Seabed gouging by ice
id:
seabed-gouging-by-ice-301-10506543
title:
Seabed gouging by ice
text:
Seabed gouging by ice is a process that occurs when floating ice features 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
brand slug:
wiki
category slug:
encyclopedia
description:
Outcome of the interaction between drifting ice and the seabed
original url:
https://en.wikipedia.org/wiki/Seabed_gouging_by_ice
date created:
date modified:
2024-01-05T12:13:41Z
main entity:
{"identifier":"Q2826098","url":"https://www.wikidata.org/entity/Q2826098"}
image:
{"content_url":"https://upload.wikimedia.org/wikipedia/commons/c/c1/SeabedScouringByIce1.svg","width":455,"height":305}
fields total:
13
integrity:
15