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An active landslide in the Gansu Province of China (Credit: Bruce D Malamud, 2012). A video of this landslide can be found at Vimeo.
A good link for ‘what are landslides’ can be found at the UK British Geological Survey.
This FAQ updated on 12 Nov 2013 by the EU FP-7 LAMPRE project.
A02. Landslides happen when rocks and sediment loosen and roll down a slope. Some of the factors that influence the occurrence of landslides include gravity, water, slope angle, climate, weathering, vegetation, overloading, geology and slope stability. How these factors interrelate is important in understanding what causes landslides along with an understanding of the impact humans have on these factors by altering natural processes.
Natural causes of landslides include (information from Geoscience Australia, 2013):
- elevation of pore water pressure by saturation of slope material from either intense or prolonged rainfall and seepage
- vibrations caused by earthquakes
- undercutting of cliffs and banks by waves or river erosion
- volcanic eruptions
Human causes include (information from Geoscience Australia, 2013):
- removal of vegetation
- interference with, or changes to, natural drainage
- leaking pipes such as water and sewer reticulation
- modification of slopes by construction of roads, railways, buildings, etc.
- overloading slopes
- mining and quarrying activities
- vibrations from heavy traffic, blasting, etc.
- excavation or displacement of rocks.
Landslides are influenced by gravity, water and triggering events. When shear stress (driving forces) of the material becomes more than its shear strength (resisting forces) the material moves down-slope. The shear strength divided by the shear stress is called the Factor of Safety. A good resource for driving and resisting forces can be found in a lecture from Humboldt University.
This FAQ updated on 12 Nov 2013 by the EU FP-7 LAMPRE project.
This FAQ updated on 12 Nov 2013 by the EU FP-7 LAMPRE project.

Location of the landslides (2007 to 2013) (Figure from National Space and Aeronautics Administration, 2014)
This FAQ updated on 26 Aug 2014 by the EU FP-7 LAMPRE project.
This FAQ updated on 12 Nov 2013 by the EU FP-7 LAMPRE project.

Types of landslides (Figure from British Geological Survey, 2013)
The types of landslides can be briefly defined as:
- Fall: Falls are landslides that involve the collapse of material from a cliff or steep slope. Falls usually involve a mixture of free fall through the air, bouncing or rolling. A fall type landslide results in the collection of rock or debris near the base of a slope.
- Topple: Topple failures involve the forward rotation and movement of a mass of rock, earth or debris out of a slope. This failure is noted to occur around an axis or point at or near the base of the block. A topple often results in the formation of debris or a debris cone at the base of the slope.
- Slide — rotational, translational: A slide type landslide is a down-slope movement of material that occurs along a distinctive surface. If the surface is straight then it is termed translational or planar. If this surface is curved the slide is called a rotational.
- Spread: Spread landslides involve lateral spread of rocks and soil masses.
- Flow: Flows are landslides that involve the movement of material down a slope in the form of a fluid. Flows often leave behind a distinctive upside-down funnel shaped deposit where the landslide material has stopped moving.
- Complex: These landslides are a combination of falls, topples, slides, spreads and flows.
This FAQ updated on 26 Aug 2014 by the EU FP-7 LAMPRE project.
- Restrict construction near steep slopes, close to mountain edges, near drainage ways, or natural erosion valleys.
- Get an assessment of your property.
- Contact local officials, regional geological surveys or departments of natural resources, and university departments of geology. Landslides occur where they have before, and in identifiable hazard locations.
- Ask for information on landslides in your area, specific information on areas vulnerable to landslides, and request a professional referral for a very detailed site analysis of your property, and corrective measures you can take, if necessary.
- If you are at risk from a landslide talk to your insurance agent. Debris flow may be covered by flood insurance policies, but this varies from country to country.
- Learn about local emergency response and evacuation plans.
- Talk to everyone in your household about what to do if a landslide occurs.
- Create and practice an evacuation plan for your family and your business.
- Assemble and maintain an emergency preparedness kit.
- Watch the patterns of storm water drainage on slopes near your home, especially where runoff water converges
- Minimize home hazards:
- Have flexible pipe fittings installed to avoid gas or water leaks, as flexible fittings are more resistant to breakage (only professionals should install gas fittings).
- Plant ground cover on slopes and build retaining walls.
- In mudflow areas, build channels or deflection walls to direct the flow around buildings.
