Landslide

Landslide is the downslope movement of soil, rock and organic materials under the effects of gravity, which occurs when the gravitational driving forces exceed the frictional resistance of the material resisting on the slope. Landslides could be terrestrial or submarine (Varnes, 1978).

Landslides can be triggered by geological and physical causes such as glacier or snow melts, heavy rains and water pressure, earthquakes, volcanic eruptions and overly steep slopes. Landslides can also be triggered by human action, the most common being building on unstable slopes. Submarine landslides, or massive slides and rock falls hitting the sea can also cause tsunamis.

Landslides can reach speeds of over 50 km/h and can bury, crush or carry away people, objects and buildings. Landslides cannot be predicted but warning systems measuring rainfall levels can provide warning to people living in landslide-prone areas.

Instrumental monitoring to detect movement and the rate of movement can be implemented, for example, extensometers, global positioning system (GPS), seismometers, aerial photography, satellite images, LiDaR (Highland and Bobrowsky, 2008) with varying degrees of success. Increasingly, the science of landslide physics is allowing the nature of these hazards to be understood, which is leading to better techniques through which they can be managed and mitigated (HIP).

Risk factors

  • Population growth
  • Rapid urbanization
  • Environmental degradation (deforestation and inappropriate use of lands and slopes)
  • High population density, heavy rainfall and rapid land use changes increase the instability of slopes

Risk reduction measures

  • Early warning systems to observe and alert before landslides happen
  • Hazard maps to identify landslides risk and vulnerabilities
  • Integrate landslide risk assessment into urban planning strategies
  • Building codes and standards for materials that reinforce landslide resilience
  • Improve drainage, building tunnels and trenches to stabilize slopes
  • Protect forest cover and regulate logging
  • Raise awareness of landslide risk
  • Regular drills and community evacuation exercises
  • Establish national, regional, and local evacuation plans

Latest Land Slide additions in the Knowledge Base

There are several ways to increase the reliability of risk maps. These include utilizing onsite monitoring data for model calibration and validation, leveraging local knowledge and information for spot checks, and conducting robust quality control.
World Bank, the
Cover IJDRR
This articleprovides insights and lessons from two case studies of unprecedented landslide-triggered tsunami risk in recently deglaciated areas that have not previously been described in the relocation literature: Iceland and Greenland.
Albania is exposed to a range of natural hazards, and it experiences recurring heavy rains, floods, landslides, droughts, and extreme summer heat, which can cause wildfires.
Global Facility for Disaster Reduction and Recovery, the (GFDRR)
The January 27 storm that hit Auckland has caused widespread damage. While climate change helps explain the intensity of the rainfall, the way land has been used and built on in the city is a major factor in what happened.
Conversation Media Group, the
Cover
This booklet refers to the initiatives taken by the National Disaster Management Authority in India, in managing the risk of landslides.
Cover
This briefing note describes a bottom-up methodology for landslide early warning systems, which should consider the knowledge and participation of local communities.
Temple in front of a waterfall in a forest in Japan.
In disaster-prone Japan, torrential rains exacerbated by the climate crisis have caused serious flooding and landslides in recent years, including in the country’s many forests.
Mongabay
Landslide on the Manali
As low-income, informal settlements bloom in the tropics, their risk of landslides increases. A new modeling tool incorporates urbanization factors to protect the region’s poorest neighborhoods.
American Geophysical Union
Eos - AGU

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