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    1. European Landslide Expert Group
    1. Inventories in Europe


    A landslide is the gravitational movement of a mass of rock, earth or debris down a slope. Landslides are usually classified on the basis of the material involved (rock, debris, earth, mud) and the type of movement (fall, topple, avalanche, slide, flow, spread). Thus, the generic term landslide also refers to mass movements such as rock falls, mudslides and debris flows. Volcanic mudflows and debris flows are also called lahars. .

    Shallow landslides usually involve only the soil layer and upper regolith zone, while deep-seated landslides additionally involve bedrock at higher depth. Landslide volume can vary from some tens of cubic metres to several cubic kilometres for giant landslides, while landslide speed may range from a few centimetres per year for slow-moving landslides to tens of kilometres per hour for fast, highly destructive landslides. According to the state of activity or movement, existing landslides can be classified as active, dormant (potentially reactivated) or inactive (often relict or fossil).

    Landslides are generally induced when the shear stress on the slope material exceeds the material’s shear strength. The occurrence and reactivation of landslides is conditioned by a number of terrain and geo-environmental factors related to slope gradient and morphology, bedrock and soil properties, weathering conditions, jointing and structure, land cover/use, surface and ground water flow, etc. 

    Landslides can be triggered by natural physical processes such as heavy or prolonged rainfall, earthquakes, volcanic eruptions, rapid snow melt, slope undercutting by rivers or sea waves and permafrost thawing. They can also be triggered by man-made activities such as slope excavation and loading (e.g. road and buildings construction, open-pit mining and quarrying), land use changes (e.g. deforestation), rapid reservoir drawdown, irrigation, blasting vibrations, water leakage from utilities, etc, or by any combination of natural and/or man-induced processes.

    Landslide in Veneto
    Tessina landslide in north-east Italy


    Landslides are a major hazard in most mountainous and hilly regions as well as in steep river banks and coastlines. Their impact depends largely on their size and speed, the elements at risk in their path and the vulnerability of these elements. Every year landslides cause fatalities and result in large damage to infrastructure (roads, railways, pipelines, artificial reservoirs, etc.) and property (buildings, agricultural land, etc.).

    Large landslides in mountainous areas can result in landslide dams blocking river courses. These natural dams cause valley inundation upstream and can be subsequently breached by lake water pressure, hence generating deadly flash floods or debris flows downstream. Submarine and large coastal cliff landslides can trigger tsunami, as can landslides in lake and reservoir shores.

    Landslides can also affect mine waste tips and tailings dams and landfills, causing fatalities and contaminating soils and surface and ground water.

    In areas affected by landslides, these are a major source of soil erosion and sediment yield to valleys and rivers, and hence of reservoir silting.

    It should be noted that most statistics on natural disasters underestimate the impacts from landslides as they often do not separate them from other triggering or concurrent natural hazards such as storms, floods or earthquakes.

    Landslides in Europe

    Landslide occurrence

    Landslides occur in many different geological and environmental settings across Europe. For example, large rockfalls, rockslides, rock avalanches and debris flows dominate in the Alps and steep slopes in other mountain ranges; slides and flows abound in flysch belts of Slovakia, Czech Republic, Poland, Slovenia, Italy, Spain, France and other countries; slides of various types are numerous on cliffs and steep slopes in Southern and Eastern England’s coast and Bulgaria’s Northern Black Sea coast; shallow slides and mudflows occur on Ireland’s peat slopes; slides and lateral spreads do as well on gentle slopes in so-called quick clays in Sweden and Norway; flows and slides also typically occur in clay-rich sediments and sedimentary sequences in Cenozoic basins as well as on river banks, etc.

    Intense and/or long-lasting rainfall represents the most frequent trigger of landslides in continental Europe. However, earthquakes are also responsible for some landslides. Human activities are also the cause of many slope failures in infrastructure and built-up areas.

    Landslides are a major factor of landscape evolution in mountainous and hilly regions in Europe. In addition to causing extensive erosion and sediment yield in these regions, large landslides have been responsible for the creation of many lakes in the Alps and other mountain ranges by damming river courses. Examples of this include the lakes of Santa Croce, Antrona (formed in 1642), Alleghe (formed in 1771) and Scanno in Italy, Eibsee and Obersee in Germany, Blindsee in Austria, Vallon in France (formed in 1943), Lacul Rosu in Romania (formed in 1837), and Poschiavo, Klöntal, Derborence (formed in 1749), Sils, Silvaplana, Oeschinen and Davos in Switzerland. Most landslide dams, however, have often formed temporary lakes that have later breached the dam causing catastrophic flash floods and debris flows. Today, hills in some alpine valley bottoms are remnants of large deposits from giant landslides (e.g. from prehistoric rock avalanches with volumes even in excess of 1 km3 such as Flims, Sierre and Tamins in Switzerland, Köfels, Fernpass and Tschirgant in Austria, etc.). Many landslide-dammed lakes have been progressively filled with sediments, thus also modifying the valley environment. Unfortunately, the hazard of river damming from landslides still exists in these regions: outstanding examples are those of La Clapière and Séchilliene rockslides in the French Alps, whose potential movement acceleration threatens communities located downstream far from the unstable slopes. On the other hand, landslides in steep coastal areas including cliffs accelerate erosion and subsequent cliff retreat by sea waves.

