Antecedent drainage is common on most
continents and it has played a major role in influencing the routes connecting cities.
The gaps
that rivers seem to cut across mountains and upland ridges are often produced by antecedent rivers.
Thus the gaps used by rivers in the rim of the London Basin and the Paris Basin are antecedent rivers, as are
those that cut in to the Appalachian mountains of North America, most spectacularly, the Delaware and Cumberland Gaps.