Kiel Canal Kiel Canal The Kiel Canal (, literally "North-[to]-Baltic Sea canal", formerly known as the Kaiser-Wilhelm-Kanal) is a long freshwater canal in the German state of Schleswig-Holstein. The canal was finished in 1895, but later widened, and links the North Sea at Brunsbüttel to the Baltic Sea at Kiel-Holtenau. An average of is saved by using the Kiel Canal instead of going around the Jutland Peninsula. This not only saves time but also avoids storm-prone seas and having to pass through the Sound or Belts. Besides its two sea entrances, the Kiel Canal is linked, at Oldenbüttel, to the navigable River
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