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 wells have revealed the existence of petroleum of Lower Paleozoic age beneath Gotland. Bibliography Geology of the Baltic Sea The Geology of the Baltic Sea is characterized by having areas located both at the Baltic Shield of the East European Craton and the Danish-North German-Polish Caledonides. There is a distinction between what is the current Baltic Sea depression, formed in the Cenozoic Era, and the much older sedimentary basins whose sediments are preserved in the zone. Although glacial erosion has contributed to shape the present depression, the Baltic trough is largely a depression of tectonic origin that existed long before