Vlie
The former Zuiderzee (called Lake Flevo) drained into the North See through the Vlie.
It is often supposed that the old Roman name for the lake that later would become the Zuiderzee: Lacus Flevo, is etymologically related to the name "Vlie" and that perhaps Vlie was once the name of the entire lake and the big river that flowed out of it. In the 13th century large floods widened the estuary and destroyed much of the peat land behind, creating a continuous area of sand and mudflats connecting the sea to the enlarged inland lake and obscuring the flow of the river. When the Afsluitdijk was created, the old streambed from the river to the sea was obstructed. The construction of the Afsluitdijk caused a 19% increase of current velocity in Vliestroom.
In the Lex Frisonum the Vlie (Fli, or Flehi) is accepted as the boundary between the territory of the East and West Frisians.
References
- ^ Encyclopædia Britannica. Vol. 28 (11th ed.). 1911. p. 1049. .
- ^ Crosato, A.; Stive, M. J. F. (2000). "Morphology and Morphodynamics of the Wadden Sea". Delft Cluster Report Theme 3, Project "coast and Ecomorphology".