of smoking, powdery dust, it is a

veritable Niagara of giant height, and as it descends towards the

forests, it carries with it whatever it finds in its path. Trees are

mown down with as much ease as the tender grass of spring. Houses are

lifted from the ground and tossed far away.

An avalanche is preceded by a blast even more destructive than the

masses of snow which it hurls along. As it advances with

ever-increasing rapidity the air in front is more and more compressed

as the avalanche rushes on with lightning-like speed behind it. The

wind sweeps everything before it, and many are the tales related by

those who have survived or witnessed a display of its power. On one

occasion more than a hundred houses were overwhelmed by a huge

avalanche at Saas (Prättigau, near Davos), and during the search

afterwards the rescue party found amidst the ruins a child lying

asleep and uninjured in his cradle, which had been blown to some

distance from his home, while close by stood a basket containing six

eggs, none of which were broken. I have myself seen a row of telegraph

posts in an Alpine valley in winter thrown flat on the ground by the

air preceding an enormous avalanche, which itself did not come within

300 yards of them. It is a very wonderful thing that persons buried

beneath an avalanche can sometimes hear every word spoken by a search

party, and yet not a sound that they utter reaches the ears of those

outside. A great deal of air is imprisoned between the particles of

snow, and so it is possible for those overwhelmed by an avalanche to

live inside it for hours. Cases have been known where a man, buried

not far below the surface, has been able to melt a hole to the outer

air with his breath, and eventually free himself from his icy prison.

On 18th January, 1885, enormous avalanches fell in some of the

mountainous districts of northern Italy, houses, cattle, crops, and

granaries being carried away, and many victims buried beneath the

ruins. Some touching episodes of wonderful escapes were related. "For

instance, at Riva, in the valley of Susa, a whole family, consisting

of an old woman of seventy, her two daughters, her four nieces, and a

child four months old, were buried with their house in the snow,

exposed apparently to certain death from cold and hunger. But the

soldiers of the Compagnie Alpine, hearing of the sad case, worked with

all their might and main to save them, and at last they were found and

brought out alive, the brave old grandmother insisting that the

children should be saved first, and then her daughters, saying that

their lives were more precious than her own." The soldiers, who worked

with a will above all praise, were obliged in several cases to

construct long galleries in the snow in order to reach the villages,

which were sometimes buried beneath 40 feet of snow.

Compact avalanches, though very terrible on account of their

frequently great size, can be more easily guarded against than dust

avalanches, because they always fall in well-defined channels. A

compact avalanche consists of snow, earth, stones, and trees, and

comes down in times of thaw. Many fall in early spring in Alpine

valleys, and though it is not unusual for them to come right across

high roads, the fatal accidents are comparatively few. The inhabitants

know that wherever, high up on the hills, there is a hollow which may

serve as a _reservoir_ or collecting-basin for the snow, and below

this a funnel or shoot, there an avalanche may be expected. Often they

take means to prevent one starting, for an avalanche, whose power is

irresistible when once it has begun to move quickly, is very easily

kept from mischief if it is not allowed a running start. The best of

all ways for preventing avalanches is to plant the gullies with trees,

but where this cannot be done, rows of stakes driven into the ground

will serve to hold up the snow, and where the hillside is extremely

steep, and much damage would be caused if an avalanche fell, stone

walls are built one above another to keep the soil and the snow

together, very much as we see on precipitous banks overlooking English

railways.

The driving roads over Alpine passes are in places exposed to

avalanches in winter. At the worst spots galleries of stone are built,

through which the sleighs can pass in perfect safety, and if an

avalanche fell while they were inside it would pass harmlessly over

their heads. On the Albula Pass, in Switzerland, as soon as the

avalanches come down, tunnels are cut in the snow through them, and

are in constant use till early summer.

Occasionally houses or churches are built in the very path of an

avalanche. A V-shaped wall, called an avalanche-breaker, is put

behind, and this cuts the snowy stream in two parts, which passes on

harmlessly on either side of the building. Sometimes avalanche-breakers

of snow, hardened into ice by throwing water over them, are constructed

behind barns which have been put in exposed places.

In order that an avalanche may get up speed enough to commence its

swift career, the slope the snow rests on where it starts must be at

an angle of from 30° to 35° at least.

True Tales of Mountain Adventures: For Non-Climbers Young and Old · 第 3 / 21 章