Subaerial unconformity

In geology, a subaerial unconformity is a surface that displays signs of erosion by processes that commonly occur on the surface.[1] These processes generating the subaerial unconformity can include wind degradation, pedogenesis, dissolution processes such as karstification as well as fluvial processes such as fluvial erosion, bypass and river rejuvenation.[2]

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  2. ^ Cite error: The named reference catuneanu was invoked but never defined (see the help page).