Management of Mass Movements

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Management of Mass Movements

Managing landslide hazards

1. Modifying the event

Slope stability can be increased by a variety of engineering

techniques, which although expensive, enable control of land sliding

to be largely successful. There are 2 key issues with this approach to

landslide hazard management: cost and responsibility. Government

funding may be available for emergency stabilization. However,

building codes can enforce some user if these techniques by private

developers.

2. Modify vulnerability

Most mass movements are not very rapid and thus forecasting, warning

and evacuation are possible techniques. Community preparedness can be

used if people are aware of the early signs of mass movement such as

bulging walls, tension cracks, tilted poles and fences and new areas

of waterlogged ground.

Hazard mapping is increasingly being used especially in MEDC’s, as the

factors that favour land sliding can be assessed to produce a hazard

map. Landslide hazard assessment maps are ways of predicting the

landslide threat using the factors, which influence slope stability.

However, forecasting the magnitude and frequency of events is not

possible. There may be problems in this approach in already developed

areas, where a high hazard rating may reduce land values.

Sharing the loss

Private insurance for landslide hazards is not easily available due to

the high risks involved for the insurance companies. Legal liability

is becoming an increasingly common loss-sharing adjustment. Since the

landslide producing processes are well understood the “acts of god”

argument when landslides occur is losing credibility.

Methods of stabilizing hill slopes

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Managing snow avalanches

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Avalanche formation and their characteristics

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An avalanche is a rapid movement of snow down a slope as a result of

structural weakness in the snow cover on the slope. There are 3 main

forms of snow avalanche with different characteristics of slope

failure, flow and occurrence – loose snow, slab and slush.

Slab avalanches are the most dangerous since large masses of snow are

involved.

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