Landslides in Greece - Europa · Elevation, land use, slope gradient, erosion, geotectonic zone,...
Transcript of Landslides in Greece - Europa · Elevation, land use, slope gradient, erosion, geotectonic zone,...
IGME LANDSLIDE DATABASE AND A IGME LANDSLIDE DATABASE AND A REVIEW OF HAZARD ZONATION IN REVIEW OF HAZARD ZONATION IN
GREECEGREECEByBy
Eleftheria PoyiadjiEleftheria PoyiadjiEngineering Geologist IGME Engineering Geologist IGME -- GreeceGreece
Member of EGS/WG Geohazards Member of EGS/WG Geohazards
InstituteInstitute of Geology and Mineral of Geology and Mineral ExplorationExploration(IGME) is the national geologigal survey of Greece (IGME) is the national geologigal survey of Greece and is the official geoscientific adviser of the and is the official geoscientific adviser of the government.government.
250 cases of landslides in 2.5 years250 cases of landslides in 2.5 yearsCreation of a database.Creation of a database.
Landslide consultancy Landslide consultancy projectprojectInstituteInstitute of Geology and Mineral of Geology and Mineral ExplorationExplorationCentral Union of MunicipalitiesCentral Union of Municipalities
Landslide databaseLandslide databaseAccess Access –– GISGIS
Data recorded:Data recorded:Geographic detailsGeographic details
Prefecture, municipality, year, season, coordinatesLocation
Elevation, land use, slope gradient, erosion, geotectonic zone, geological formation, lithological composition, hydrogeology, inclination of strata, thickenss of weathered zone, precipitation, manmade impact, groundwater level, seismic risk zone
Landslide dataLandslide data
Older history, type of movement, geometry, rate,
Landslide process
Triggering factor, causes, consequences, structures affected, proposed mitigation measurements, degree of compliance
Database includes mostly landslides that affect the Database includes mostly landslides that affect the urban environment, structures and lifelinesurban environment, structures and lifelines
The landslide database has been The landslide database has been included in geoincluded in geo--database ofdatabase of IGME IGME
Next step: Introduction of more than 2,000 reports on landslides (analogue)
Statistical analysis
A landslide hazard zonation map of Greece was A landslide hazard zonation map of Greece was produced in a scale of 1:500,000 according to the produced in a scale of 1:500,000 according to the number of landslides per 100Kmnumber of landslides per 100Km22
Methodology for the identification of Methodology for the identification of risk areasrisk areas
Factors Factors ““Driving forcesDriving forces””
They are related to the scope of risk They are related to the scope of risk mapping mapping –– different scalesdifferent scales
Risk zonation in urban areasRisk zonation in urban areasLarge scales (1:1,000)Large scales (1:1,000)
Multi hazard approachMulti hazard approach
Risk zonation in urban areasRisk zonation in urban areasLarge scales (1:1,000)Large scales (1:1,000)
Multi hazard approachMulti hazard approach
Risk zonation in urban areasRisk zonation in urban areasLarge scales (1:1,000)Large scales (1:1,000)
Multi hazard approachMulti hazard approach
Risk zonation in urban areasRisk zonation in urban areasLarge scales (1:1,000)Large scales (1:1,000)
Multi hazard approachMulti hazard approach
Risk zonation at national or european levelRisk zonation at national or european levelSmall scales (1:50,000, 1:100,000??)Small scales (1:50,000, 1:100,000??)
Common elements for the identification of Common elements for the identification of areas at risk of landslidesareas at risk of landslides
Directive of the European parliament and of the Directive of the European parliament and of the counsil counsil –– COM(2006) 232 finalCOM(2006) 232 final
Common elements for the identification of Common elements for the identification of areas at risk of landslidesareas at risk of landslides
Directive of the European parliament and of the Directive of the European parliament and of the counsil counsil –– COM(2006) 232 finalCOM(2006) 232 final
Seismic riskClimate
Land useLand cover
TopographyBedrock
Occurrence/density of existing landslides
Soil typological unit (STU) (soil type)
More driving forcesMore driving forces
Relevant orientation of strata relative to slope orientation *
Manmade factors
erosionDeforestation
PrecipitationGround water
* Applied only in large scale
CONCLUSIONSCONCLUSIONS
Common MethodologyCommon MethodologyFactors are related to:Factors are related to:
scalescalescopescope
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