- Remember: If you build walls to divert debris flow and the flow lands on a neighbour’s property, you may be liable for damages.
This FAQ updated on 11 Jan 2015 by the EU FP-7 LAMPRE project.
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Signs of Slope instability (Figure from North Vancouver District, 2013) |
- Doors or windows stick or jam for the first time.
- New cracks appear in plaster, tile, brick, or foundations.
- Outside walls, walks, or stairs begin pulling away from the building.
- Slowly developing, widening cracks appear on the ground or on paved areas such as streets or driveways.
- Underground utility lines break.
- Bulging ground appears at the base of a slope.
- Water breaks through the ground surface in new locations.
- Fences, retaining walls, utility poles, or trees tilt or move.
- A faint rumbling sound that increases in volume is noticeable as the landslide nears.
- The ground slopes downward in one direction and may begin shifting in that direction under your feet.
- Unusual sounds, such as trees cracking or boulders knocking together, might indicate moving debris.
- Collapsed pavement, mud, fallen rocks, and other indications of possible debris flows or landslides can be seen when driving (embankments along roadsides are particularly susceptible to landslides.
- Storm-water drainage on slopes changing their patterns (especially where runoff water converges).
This FAQ updated on 12 Nov 2013 by the EU FP-7 LAMPRE project.
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Be alert while driving (Figure from Be Safe During a Landslide, 2013) |
- If you remain or are caught suddenly at home, move to a second story if possible. Staying out of the path of a landslide or debris flow saves lives.
- If you are near a stream or channel, be alert for any sudden increase or decrease in water flow and for a change from clear to muddy water. Such changes may indicate landslide activity upstream, so be prepared to move quickly. Don't delay! Save yourself, not your belongings.
- Be especially alert if you are driving. Embankments along roadsides are particularly susceptible to landslides. Watch the road for collapsed pavement, mud, fallen rocks, and other indications of possible debris flows. A landslide can completely engulf a car on a road that is in its path.
- Whenever you are in the path of a landslide or debris flow, move away as quickly as possible. If escape is not possible, curl into a tight ball and protect your head with your hands or a helmet.
This FAQ updated on 12 Nov 2013 by the EU FP-7 LAMPRE project.
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Obey Safey warnings (Figure from Be Safe During a Landslide, 2013) |
- Stay away from the slide area. There may be danger of additional slides.
- Check for injured and trapped persons near the slide, without entering the direct slide area. Direct rescuers to their locations.
- Watch for associated dangers such as broken electrical, water, gas, and sewage lines and damaged roadways and railways.
- Return home with care. If you left your property or home to go to safer ground, be very careful when you return. Things to consider include:
- Understanding that returning home can be both physically and mentally challenging. Above all, use caution.
- Keep a battery-powered radio with you so you can listen for emergency updates and news reports.
- Use a battery-powered flash light to inspect a damaged home. The flashlight should be turned on outside before entering—the battery may produce a spark that could ignite leaking gas, if present.
- Watch out for animals, especially venomous snakes. Use a stick to poke through debris.
- Use the phone only to report life-threatening emergencies.
- Stay off the streets. If you must go out, watch for fallen objects, downed electric wires, and weakened walls, bridges, roads, and sidewalks.
This FAQ updated on 12 Nov 2013 by the EU FP-7 LAMPRE project.
This FAQ updated on 12 Nov 2013 by the EU FP-7 LAMPRE project.
This FAQ updated on 12 Nov 2013 by the EU FP-7 LAMPRE project.
- property damage,
- injury
- (less often) death
The negative economic effects of landslides include
- the cost to repair structures
- loss of property value
- disruption of transportation routes
- medical costs in the event of injury
- indirect costs, such as lost timber and fish stocks
- Water availability, quantity, and quality
- adversely affecting a variety of environmental and human systems and resources including water supplies, sewage disposal systems, and roadways.
Resources like fisheries, forests, dams, and mines can be affected for years after a slide event.
This FAQ updated on 12 Nov 2013 by the EU FP-7 LAMPRE project.
A. Addressing the slope (gradient): One of the main causes of landslides is gravity, so that the steeper the slope, the greater the likelihood of a landslide occurring. One landslide prevention technique is to regrade the slope, which means reducing the steepness (i.e. the angle) of the slope.
