Ice foot: Difference between revisions
From Glossary of Meteorology
imported>Perlwikibot (Created page with " {{TermHeader}} {{TermSearch}} <div class="termentry"> <div class="term"> == ice foot == </div> <div class="definition"><div class="short_definition">Sea ice firmly...") |
imported>Perlwikibot No edit summary |
||
| Line 9: | Line 9: | ||
</div> | </div> | ||
<div class="definition"><div class="short_definition">[[Sea ice]] firmly frozen to the shore at the high-tide line and unaffected by [[tide]].</div><br/> <div class="paragraph">This type of [[fast ice]] is formed by the [[freezing]] of [[seawater]] during [[ebb tide]] and of spray. It is separated from the floating sea ice by a [[tide crack]]; in many areas it offers a fairly level, continuous route for surface travel.</div><br/> </div> | <div class="definition"><div class="short_definition">[[sea ice|Sea ice]] firmly frozen to the shore at the high-tide line and unaffected by [[tide]].</div><br/> <div class="paragraph">This type of [[fast ice]] is formed by the [[freezing]] of [[seawater]] during [[ebb tide]] and of spray. It is separated from the floating sea ice by a [[tide crack]]; in many areas it offers a fairly level, continuous route for surface travel.</div><br/> </div> | ||
</div> | </div> | ||
Latest revision as of 16:11, 25 April 2012
ice foot
This type of fast ice is formed by the freezing of seawater during ebb tide and of spray. It is separated from the floating sea ice by a tide crack; in many areas it offers a fairly level, continuous route for surface travel.
