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http://geoserver4.d4science.org/geoserver/wcs?service=wcs&version=1.0.0&request=GetCoverage&coverage=tdme2d91f5dc5f84c278906006f28d2cb51&CRS=EPSG:4326&bbox=-180.0,-90.0,180.0,90.0&width=676&height=330&format=geotiff https://goo.gl/NkAw9V geo_fea_slope English UTF-8 Dataset dataset 2014-02-05 INSPIRE Metadata Implementing Rules: Technical Guidelines based on EN ISO 19115 and EN ISO 19119 V. 1.2 http://www.opengis.net/def/crs/EPSG/0/4326 0 Slope geomorphic feature layer c9c1d53a-f9d6-48f5-bf5a-4d27831a7728 Miles Macmillan-Lawler GRID-Arendal Miles.Macmillan-Lawler@grida.no Custodian The slope geomorphic feature layer represents the spatial extent of the slope areas of the worlds oceans based on interpretation of the SRTM30 plus v7 global bathymetry model. The layer is one of the 25 layers that make up the global seafloor geomorphic features map (Harris et.al. 2014). The slope is “the deepening sea floor out from the shelf edge to the upper limit of the continental rise, or the point where there is a general decrease in steepness” (IHO, 2008). In this study, the foot of slope was digitised manually at a nominal spatial scale of 1:500,000 in ArcGIS based on 100 m contours and 3D viewing. ArcGIS was used to highlight zones of abrupt changes in seabed gradient (contour spacing) which suggests the foot of slope in many areas. In areas where marginal plateaus abut the margin, the foot of slope was allowed to extend offshore to encompass the plateau feature, where a clear seaward dipping gradient was apparent. Otherwise the first significant decrease in gradient encountered in a seaward direction from the shelf break was selected as the foot of slope. Note our foot of slope locations are based only on bathymetric data and our interpretation is not intended to define the foot of slope under Article 76 of the 1982 United Nations Convention on the Law of the Sea, particularly in areas of geomorphologically complex, continent-ocean transition. Miles Macmillan-Lawler GRID-Arendal Miles.Macmillan-Lawler@grida.no Custodian The global seafloor geomorphic feature map is available for download from bluehabitats.org Other restrictions Vector English UTF-8 oceans -180.0 -76.516483 180.0 84.540813 WMS 1.1.0 WFS 1.1.0 WCS 1.0.0 http://geoserver.d4science.org/geoserver/wms?service=wms&version=1.1.0&request=GetMap&layers=W_mpa:geo_fea_slope&styles=&bbox=-180,-90,180,90&width=676&height=330&srs=EPSG:4326&crs=EPSG:4326&format=application/openlayers http://geoserver.d4science.org/geoserver/ows?service=WFS&version=1.0.0&request=GetFeature&typeName=W_mpa:geo_fea_slope&format=json http://geoserver.d4science.org/geoserver/wms?service=wms&version=1.1.0&request=GetMap&layers=W_mpa:geo_fea_slope&styles=&bbox=-180,-90,180,90&width=676&height=330&srs=EPSG:4326&crs=EPSG:4326&format=application/openlayers http://data.d4science.org/gis?scope=%252Fd4science.research-infrastructures.eu%252FgCubeApps&gis-UUID=c9c1d53a-f9d6-48f5-bf5a-4d27831a7728 This data was generated based on interpretation of the SRTM30 plus v7 global bathymetry model. The layer is one of the 25 layers that make up the global seafloor geomorphic features map (Harris et.al. 2014). geo_fea_shelf English UTF-8 Dataset dataset 2014-02-05 INSPIRE Metadata Implementing Rules: Technical Guidelines based on EN ISO 19115 and EN ISO 19119 V. 1.2 http://www.opengis.net/def/crs/EPSG/0/4326 0 Shelf geomorphic feature layer d7733bec-0ecd-4ff7-a4f1-f185032eb527 Miles Macmillan-Lawler GRID-Arendal Miles.Macmillan-Lawler@grida.no Custodian The shelf geomorphic feature layer represents the spatial extent of the shelf areas of the worlds oceans based on interpretation of the SRTM30 plus v7 global bathymetry model. The layer is one of the 25 layers that make up the global seafloor geomorphic features map (Harris et.al. 2014). The continental shelf is defined by IHO (2008)as “a zone adjacent to a continent (or around an island) and extending from the low water line to a depth at which there is usually a marked increase of slope towards oceanic depths”. The low-water mark is taken in this study as the 0 m depth contour. The shelf break (i.e. the line along which there is marked increase of slope at the seaward margin of a shelf) was digitised manually at a nominal spatial scale of 1:500,000 in ArcGIS based on 10 m, 50 m and 100 m contours, depending on the slope and bathymetric profile of the region. In most cases 100 m contours were sufficient at the selected scale of 1:500,000 to identify the shelf break. However, where there was a