GeoNodeFeatureCatalogue Generic Feature Catalogue Generic Feature Catalogue 1.0 2016-01-11 Organization Name pointOfContact geonode:Submarine_Canyon The aim of this study is to assess the global occurrence of large submarine canyons to provide context and guidance for discussions regarding canyon occurrence, distribution, geological and oceanographic significance and conservation. Based on an analysis of the ETOPO1 data set, this study has compiled the first inventory of 5849 separate large submarine canyons in the world ocean. Active continental margins contain 15% more canyons (2586, equal to 44.2% of all canyons) than passive margins (2244, equal to 38.4%) and the canyons are steeper, shorter, more dendritic and more closely spaced on active than on passive continental margins. This study confirms observations of earlier workers that a relationship exists between canyon slope and canyon spacing (increased canyon slope correlates with closer canyon spacing). The greatest canyon spacing occurs in the Arctic and the Antarctic whereas canyons are more closely spaced in the Mediterranean than in other areas. River-associated, shelf-incising canyons are more numerous on active continental margins (n = 119) than on passive margins (n = 34). They are most common on the western margins of South and North America where they comprise 11.7% and 8.6% of canyons respectively, but are absent from the margins of Australia and Antarctica. Geographic areas having relatively high rates of sediment export to continental margins, from either glacial or fluvial sources operating over geologic timescales, have greater numbers of shelf-incising canyons than geographic areas having relatively low rates of sediment export to continental margins. This observation is consistent with the origins of some canyons being related to erosive turbidity flows derived from fluvial and shelf sediment sources. Other workers have shown that benthic ecosystems in shelf-incising canyons contain greater diversity and biomass than non-incising canyons, and that ecosystems located above 1500 m water depth are more vulnerable to destructive fishing prac false Submarine Canyon fid 1 1 xsd:int the_geom 1 1 gml:MultiLineStringPropertyType LineSegs 1 1 xsd:long dend2_max 1 1 xsd:long low_height 1 1 xsd:long status 1 1 xsd:string can_per_km 1 1 xsd:double MarginType 1 1 xsd:string CanyonName 1 1 xsd:string Dist_bet_p 1 1 xsd:double dens_LWM 1 1 xsd:double sinuosity 1 1 xsd:double Group 1 1 xsd:string height_dif 1 1 xsd:double X 1 1 xsd:double class 1 1 xsd:long dend2_min 1 1 xsd:long slope_LWM 1 1 xsd:double sed_LWM 1 1 xsd:double Y 1 1 xsd:double dens_MAX 1 1 xsd:double slope_max 1 1 xsd:double sed_max 1 1 xsd:double hemisphere 1 1 xsd:string dens_MIN 1 1 xsd:double dend2_LWM 1 1 xsd:double Slope_min 1 1 xsd:double DENDper_ht 1 1 xsd:double sed_min 1 1 xsd:double Length_km 1 1 xsd:double DENDperkm2 1 1 xsd:double gt1500m 1 1 xsd:string top_height 1 1 xsd:long