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- Seabed_gouging_by_ice abstract "Seabed gouging by ice is a process that occurs when floating ice features (typically icebergs and sea ice ridges) drift into shallower areas and their keel comes into contact with the seabed. As they keep drifting, they produce long, narrow furrows most often called gouges, or scours. This phenomenon is common in offshore environments where ice is known to exist. Although it also occurs in rivers and lakes, it appears to be better documented from oceans and sea expanses, as suggested by recent reviews.Seabed scours produced via this mechanism should not be confused with strudel scours. These results from spring run-off water flowing onto the surface of a given sea ice expanse, which eventually drains away through cracks, seal breathing holes, etc. The resulting turbulence is strong enough to carve a depression into the seabed. Seabed scouring by ice should also be distinguished from another scouring mechanism: the erosion of the sediments around a structure due to water currents, a well known issue in ocean engineering and river hydraulics – see bridge scour.".
- Seabed_gouging_by_ice thumbnail SeabedScouringByIce1.svg?width=300.
- Seabed_gouging_by_ice wikiPageExternalLink %28ASCE%291532-3641%282007%297%3A3%28206%29)..
- Seabed_gouging_by_ice wikiPageExternalLink m162p001.pdf.
- Seabed_gouging_by_ice wikiPageExternalLink Abstract.cfm?cat_no=2232s)..
- Seabed_gouging_by_ice wikiPageExternalLink S0165232X11001091)..
- Seabed_gouging_by_ice wikiPageID "1452030".
- Seabed_gouging_by_ice wikiPageRevisionID "605195667".
- Seabed_gouging_by_ice hasPhotoCollection Seabed_gouging_by_ice.
- Seabed_gouging_by_ice subject Category:Glaciology.
- Seabed_gouging_by_ice subject Category:Oceanography.
- Seabed_gouging_by_ice subject Category:Sea_ice.
- Seabed_gouging_by_ice comment "Seabed gouging by ice is a process that occurs when floating ice features (typically icebergs and sea ice ridges) drift into shallower areas and their keel comes into contact with the seabed. As they keep drifting, they produce long, narrow furrows most often called gouges, or scours. This phenomenon is common in offshore environments where ice is known to exist.".
- Seabed_gouging_by_ice label "Affouillement des fonds marins par la glace".
- Seabed_gouging_by_ice label "Seabed gouging by ice".
- Seabed_gouging_by_ice sameAs Affouillement_des_fonds_marins_par_la_glace.
- Seabed_gouging_by_ice sameAs m.052p7q.
- Seabed_gouging_by_ice sameAs Q2826098.
- Seabed_gouging_by_ice sameAs Q2826098.
- Seabed_gouging_by_ice wasDerivedFrom Seabed_gouging_by_ice?oldid=605195667.
- Seabed_gouging_by_ice depiction SeabedScouringByIce1.svg.
- Seabed_gouging_by_ice isPrimaryTopicOf Seabed_gouging_by_ice.
