Eider Canal conservation areas. Eider Canal The Eider Canal (also called the Schleswig-Holstein Canal) was an artificial waterway in southern Denmark (later northern Germany) which connected the North Sea with the Baltic Sea by way of the rivers Eider and Levensau. Constructed between 1777 and 1784, the Eider Canal was built to create a path for ships entering and exiting the Baltic that was shorter and less storm-prone than navigating around the Jutland peninsula. In the 1880s the canal was replaced by the enlarged Kiel Canal, which includes some of the Eider Canal's watercourse. The canal's watercourse followed the border between the
Geology of the Baltic Sea Silurian. At this time the Baltic sea basin and the East European Craton were part of a continent and tectonic plate known as Baltica. Baltica collided with the continent Laurentia in the Late Silurian and Early Devonian. This caused compression in the basin in a north-west to south-east direction. This collision further led to the formation of a fold and thrust belt and faults north of the Danish–North German–Polish Caledonides. During the Carboniferous and Permian the basin areas around Rügen and northern Poland were subject to the intrusion of magma. After the Permian there was little tectonic activity in the