Isostatic adjustment: Difference between revisions
From Glossary of Meteorology
imported>Perlwikibot (Created page with " {{TermHeader}} {{TermSearch}} <div class="termentry"> <div class="term"> == isostatic adjustment == </div> <div class="definition"><div class="short_definition">The mo...") |
imported>Perlwikibot No edit summary |
||
Line 9: | Line 9: | ||
</div> | </div> | ||
<div class="definition"><div class="short_definition">The movement of the solid part of the earth until it is in balance; <br/>''also called'' isostatic compensation.</div><br/> <div class="paragraph">The prime example of isostatic adjustment is the continents | <div class="definition"><div class="short_definition">The movement of the solid part of the earth until it is in balance; <br/>''also called'' isostatic compensation.</div><br/> <div class="paragraph">The prime example of isostatic adjustment is the continents "floating" on the denser parts of the crust.</div><br/> </div> | ||
</div> | </div> | ||
Latest revision as of 14:31, 20 February 2012
isostatic adjustment
The movement of the solid part of the earth until it is in balance;
also called isostatic compensation.
also called isostatic compensation.
The prime example of isostatic adjustment is the continents "floating" on the denser parts of the crust.