WFS2.0.01.0.01.1.02.0.0text/xmlServiceIdentificationServiceProviderOperationsMetadataFeatureTypeListFilter_Capabilitiesapplication/gml+xml; version=3.2resultshitsapplication/gml+xml; version=3.2GML2KMLSHAPE-ZIPapplication/jsonapplication/vnd.google-earth.kml xmlapplication/vnd.google-earth.kml+xmlcsvgml3gml32jsontext/csvtext/javascripttext/xml; subtype=gml/2.1.2text/xml; subtype=gml/3.1.1text/xml; subtype=gml/3.2nonelocalFALSE1000000nonelocalapplication/gml+xml; version=3.2urn:ogc:def:queryLanguage:OGC-WFS::WFSQueryExpressionALLSOMEresultshitsapplication/gml+xml; version=3.2GML2KMLSHAPE-ZIPapplication/jsonapplication/vnd.google-earth.kml xmlapplication/vnd.google-earth.kml+xmlcsvgml3gml32jsontext/csvtext/javascripttext/xml; subtype=gml/2.1.2text/xml; subtype=gml/3.1.1text/xml; subtype=gml/3.2nonelocalapplication/gml+xml; version=3.2ALLSOMETRUETRUETRUETRUETRUETRUEFALSEFALSETRUETRUETRUETRUEFALSETRUEFALSEwfs:Querywfs:StoredQueryepos:Arctic_deposits_WGS84The Euro-Mediterranean Submarine landSlide database (EMSS21) displays information collected from both the literature and geophysical records. Data from the literature is collected from georeferenced map figures, from which the outline of the landslide deposit and the landslide scar have been digitized. Most information such as age, volume, typology, inferred trigger mechanism and relationship to fluid flow features and metadata is extracted from the relevant article. Area of the deposit and landslide runout is determined from the digitized polygons and polylines, volume (if not available) is determined from area and mean thickness. If the latter is not available, the volume is determined from the Area-Volume relationship for landslides where volume has already been determined. When the dat originates directly from geophysical records the outline and scars have been determined from geomorphological interpretation of swath bathymetric maps and interpretation of submarine landslides on a variety of seismic records. In such instances, age information originates from a variety of methods presenting a wide range of accuracies, from radiometric dating to well-seismic correlation as well as ages inferred from mean sedimentation rates. In many instances, landslides identified in the literature are dated with an age epoch only.featuresArctic_deposits_WGS84urn:ogc:def:crs:EPSG::4326-1.064834713935852 61.8853683471679733.170166015625 84.1023941040039epos:Demarcaciones_Marinas_20220909_ModeloDatosINSPIREDemarcaciones Marinas MITECOfeaturesDemarcaciones_Marinas_20220909_ModeloDatosINSPIREurn:ogc:def:crs:EPSG::4326-21.895280499995817 24.5887327983274386.300000000000139 46.87887049779749test:Depositsfeaturesurn:ogc:def:crs:EPSG::4326-24.60923194885254 22.8983821868896539.13383102416992 77.60060119628906epos:Deposits_EMSS25featuresurn:ogc:def:crs:EPSG::4326-24.293672561645508 23.169185638427734131.8426971435547 83.9924087524414test:Deposits_points_layerfeaturesurn:ogc:def:crs:EPSG::432627.69261699174312 40.835719652647228.64249724726731 42.1692693202056epos:Deposits_points_layer_EMSS25featuresurn:ogc:def:crs:EPSG::4326-2.525486463330207 36.6107679555612328.919579594861954 42.1692693202056epos:Med_depositsThe Euro-Mediterranean Submarine landSlide database (EMSS21) displays information collected from both the literature and geophysical records. Data from the literature is collected from georeferenced map figures, from which the outline of the landslide deposit and the landslide scar have been digitized. Most information such as age, volume, typology, inferred trigger mechanism and relationship to fluid flow features and metadata is extracted from the relevant article. Area of the deposit and landslide runout is determined from the digitized polygons and polylines, volume (if not available) is determined from area and mean thickness. If the latter is not available, the volume is determined from the Area-Volume relationship for landslides where volume has already been determined. When the dat originates directly from geophysical records the outline and scars have been determined from geomorphological interpretation of swath bathymetric maps and interpretation of submarine landslides on a variety of seismic records. In such instances, age information originates from a variety of methods presenting a wide range of accuracies, from radiometric dating to well-seismic correlation as well as ages inferred from mean sedimentation rates. In many instances, landslides identified in the literature are dated with an age epoch only.featuresMed_depositsurn:ogc:def:crs:EPSG::4326-13.480091094970703 30.43313598632812539.078495025634766 44.666866302490234epos:Med_scarsThe Euro-Mediterranean Submarine landSlide database (EMSS21) displays information collected from both the literature and geophysical records. Data from the