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- Tideline abstract "A tideline refers to where two currents in the ocean converge. Driftwood, floating seaweed, foam, and other floating debris may accumulate, forming sinuous lines called tidelines (although they generally have nothing to do with the tide).There are four mechanisms that can cause tidelines to form: Where one body of water is sinking beneath or riding over top of the surface layer of another body of water (somewhat similar in mechanics to subduction of the earth plates at continental margins). These types of tidelines are often found where rivers enter the ocean. Along the margins of back-eddies. Convergence zones associated with internal gravity waves. Along adjacent cells formed by wind currents.".
- Tideline wikiPageID "6828483".
- Tideline wikiPageLength "1191".
- Tideline wikiPageOutDegree "10".
- Tideline wikiPageRevisionID "661522626".
- Tideline wikiPageWikiLink Category:Physical_oceanography.
- Tideline wikiPageWikiLink Category:Tides.
- Tideline wikiPageWikiLink Flotsam,_jetsam,_lagan,_and_derelict.
- Tideline wikiPageWikiLink Flotsam_and_jetsam.
- Tideline wikiPageWikiLink Internal_gravity_waves.
- Tideline wikiPageWikiLink Internal_wave.
- Tideline wikiPageWikiLink Langmuir_circulation.
- Tideline wikiPageWikiLink Ocean.
- Tideline wikiPageWikiLink Ocean_circulation.
- Tideline wikiPageWikiLink Ocean_current.
- Tideline wikiPageWikiLink Oceanography.
- Tideline wikiPageWikiLink Tide.
- Tideline wikiPageWikiLinkText "Tideline".
- Tideline wikiPageWikiLinkText "tideline".
- Tideline hasPhotoCollection Tideline.
- Tideline wikiPageUsesTemplate Template:About.
- Tideline wikiPageUsesTemplate Template:Physical_oceanography.
- Tideline subject Category:Physical_oceanography.
- Tideline subject Category:Tides.
- Tideline type Geophysic.
- Tideline comment "A tideline refers to where two currents in the ocean converge. Driftwood, floating seaweed, foam, and other floating debris may accumulate, forming sinuous lines called tidelines (although they generally have nothing to do with the tide).There are four mechanisms that can cause tidelines to form: Where one body of water is sinking beneath or riding over top of the surface layer of another body of water (somewhat similar in mechanics to subduction of the earth plates at continental margins).".
- Tideline label "Tideline".
- Tideline sameAs m.0grc18.
- Tideline sameAs Q7800849.
- Tideline sameAs Q7800849.
- Tideline wasDerivedFrom Tideline?oldid=661522626.
- Tideline isPrimaryTopicOf Tideline.