B. Addressing the amount of water: Another main cause of landslides is water, which can cause the earth to be much heavier and change the grain to grain contact. This results in more likelihood of a landslide occurring. Heavy rains, flash floods, melting of snow in warm weather, changes in the groundwater table, and poor drainage, can all result in increasing the likelihood of landslides. Geotechnical engineering practices, that can reduce the likelihood of landslides occurring include: diverting water and draining water from slopes.
C. Addressing added weight at the top of a hill or slope: Human-made structures (houses, buildings, mine waste areas, water reservoirs) on top of hills or slopes can also result in landslides, as they add weight. One technique in this case is to calculate an adequate setback distance between the top of slope and construction.
D. Addressing undercutting of the toe of the slope: Another human-made cause of landslides is undercutting the toe of a slope. This can happen when a road is cut into the side of a hill, or water from a river or large body of water undercuts a slope. The toe plays a critical role in keeping the upper portion stable. Landslide prevention in this case entails either filling in the toe with material, regrading the slope (see A above), stabilizing the slope (see E below), or the construction of soil mounds with sloping sides, placed at the toe of the slope to provide additional resistance to the potential movement of the upper part of the slope.
E. Stabilizing the slope: Other landslide protection can include stabilizing the slope, for example:
- wire meshing
- retaining walls
- soil nailing
- rock bolting
- shotcreting
One can also use vegetation to stabilize a slope.
F. Sustainable land use: Certain types of land use increase slope instability, for example roads or trails and forest conversion to agriculture (typically associated with burning). Restricting those land use types and engaging in sustainable land use practises can reduce landslide. These include tree planting, soil and water conservation activities. Finally, we should recognize that we cannot protect ‘everyone’ in ‘every location’, and there are other approaches to managing landslide risk, such as ensuring appropriate land-use regulations are in place. For example, people might be refused zoning permission to have a house where landslides are known to frequently occur.
This FAQ updated on 12 Nov 2013 by the EU FP-7 LAMPRE project.
- when (for example, a specific day, or hour)
- where (for example, what city, or what specific hill, or side of a hill)
- how big (for example, how much energy is released or the volume of material)
Predictions (in the landslide community) often depend on knowledge of where past landslides have occurred. This knowledge can come from photos taken by airplanes (air photos), images taken by satellites (remote sensing), asking local people where landslides have occurred in the past (local knowledge) and locally kept reports (town records, newspapers). Knowledge of past landslide events can be combined with information on topography and geology, to give a broad idea of which slopes are more or less likely to fail. Although scientists have an idea that one slope might be more prone to failure than another one, nobody knows which slope will actually have a landslide. Exact predictions are difficult, hence estimation of the chance of one slope being more likely to fail than another is more common.
There are warning signs for individual landslides. A good list of these is given by the United States Geological Survey.
Not all rainfall or earthquakes trigger landslides, but a greater volume of rain over a longer period will generally trigger more landslides (sometimes many more) than a smaller volume of rain over the same time period. Very large triggered landslide events, where the number of landslides can be tens to hundreds of thousands, can result in large amounts of damage, community isolation, and fatalities. Therefore, some early warning about a large rainfall storm, would give some idea that there may be a large number of landslides occurring soon afterwards. This is part of a national landslide warning system currently being used in Italy.
Predicting where a given landslide will occur, when AND how big is currently beyond our capabilities. But, we can have general ideas of where is more likely and where is less likely for landslides to occur. See also Q20 on landslide susceptibility.
With this knowledge, we can prepare ourselves the possibility of landslides.
This FAQ updated on 12 Nov 2013 by the EU FP-7 LAMPRE project.
This FAQ updated on 12 Nov 2013 by the EU FP-7 LAMPRE project.
This FAQ updated on 12 Nov 2013 by the EU FP-7 LAMPRE project.
This FAQ updated on 26 Aug 2014 by the EU FP-7 LAMPRE project.
This FAQ updated on 26 Aug 2014 by the EU FP-7 LAMPRE project.
Landslide susceptibility map (Figure from European Commission – Joint Research Centre, 2013)
A Europe wide landslide susceptibility map (the likelihood of landslides occurring) is given by Günther et al. (2013).
This FAQ updated on 12 Nov 2013 by the EU FP-7 LAMPRE project.