gradual break in slope over a broad area, more closely spaced contours were used. Floating ice shelves cover large sections of the Antarctic continental shelf and these areas were simply left blank. Miles Macmillan-Lawler GRID-Arendal Miles.Macmillan-Lawler@grida.no Custodian The global seafloor geomorphic feature map is available for download from bluehabitats.org Other restrictions Vector English UTF-8 oceans -180.0 -78.686972 180.0 84.207354 WMS 1.1.0 WFS 1.1.0 WCS 1.0.0 http://geoserver.d4science.org/geoserver/wms?service=wms&version=1.1.0&request=GetMap&layers=W_mpa:geo_fea_shelf&styles=&bbox=-180,-90,180,90&width=676&height=330&srs=EPSG:4326&crs=EPSG:4326&format=application/openlayers http://geoserver.d4science.org/geoserver/ows?service=WFS&version=1.0.0&request=GetFeature&typeName=W_mpa:geo_fea_shelf&format=json http://geoserver.d4science.org/geoserver/wms?service=wms&version=1.1.0&request=GetMap&layers=W_mpa:geo_fea_shelf&styles=&bbox=-180,-90,180,90&width=676&height=330&srs=EPSG:4326&crs=EPSG:4326&format=application/openlayers http://data.d4science.org/gis?scope=%252Fd4science.research-infrastructures.eu%252FgCubeApps&gis-UUID=d7733bec-0ecd-4ff7-a4f1-f185032eb527 This data was generated based on interpretation of the SRTM30 plus v7 global bathymetry model. The layer is one of the 25 layers that make up the global seafloor geomorphic features map (Harris et.al. 2014). geo_fea_troughs English UTF-8 Dataset dataset 2014-02-05 INSPIRE Metadata Implementing Rules: Technical Guidelines based on EN ISO 19115 and EN ISO 19119 V. 1.2 http://www.opengis.net/def/crs/EPSG/0/4326 0 Trough geomorphic feature layer 1e0c14c6-4719-42e8-a57f-d6c04cd02518 Miles Macmillan-Lawler GRID-Arendal Miles.Macmillan-Lawler@grida.no Custodian The trough geomorphic feature layer represents the spatial extent of the troughs of the worlds oceans based on interpretation of the SRTM30 plus v7 global bathymetry model. The layer is one of the 25 layers that make up the global seafloor geomorphic features map (Harris et.al. 2014). The IHO (IHO, 2008) definition of a trough is “a long depression of the sea floor characteristically flat bottomed and steep sided and normally shallower than a trench”. In this study we found that troughs are also commonly open at one end (i.e. not defined by closed bathymetric contours) and their broad, flat floors may exhibit a continuous gradient along a thalweg. Troughs may originate from glacial erosion processes or have formed through tectonic processes. In this study, glacial troughs incised into the shelf are a separate category; here we include all troughs not of a glacial origin, typically superimposed on the slope and/or abyssal base layers. Trenches that have been infilled with sediment may evolve into troughs, as appears to have occurred in troughs adjacent to North and South America, for example. Slumping on the sides of some troughs has formed a bridge across the trough, thereby dividing it into two separate sections (see “bridges” below). In this study all troughs were digitised by hand based on the interpretation of 100 m bathymetric contours. Miles Macmillan-Lawler GRID-Arendal Miles.Macmillan-Lawler@grida.no Custodian The global seafloor geomorphic feature map is available for download from bluehabitats.org Other restrictions Vector English UTF-8 oceans -180.0 -71.905139 180.0 89.049382 WMS 1.1.0 WFS 1.1.0 WCS 1.0.0 http://geoserver.d4science.org/geoserver/wms?service=wms&version=1.1.0&request=GetMap&layers=W_mpa:geo_fea_troughs&styles=&bbox=-180,-90,180,90&width=676&height=330&srs=EPSG:4326&crs=EPSG:4326&format=application/openlayers http://geoserver.d4science.org/geoserver/ows?service=WFS&version=1.0.0&request=GetFeature&typeName=W_mpa:geo_fea_troughs&format=json http://geoserver.d4science.org/geoserver/wms?service=wms&version=1.1.0&request=GetMap&layers=W_mpa:geo_fea_troughs&styles=&bbox=-180,-90,180,90&width=676&height=330&srs=EPSG:4326&crs=EPSG:4326&format=application/openlayers http://data.d4science.org/gis?scope=%25252Fd4science.research-infrastructures.eu%25252FgCubeApps&gis-UUID=1e0c14c6-4719-42e8-a57f-d6c04cd02518 This data was generated based on interpretation of the SRTM30 plus v7 global bathymetry model. The layer is one of the 25 layers that make up the global seafloor geomorphic features map (Harris et.al. 2014). geo_fea_terraces English UTF-8 Dataset dataset 2014-02-05 INSPIRE Metadata Implementing Rules: Technical Guidelines based on EN ISO 19115 and EN ISO 19119 V. 1.2 http://www.opengis.net/def/crs/EPSG/0/4326 0 Terrace geomorphic feature layer 