Difference between revisions of "Dictionary:Retrogradation"

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Landward movement of the shoreline when the rate of sediment supply is less than can be accommodated by the rate of rise of relative sea level. As a consequence the distal toes of successively younger parasequences move landward. See Figure [[Special:MyLanguage/Dictionary:Fig_D-6|D-6]].
 
Landward movement of the shoreline when the rate of sediment supply is less than can be accommodated by the rate of rise of relative sea level. As a consequence the distal toes of successively younger parasequences move landward. See Figure [[Special:MyLanguage/Dictionary:Fig_D-6|D-6]].
 
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Latest revision as of 15:03, 27 July 2017

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Landward movement of the shoreline when the rate of sediment supply is less than can be accommodated by the rate of rise of relative sea level. As a consequence the distal toes of successively younger parasequences move landward. See Figure D-6.