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Statements

Subject Item
dbr:Tidal_scour
rdf:type
yago:PhysicalEntity100001930 yago:GeologicalProcess113486838 yago:Process100029677 yago:NaturalProcess113518963 yago:WikicatGeologicalProcesses
rdfs:label
Tidal scour
rdfs:comment
Tidal scour is “sea-floor erosion caused by strong tidal currents resulting in the removal of inshore sediments and formation of deep holes and channels”. Examples of this hydrological process can be found globally. Two locations in the United States where tidal scour is the predominant shaping force is the San Francisco Bay and the Elkhorn Slough. Tidal force can also contribute to bridge scour.
foaf:depiction
n14:Moss_Landing_California_aerial_view.jpg
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dbc:Geology dbc:Geomorphology dbc:Geological_processes
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dbr:Benthos dbr:Barrier_island dbr:Estuary dbc:Geomorphology dbr:Bathymetry dbr:Agricultural_runoff dbr:San_Francisco_Bay dbr:Geomorphology dbr:Cross-sectional_study dbr:Moss_Landing,_California dbr:Eelgrass dbr:United_States dbr:Elkhorn_Slough dbr:Tidal_currents dbr:Lidar dbc:Geological_processes dbr:River_delta dbr:Grain_size dbr:Sediment_transport dbr:Anthropogenic_effects dbr:Sonar dbr:Bridge_scour dbc:Geology dbr:Erosion n21:Moss_Landing_California_aerial_view.jpg
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dbo:abstract
Tidal scour is “sea-floor erosion caused by strong tidal currents resulting in the removal of inshore sediments and formation of deep holes and channels”. Examples of this hydrological process can be found globally. Two locations in the United States where tidal scour is the predominant shaping force is the San Francisco Bay and the Elkhorn Slough. Tidal force can also contribute to bridge scour.
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dbr:Erosion
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