5ea07cca-1696-40b4-bf40-3482b5e628ef Miles Macmillan-Lawler GRID-Arendal Miles.Macmillan-Lawler@grida.no Custodian The terrace geomorphic feature layer represents the spatial extent of the terraces of the worlds oceans based on interpretation of the SRTM30 plus v7 global bathymetry model. The layer is one of the 25 layers that make up the global seafloor geomorphic features map (Harris et.al. 2014). Terraces are “An isolated (or group of) relatively flat horizontal or gently inclined surface(s), sometimes long and narrow, which is (are) bounded by a steeper ascending slope on one side and by a steeper descending slope on the opposite side” (IHO, 2008). In this study terraces (broad steps) were calculated based on the gradient of the SRTM30_PLUS model. The SRTM30_PLUS model was masked using the slope feature layer (i.e. terraces we only mapped on the continental slope). Miles Macmillan-Lawler GRID-Arendal Miles.Macmillan-Lawler@grida.no Custodian The global seafloor geomorphic feature map is available for download from bluehabitats.org Other restrictions Vector English UTF-8 oceans -179.999938 -74.686809 179.999965 88.860097 WMS 1.1.0 WFS 1.1.0 WCS 1.0.0 http://geoserver.d4science.org/geoserver/wms?service=wms&version=1.1.0&request=GetMap&layers=W_mpa:geo_fea_terraces&styles=&bbox=-180,-90,180,90&width=676&height=330&srs=EPSG:4326&crs=EPSG:4326&format=application/openlayers http://geoserver.d4science.org/geoserver/ows?service=WFS&version=1.0.0&request=GetFeature&typeName=W_mpa:geo_fea_terraces&format=json http://geoserver.d4science.org/geoserver/wms?service=wms&version=1.1.0&request=GetMap&layers=W_mpa:geo_fea_terraces&styles=&bbox=-180,-90,180,90&width=676&height=330&srs=EPSG:4326&crs=EPSG:4326&format=application/openlayers http://data.d4science.org/gis?scope=%25252Fd4science.research-infrastructures.eu%25252FgCubeApps&gis-UUID=5ea07cca-1696-40b4-bf40-3482b5e628ef This data was generated based on interpretation of the SRTM30 plus v7 global bathymetry model. The layer is one of the 25 layers that make up the global seafloor geomorphic features map (Harris et.al. 2014). geo_fea_trenches English UTF-8 Dataset dataset 2014-02-05 INSPIRE Metadata Implementing Rules: Technical Guidelines based on EN ISO 19115 and EN ISO 19119 V. 1.2 http://www.opengis.net/def/crs/EPSG/0/4326 0 Trench geomorphic feature layer 2e5f7df1-aa2d-4901-8ad2-471b00c8b674 Miles Macmillan-Lawler GRID-Arendal Miles.Macmillan-Lawler@grida.no Custodian The trench geomorphic feature layer represents the spatial extent of the trenches of the worlds oceans based on interpretation of the SRTM30 plus v7 global bathymetry model. The layer is one of the 25 layers that make up the global seafloor geomorphic features map (Harris et.al. 2014). Trenches are “a long narrow, characteristically very deep and asymmetrical depression of the sea floor, with relatively steep sides” (IHO, 2008). Trenches are generally distinguished from troughs by their “V” shape in cross section (in contrast with flat-bottomed troughs). In this study trenches were mapped by selecting closed bathymetric contours that defined basins contained within the trench feature, and then joining the basin segments together by hand digitizing along more elevated sections. In this way, bridge features were also identified (as coinciding with infilled sections of trenches; see section on “bridges”). Miles Macmillan-Lawler GRID-Arendal Miles.Macmillan-Lawler@grida.no Custodian The global seafloor geomorphic feature map is available for download from bluehabitats.org Other restrictions Vector English UTF-8 oceans -180.0 -61.062679 180.0 55.526452 WMS 1.1.0 WFS 1.1.0 WCS 1.0.0 http://geoserver.d4science.org/geoserver/wms?service=wms&version=1.1.0&request=GetMap&layers=W_mpa:geo_fea_trenches&styles=&bbox=-180,-90,180,90&width=676&height=330&srs=EPSG:4326&crs=EPSG:4326&format=application/openlayers http://geoserver.d4science.org/geoserver/ows?service=WFS&version=1.0.0&request=GetFeature&typeName=W_mpa:geo_fea_trenches&format=json http://geoserver.d4science.org/geoserver/wms?service=wms&version=1.1.0&request=GetMap&layers=W_mpa:geo_fea_trenches&styles=&bbox=-180,-90,180,90&width=676&height=330&srs=EPSG:4326&crs=EPSG:4326&format=application/openlayers http://data.d4science.org/gis?scope=%25252Fd4science.research-infrastructures.eu%25252FgCubeApps&gis-UUID=2e5f7df1-aa2d-4901-8ad2-471b00c8b674 This data was generated based on interpretation of the SRTM30 plus v7 global bathymetry model. The layer is one of the 25 layers that make up the global seafloor geomorphic features map (Harris et.al. 2014).