literature is collected from georeferenced map figures, from which the outline of the landslide deposit and the landslide scar have been digitized. Most information such as age, volume, typology, inferred trigger mechanism and relationship to fluid flow features and metadata is extracted from the relevant article. Area of the deposit and landslide runout is determined from the digitized polygons and polylines, volume (if not available) is determined from area and mean thickness. If the latter is not available, the volume is determined from the Area-Volume relationship for landslides where volume has already been determined. When the dat originates directly from geophysical records the outline and scars have been determined from geomorphological interpretation of swath bathymetric maps and interpretation of submarine landslides on a variety of seismic records. In such instances, age information originates from a variety of methods presenting a wide range of accuracies, from radiometric dating to well-seismic correlation as well as ages inferred from mean sedimentation rates. In many instances, landslides identified in the literature are dated with an age epoch only.featuresMed_scarsurn:ogc:def:crs:EPSG::4326-12.85317611694336 31.6081676483154332.36977767944336 44.84532928466797test:Scar_crownfeaturesScar_crownurn:ogc:def:crs:EPSG::4326-16.513839721679688 31.6073398590087937.501686096191406 45.008121490478516epos:Scar_crown_EMSS25The Euro-Mediterranean Submarine landSlide database (EMSS25) displays information collected from both the literature and geophysical records. Data from the literature is collected from georeferenced map figures, from which the outline of the landslide deposit and the landslide scar have been digitized. Most information such as age, volume, typology and metadata is extracted from the relevant article. Area of the deposit and landslide runout is determined from the digitized polygons and polylines, volume (if not available) is determined from area and mean thickness. If the latter is not available, the volume is determined from the Area-Volume relationship for landslides where volume has already been determined. When the data originates directly from geophysical records the outline and scars have been determined from geomorphological interpretation of swath bathymetric maps and interpretation of submarine landslides on a variety of seismic records. In such instances, age information originates from a variety of methods presenting a wide range of accuracies, from radiometric dating to well-seismic correlation as well as ages inferred from mean sedimentation rates. In many instances, landslides identified in the literature are dated with an age epoch only.featuresScar_crown_EMSS25urn:ogc:def:crs:EPSG::4326-20.0 25.2152233123779337.517276763916016 75.0test:Source_areafeaturesSource_areaurn:ogc:def:crs:EPSG::4326-16.518903732299805 31.54982757568359437.501712799072266 45.00840759277344epos:Source_area_EMSS25The Euro-Mediterranean Submarine landSlide database (EMSS25) displays information collected from both the literature and geophysical records. Data from the literature is collected from georeferenced map figures, from which the outline of the landslide deposit and the landslide scar have been digitized. Most information such as age, volume, typology and metadata is extracted from the relevant article. Area of the deposit and landslide runout is determined from the digitized polygons and polylines, volume (if not available) is determined from area and mean thickness. If the latter is not available, the volume is determined from the Area-Volume relationship for landslides where volume has already been determined. When the data originates directly from geophysical records the outline and scars have been determined from geomorphological interpretation of swath bathymetric maps and interpretation of submarine landslides on a variety of seismic records. In such instances, age information originates from a variety of methods presenting a wide range of accuracies, from radiometric dating to well-seismic correlation as well as ages inferred from mean sedimentation rates. In many instances, landslides identified in the literature are dated with an age epoch only.featuresSource_area_EMSS25urn:ogc:def:crs:EPSG::4326-20.0 25.2152233123779337.517276763916016 75.0epos:etris_geodatafeaturesetris_geodataurn:ogc:def:crs:EPSG::4326-173.32460021972656 -36.93227767944336143.11209106445312 40.91508483886719epos:etris_geodata_fragilityfeaturesetris_geodata_fragilityurn:ogc:def:crs:EPSG::4326-74.01188659667969 -36.93227767944336142.87648010253906 40.91508483886719epos:etris_geodata_vulnerabilityfeaturesetris_geodata_vulnerabilityurn:ogc:def:crs:EPSG::4326-72.938176 -36.546893119.87802 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