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Avalanches



AVALANCHES

What is an avalanche: An avalanche is a mass of snow which is set in motion by its own weight through a violent disturbance of its equilibrium. There are two kinds of avalanches; the surface avalanche, in which only the top covering of snow slips, and the ground avalanche, in which the whole mass is carried away. A dreaded hazard. Often the victims are not individual climbers but whole group in the area. Prudent climbers and experienced mountaineers have also been killed or injured in avalanches. The secret lies in keeping off the dangerous slopes at the correct time, and also in knowing the conditions that cause avalanches. The subject requires thorough study of the causes, precautions, and conduct if caught in an avalanche.

The formation of avalanches: In summer, there are slides of stones and ice but relatively fewer avalanches, because of the stabilised snow. However, an increasing number of climbers are taking to the mountains in spring and even in winter. In addition to good technique, this demands a close knowledge of the mountains, because in winter and spring the snow not being stabilised there is the danger that sometime an avalanche will occur. The formation of an avalanche depends on the nature of the terrain, the quality/ quantity of the snow and the temperature.

The nature of the terrain: Slippery surfaces, turf, flattened grass, slabs of laminated rock or smooth rock, under-layers of hard snow or ice, all these are surfaces on which avalanches are likely to occur because the snow does not cling to them.

The contour of the terrain: Convex slopes are more dangerous than concave ones which flatten out at the base. Similarly with the incline any slope of under 15 degrees is safe, provided that it is not dominated by steeper slopes. Snow slabs are dangerous above 15 degree onwards. Fresh snows (powdery and wet) are dangerous from 25 degree onwards; compressed powder snows, and spring snows, are safe upto 30 degrees. Most of the dangerous avalanches originate on slopes between 30 and 45 degrees. Be careful when you are on such slopes.

The nature of the snow: Instability increases with the thickness of the covering, but also according to the physical characteristics of snow. Fresh snow and snow which does not adhere (powder snow or moist snow on a wet base) are the most unstable.

Temperature: When the temperature rises, the snow humidifies and becomes heavy and therefore unstable. Cold on the other hand stabilizes it by causing the crystals to interlock. In summer, after fresh snowfall, one should wait two or three days before setting out on a climb.

How avalanches are triggered off: In certain terrain and under certain conditions avalanches can be predicted but sometimes they start unexpectedly when the top layers of snow become detached by a sudden disturbance of their mechanical or thermal equilibrium.

Failure of mechanical equilibrium: This may be caused by the passage of a climber or a skier, particularly if he is traversing the mountain slope. Overloading of a slope by several climbers and skiers; fall of a cornice, or falling seracs or stones, vibrations of the atmosphere can trigger off an avalanche particularly on slopes with powder snow.

Principal types of Avalanches.

Rules to be observed in an Avalanche zone.

If caught in an Avalanche.

If you are the Survivor.

KEEP THE MOUNTAINS CLEAN









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Published on: 2005-06-02 (3675 reads)

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