    Giant subaerial landslides are not exclusive of the Alps. They have also occurred in prehistoric times in areas such as southern Crimea in Ukraine, Isle of Skye in UK, and especially in the Canary Islands, Spain. In the latter, a number of huge debris avalanches entered the ocean triggering tsunami. Evidence of large tsunami are also found in Scotland and other coastal areas bordering the Norwegian Sea, mainly attributed to the Storegga submarine megaslide (ca. 3,500 km3) off the west coast of Norway. In the Mediterranean, landslide-triggered tsunami have been observed dominantly in the Corinth Gulf, Greece, and the Aeolian Islands, Italy. Recent examples include the local tsunami caused by the collapse of the Nice airport embankment in 1979 and the small to moderate tsunami produced by a landslide on a Stromboli Island flank in 2002.

    Nowadays, population growth and expansion into landslide-prone areas is raising landslide risk in Europe. In addition, an increase of landslides associated to extreme rainfall events is expected in the future due to climate change.

    Major historic landslide disasters

    There is a long record of landslide disasters in historical and recent times in Europe causing many fatalities and high economic losses. Major disasters include, among others, those of Goldau (1806), Elm (1881) and Gondo (2000) in Switzerland; Piuro (1618), Antronapiana (1642), Roccamontepiano (1765), Monte Antelao (1814, 1925), Vajont (nearly 2000 killed by reservoir wave caused by man-induced landslide in 1963) and, more recently, Valpola (1987), the multi-landslide events in Piedmont region (1994), Sarno and Quindici (1998), Messina (2009), and the train accident at Laces (2010), all in Italy; Granier (1248) and Plateau d’Assy (1970) in France; Felanitx (1844), Azagra (1874) and Granada province (earthquake-triggered multi-landslide event, 1884) in Spain; Mount Dobratsch (1348) in Austria; Getå (1918) and Tuve (1977) in Sweden; Verdalen (1893) and landslide-triggered local tsunami at Loen (1905, 1936) and Tafjord (1934) in Norway.

    In addition, landslides occurring in mine waste tips and tailings dams have been the origin of the catastrophes of Sgorigrad, Bulgaria (1966), Aberfan (1966) in Wales, UK, and Stava (1985) in Trento, Italy.

    Lessons learnt from the management of a number of landslide disasters occurred in Europe in the 1990s and early 2000s are reported here

    Landslides and the EU Soil Thematic Strategy

    Landslides are one of the soil threats considered in the EU Thematic Strategy for Soil Protection and the related Proposal for a Soil Framework Directive. The Strategy calls for actions and means for the protection and sustainable use of soils as a physical platform on which human activities are developed. The proposed Directive, in turn, intended to be the Strategy implementing tool. This would mainly require to identify landslide and other soil threat risk areas in the European Union, set risk reduction targets for those areas and establish programmes of measures by Member States to achieve them.

    On 13 February 2012 the European Commission published the report The implementation of the Soil Thematic Strategy and ongoing activities (COM(2012) 46). The report provides an overview of the actions undertaken by the Commission to implement the four pillars of the Strategy, namely awareness raising, research, integration, and legislation. It also presents current and future challenges to ensure soil protection. The report includes a preliminary version of the later published landslide susceptibility map of the EU and neighbouring, countries produced by the European Landslide Expert Group coordinated by JRC.

    JRC activities

    The JRC provides scientific and technical support to the European Commission Services for the implementation of the EU Thematic Strategy for Soil Protection, both through its own work activities and in collaboration with national research organizations, mapping agencies and academia. Our main activities and expertise include harmonisation of methods for landslide mapping and zoning in Europe (inventory, susceptibility, hazard and risk) at various scales, development of satellite, airborne and ground-based remote sensing techniques for landslide mapping and long term monitoring, analysis of lessons learnt from management of past landslide disasters, and geospatial database creation and management. Find more information in the publications list (below).

