Nordereider
Coordinates: 54 ° 24 ′ 30 ″ N , 9 ° 0 ′ 0 ″ E
The Nordereider ( Danish : Nørre Ejder ) was a connection between the Eider and Hever , which was probably formed in the Second Marcellus Flood of 1362 and separated Eiderstedt from the mainland for over a century. It went from the area where Friedrichstadt is nowadays , between Eiderstedt (until 1489 still an island) on one side and Stapelholm , the episcopal district of Schwabstedt , and Lundenberg , an island separated from Nordstrand , into the North Sea, then called the West Sea .
In the course of time, the water had lost its breadth, as the right bank grew due to deposits. Eiderstedt had become land-tight in 1489 with the completion of the Dammkooges with Schwabstedt, whereby the remaining parts of the river quickly silted up and formed a number of fertile kays . The area north of the Büttelkoog was in the natural silting area of the old Treene and the priel streams of the Nordereider. Even today, the low-lying marshland points to the remains of the old arms of the north Eider.
Individual evidence
- ↑ Heinz Dargel: Uelvesbüll: From the local history , on: dargelo.de, accessed November 2, 2015
- ^ A b Niels Nikolaus Falck: Handbook of Schleswig-Holstein Private Law , Vol. 1, 1825, p. 307
- ↑ Dirk Meier: De Dam was logged between Eyderstede and Husum ... The dike in the 'Nordt Eyder' , Eiderstedt (Schleswig-Holstein), p. 237, on: kuestenarchaeologie.de, accessed November 2, 2015