Onlap

{{Short description|Geological phenomenon}} '''Onlap''' or ''overlap'' is the geological phenomenon of successively wedge-shaped younger rock strata extending progressively further across an erosion surface cut in older rocks. It is generally associated with a marine transgression. It is a more general term than ''overstep'', in which the younger beds overlap onto successively older beds.<ref>{{cite book |editor1-last=Jackson |editor1-first=Julia A. |title=Glossary of geology. |date=1997 |publisher=American Geological Institute |location=Alexandria, Virginia |isbn=0922152349 |edition=Fourth |chapter=onlap}}</ref> The opposite is '''offlap''', in which each younger rock bed pinches out short of the full extent of the underlying older bed, typically due to a marine regression.{{sfn|Jackson|1997|loc="offlap"}}

== References == {{reflist}}

Category:Stratigraphy

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