Post-glacial rebound: Difference between revisions
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'''Post-glacial rebound''' (sometimes called '''continental rebound''', '''isostatic rebound''' or '''isostatic adjustment''') is the rise of land masses that were depressed by the huge weight of ice sheets during the last [[ice age]], through a process known as '''isostatic depression'''. It affects northern Europe, especially [[Scotland]] and [[ |
'''Post-glacial rebound''' (sometimes called '''continental rebound''', '''isostatic rebound''' or '''isostatic adjustment''') is the rise of land masses that were depressed by the huge weight of ice sheets during the last [[ice age]], through a process known as '''isostatic depression'''. It affects northern Europe, especially [[Scotland]] and [[Scandinavia]], [[Siberia]] and [[Canada]]. |
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Revision as of 19:44, 15 December 2004
Post-glacial rebound (sometimes called continental rebound, isostatic rebound or isostatic adjustment) is the rise of land masses that were depressed by the huge weight of ice sheets during the last ice age, through a process known as isostatic depression. It affects northern Europe, especially Scotland and Scandinavia, Siberia and Canada.
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