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- Q2826098 subject Q7066307.
- Q2826098 subject Q8723989.
- Q2826098 subject Q8791517.
- Q2826098 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.Seabed scours produced via this mechanism should not be confused with strudel scours. These result 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.".
- Q2826098 thumbnail SeabedScouringByIce1.svg?width=300.
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- Q2826098 wikiPageWikiLink Q7066307.
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- Q2826098 wikiPageWikiLink Q8723989.
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- Q2826098 wikiPageWikiLink Q8791517.
- Q2826098 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.".
- Q2826098 label "Seabed gouging by ice".
- Q2826098 depiction SeabedScouringByIce1.svg.