Part of a landslide inventory map resulting from the 1998 earthquake in Northridge, California, USA (Data from USGS open file 95-213) overlayed on Google Earth
It is very important to prepare landslide inventory maps and to know where the landslides occurred in the past. This information can be used in preparing landslide susceptibility maps and in predicting landslides, which in turn can be used to reduce the damage caused by landslides.
This FAQ updated on 12 Nov 2013 by the EU FP-7 LAMPRE project.
Risk = (Probability of Occurrence) times (Potential Impact)
The impact might be monetary loss, loss of life, etc. A landslide economic risk map shows the potential annual cost of landslide damage throughout a region. Risk maps combine the probability information from a landslide hazard map with an analysis of all possible consequences (property damage, casualties, and loss of service).
Landslide risk index map, Cuban Archiepelago (Figure from Castellanos and Van Western, 2007)
This FAQ updated on 26 Aug 2014 by the EU FP-7 LAMPRE project.
Landslide hazard map (Figure from European Spatial Planning Observation Network (ESPON) (2006))
This FAQ updated on 12 Nov 2013 by the EU FP-7 LAMPRE project.
This FAQ updated on 12 Nov 2013 by the EU FP-7 LAMPRE project.
A25.
- Start with some of the links given in Q24 above.
- Some useful links online.
- American Red Cross
- Be Safe net
- Be Safe During a Landslide
- California Emergency Management Agency
- European Commission – Joint Research Centre
- British Geological Survey
- British Geological Survey landslides case studies
- European Spatial Planning Observation Network
- Federal Emergency Management Agency
- Geoscience Australia
- Landslide Hazard Program, USA
- North Vancouver DistrictUnited States Geological Survey
- References Cited in Text or Other Good Articles
- Brunsden, D. (1985). Landslide types, mechanisms, recognition, identification. Proc. Symposium on Landslides in the South Wales Coalfield, 1-3 April 1985. The Poly. of Wales, 19-28.
- Cruden, D.M. 1991, "A simple definition of a landslide", Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur, vol. 43, no. 1, pp. 27-29.
- Cruden, D.M. and Varnes, D.J. (1996). Landslide types and processes. Landslides: investigation and mitigation, 247, pp. 36-75.
- Dikau, R., Brunsden, D., Shrott, L., Ibsen, M. L. eds (1996). Landslide Recognition. Identification, Movement and Causes. Wiley, Chichester, UK, 251 pp.
- Günther, A., Reichenbach, P., Malet, J., Eeckhaut, M., Hervás, J., Dashwood, C. & Guzzetti, F. 2013, "Tier-based approaches for landslide susceptibility assessment in Europe", Landslides, vol. 10, no. 5, pp. 529-546.
- Guzzetti, F., Carrara, A., Cardinali, M. and Reichenbach, P. (1999). Landslide hazard evaluation: a review of current techniques and their application in a multi-scale study, Central Italy. Geomorphology, 31(1), pp. 181-216.
- Hervas, J. ed (2003). Lessons learnt from landslide disasters in Europe. EUR 20558 EN, European Commission, Ispra, Italy, 91 p.[Online] Available here [Accessed on 21 October 2013]
- Highland, L. M. and Bobrowski, P. (2008). The Landslide Handbook – A Guide to Understanding Landslides, U. S. Geological Survey Circular 1325, 129 p. [Online] Available here [Accessed on 18 July 2014]
- Hutchinson, J.N., 1988. Morphological and geotechnical parameters of landslides in relation to geology and hydrology, General Report. In: Bonnard, C., (Ed), Landslides, Proc. 5th International Symposium on Landslides, Rotterdam: Balkema. Vol. 1, 3-35.
- IUGS—Working group on landslide (1995). A suggested method for describing the rate of movement of a landslide. Bulletin of the International Association of Engineering Geology 52, 75–78.
- Schuster, R. L., and Highland, L. M. (2004). Impact of landslides and innovative landslide-mitigation measures on the natural environment. International Conference on Slope Engineering, Hong Kong, China, December 8-10, 2003. Keynote address, Proceedings 29. [Online] Available here [Accessed on 7 November 2013]
- Varnes, D.J. and the International Association of Engineering Geology Commission on Landslides and Other Mass Movements (1984). Landslide hazard zonation: A review of principles and practice. Natural Hazards, vol.3, Paris, France. UNESCO, 63p. [Online] Available here [Accessed on 7 November 2013]
This FAQ updated on 12 Nov 2013 by the EU FP-7 LAMPRE project.