Glacial rebound — the rise or fall of land masses that were depressed by the huge weight of ice sheets during the last glacial period — explains differences in relative sea levels along the English coast, according to a new study.
Glacial rebound — the rise or fall of land masses that were depressed by the huge weight of ice sheets during the last glacial period — explains differences in relative sea levels along the English coast, according to a new study.
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