Great Belt

The Great Belt (Danish:Storebælt) is a strait between the main Danish islands of Zealand and Funen. Since 1997 the islands have been connected by the Great Belt Bridge.

Geography

The Great Belt is the major of the three straits of Denmark that connect the Kattegat to the Baltic Sea. The others are listed below under See also.

The Great Belt is 40 miles (60 kilometers) long and 10-20 mi. (16-32 km.) wide. It flows around two major islands: Sprogø in the north and Langeland to the south. At Sprogø the Great Belt divides into East Channel and West Channel. Both East and West are traversed by the Great Belt Bridge, but a tunnel runs under the East also.

Geology

In pre-glacial times, a river, which the Baltic Sea basin contained then, must have passed through the region. So also did the Eemian sea, just prior to the last glaciation, which covered the entire region with ice thousands of feet thick. Today's topography is totally post-glacial. The Great Belt was eroded into existence by streams passing between the Baltic sea basin and the Kattegat. Currently it is a drowned channel.

Beneath the surface it is possible to speak of northern and southern thresholds. The northern consists of two v-shaped cuts more than 50 m deep. The southern is a relatively shallow bottom, 30 m deep, showing the tops of riverine and lacustrine sediments. This configuration gives evidence that for most of its life the Great Belt hosted an outward, downhill flow.

The north threshold is located in the sea off the north coast of Zeeland. The southern is just south of Langeland, leading into the Kieler bucht, or Bay of Kiel. The Fremerbaelt then connects the Bay of Kiel to the Lübecker bucht, or Bay of Lübeck to the south of Lolland. The Bay of Lübeck is open to the Baltic sea.

The current channel of the Great Belt was created by a relatively high fresh water phase of the rising Yoldia sea breaking through to lower Kattegat levels at about 10,000 BP. At that time the exposed northern threshold was a valley less than 1 km wide.

Yoldia sea continued to drain and Kattegat levels continued to rise. By 9500 BC the outward flow stopped and the sea began to transgress into the enlarged Great Belt, turning it brackish very slowly. During the Ancylus lake phase, 9500-8000 BP, the Great Belt was an extension of the Kattegat. At the end of that time rising Kattegat levels broke into Ancylus lake, creating Littorina sea.

Biology

The Great Belt is home to some popular fish: flatfish, sea trout, cod and garfish, which are fished avidly for sport and for sale to consumers.

International Waterway

The Great Belt was navigable to ocean-going vessels in history and, despite a few collisions and near collisions with the bridge, still is. The Danish navy finds it necessary to keep a watchful eye on ships passing through.

In history the Danish government supported itself largely from tolls levied from through traffic under threat of sinking. In the 19th century this practice became so troublesome that the Danish government gave it up. The Copenhagen Convention of 1857 made the Danish straits an International waterway.

External links

Maritime Law at UNESCO

Geography of Denmark | Straits of Europe

Gourt Home::Gourt :: Great Belt

Geography

Geology

Biology

International Waterway

See also

External links