Landslides - the sliding danger

However, they can be very drastic locally

 

Landslides and hillslope debris flows occur everywhere in Switzerland. Nationally, however, they are not among the biggest causes of damage. However, they can be very drastic locally, such as in 1994 in Falli-Hölli, Fribourg, when an entire holiday home settlement with 37 houses was swept away and destroyed by a landslide.

Depending on the depth of the sliding surface, landslides are labelled as shallow, medium or deep. A distinction is also made as to whether they move permanently or spontaneously. If the landslide mass is pulpy with a high water content, it is referred to as a hillslope debris flow.

 

In contrast to hillslope debris flows, debris flows are not categorised as landslide processes. Debris flows occur in the channel of a watercourse. It is not uncommon for landslides to lead to secondary rockfall from the landslide mass.

Effects of climate change

Climate change leads to landslides

As a result of climate change, heavy rainfall is becoming more frequent and more intense. The soils on slopes are becoming saturated and can increasingly lead to shallow to medium landslides and hillslope debris flows. In addition, the retreat of the glaciers leads to more unstable slopes. One example of this is the large Moosfluh landslide in the Aletsch region (VS), where the slope slides up to 30 metres per year due to glacier retreat.

 

The retreat of the glaciers is also leading to more unstable slopes

 

Monitoring and protective measures

Monitoring and protective measures

The damage caused by landslides has been reduced in recent years by means of various measures. These include hazard maps, monitoring (as in Moosfluh, Aletsch) or targeted structural protection measures (such as dams or drainage). Adapted construction methods and, last but not least, evacuation and resettlement orders also help to minimise damage.

 

Effective measures

Effective measures

With their spatial planning instruments and authorisation practices, the cantons and municipalities make a significant contribution to reducing the risks posed by landslides. Owners can protect themselves and their buildings with hazard-adapted construction methods. Examples of measures include

 

Spatial planning measures

  • Plan settlement development in hazard-free areas
  • Designate differentiated hazard zones and restrict uses
  • Issue building bans in high-risk areas
  • Decide on conditions for new buildings and conversions in endangered areas

Technical measures

  • Constructing buildings and facilities using robust construction methods
  • Collect and drain surface water in a controlled manner
  • Build drainage systems, open drainage ditches and tunnels
  • Construct protective structures such as slope debris networks, slope stabilisation or protective dams
  • Maintain and repair existing protective structures
  • Keep the drainage corridors of watercourses in landslide areas clear

Biological measures

  • Plant potential landslide areas with suitable tree species (against shallow and medium landslides)
  • Maintain existing protection forests

Organisational measures

  • Monitor known landslide areas
  • Set up warning and alarm systems
  • Draw up evacuation plans
  • (Temporarily) close traffic routes and hiking trails
  • Plan resettlements

Risk communication in Brienz (GR)

Thanks to permanent monitoring and an ordered evacuation, there was no disaster in the municipality of Albula. The existing uncertainties in the development were communicated transparently. The municipality and the canton provided comprehensive information to those affected on an ongoing basis.

 

Chronicle

Important landslides and hillslope debris flows

1857 Campo Vallemaggia

A landslide mass of over 100 million cubic metres destroyed ten houses and numerous stables in Campo Vallemaggia (TI). 

1994 Falli-Hölli

A landslide with a volume of 40 million m3 and a surface area of 2 km2 partially or completely destroyed more than 30 holiday homes in Falli-Hölli (FR). Damage totalling around CHF 20 million was caused. Thanks to timely evacuation, there were no injuries. 

 

2000 Gondo

On 14 October, a tragedy occurred in the village of Gondo (VS): the persistent rain softened the foundations of a retaining wall above the village. When a mudslide pressed down on top of it, the massive concrete wall toppled over. Within 20 seconds, an avalanche of mud, debris and boulders poured over the village, burying it under its weight. 13 people lost their lives.

 

2005

During the storms in August, more than 5000 landslides and debris flows were documented. Major damage was caused to buildings. In Entlebuch (LU), two firefighters were caught in a landslide and killed. In Weggis (LU), landslides and a secondary landslide destroyed three buildings. The residents were evacuated in good time.

 

2023 Brienz

The village of Brienz/Brinzauls (GR) lies on a large landslide that has accelerated in recent years - from a few centimetres to over one metre per year. A smaller, higher landslide also threatened the village. The landslide occurred in mid-June 2023, but was relatively minor: The authorities had temporarily evacuated the population beforehand. 

 

2023 Schwanden

At the end of August, after heavy rainfall above Schwanden (GL), a landslide occurred that extended over a length of more than 400 metres. Almost 100 people were evacuated in time. A total of 38 buildings were buried or destroyed.

 

Cascade of natural hazards

Cascade of natural hazards

Sometimes natural hazards lead to a chain of events. Landslides can play a role in other natural hazards:

 

Rock and landslide

Landslides and hillslope debris flows can trigger a secondary rock or boulder fall.

Water hazards

Large landslides and in particular hillslope debris flows can lead to blockages in watercourses or to surge waves.  

Further information on landslides can be found at

 

Last change: 27.08.2024