    Collaborative activities with external partners are mainly carried out in various frameworks:

    • European Landslide Expert Group. Founded and coordinated by JRC, this group includes experts from a number of national geological surveys, national research institutes, and universities. The group is currently developing landslide inventories and models for landslide susceptibility assessment and mapping at European and national scales (see publications).
    • International Consortium on Landslides (ICL), an international non-governmental scientific organisation supported by UNESCO, UN/ISDR, FAO, WMO and intergovernmental programmes. ICL promotes and coordinates collaborative research and expertise, as well as capacity building, on landslide disaster risk reduction. 
      JRC is a member of the Board of Representatives of ICL and participates in its International Programme on Landslides (IPL) and other activities such as the organisation of World Landslide Forums. Its former JRC’s Institute of Environment and Sustainability (IES) was awarded the status of World Centre of Excellence on Landslide Disaster Reduction for the period 2011-2014 in the field of research on landslide risk management harmonisation in support to European Union policy making.
    • EU Framework Programme research projects, e.g. the recent one SAFELAND and previous landslide-related projects GALAHAD, MUSCL, RUNOUT, ENVASSO and RAMSOIL.
    • European Centre on Geomorphological Hazards (CERG), a specialized research network of the Council of Europe’s EUR-OPA Major Hazards Agreement co-operation platform.
    • Collaboration with EuroGeoSurveys (EGS) Earth Observation and Geohazards Expert Group.

    European Landslide Susceptibility Map version 1 (ELSUS1000 v1)

    N.B. This former version of ELSUS has been superseded by ELSUS v2 and has been removed from ESDAC.

    European Landslide Susceptibility Map version 2 (ELSUS v2)

    ELSUS v2 shows levels of spatial probability of generic landslide occurrence at continental scale. It covers all European Union member states except Malta, and several neighbouring countries. The map has been produced by regionalizing the study area based on elevation and climatic conditions, followed by spatial multi-criteria evaluation modelling using pan-European slope angle, shallow sub-surface lithology, and land cover spatial datasets as the main landslide conditioning factors. In addition, the location of over 149,000 landslides across Europe, provided by various national organizations or collected by the authors, has been used for model calibration and map validation. Additional information is given in both the metadata and the references below.

    Compared with the previous version ELSUS1000 v1, ELSUS v2 provides larger geographical coverage, higher spatial resolution and higher prediction model performance.

    The map has been produced jointly by Bundesanstalt für Geowissenschaften und Rohstoffe (BGR, Hannover, Germany), Istituto di Ricerca per la Protezione Idrogeologica (CNR-IRPI, Perugia, Italy), Institut de Physique du Globe de Strasbourg (CNRS-EOST, Strasbourg, France), and the Joint Research Centre (JRC, Ispra, Italy), as part of the collaborative work of the European Landslide Expert Group and the European Centre on Geomorphological Hazards (CERG)  in support of the EU Thematic Strategy for Soil Protection.

    The landslide susceptibility map is available to download together with ancillary maps including confidence level of the classified landslide susceptibility, climate-physiographic regions, slope angle, lithology, and land cover. ELSUS v2 is to be viewed at scales up to 1:200,000 and should not be used to deduce local information on landslide susceptibility.

    Title: European Landslide Susceptibility Map version 2 (ELSUS v2)
    Description: The map shows landslide susceptibility levels at continental scale, derived from heuristic-statistical modelling of main landslide conditioning factors using also landslide location data
    Spatial coverage: All European Union member states except Malta, in addition to Albania, Andorra, Bosnia and Herzegovina, Croatia, FYR Macedonia, Iceland, Kosovo, Liechtenstein, Montenegro, Norway, San Marino, Serbia, and Switzerland
    Cell size: 200 m
    Format: Esri ASCII Grid
    Map datum, projection: ETRS89, Lambert Azimuthal Equal Area 
    Landslide susceptibility coding: 0 = no data; 1 = very low; 2 = low; 3 = moderate; 4 = high; 5 = very high
    Files: elsus_v2.asc and ancillary files
    Ancillary datasets: Confidence Level Map of ELSUS v2, Climate-Physiographic regions, Slope Angle, Lithology, and Land Cover
    Authoring organisations: BGR, CNR-IRPI, CNRS-EOST and EC-JRC.D
    Release date: 12 February 2018

    Contact: Javier Hervas, Panos Panagos (EC-JRC.D), Andreas Günther (BGR)

    (note: Dr. Günther kindly agreed to have his name as contact point on this website)



    To get access to the spatial datasets and associated metadata, please compile the Request form; instructions on how to download the data will then follow.




    Contact Point

    Javier Hervas, Panos Panagos


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    Title: European Landslide Susceptibility Map version 2 (ELSUS v2)
    Resource Type: Datasets, Soil Threats Data
    Registration requested: Request Form
    Year: 2018