|
|
|
|
Zuider Zee
|
| |
|
| |
The Zuiderzee (Dutch: Zuiderzee, ) was a shallow inlet of the North Sea in the northwest of the Netherlands, extending about 100 km inland and at most 50 km wide, with an overall depth of about 4 to 5 meters and a coastline of about 300 km. It covered 5,000 kmē. (2,000 square miles). Its name means "southern sea" in Dutch, indicating that the origin of the name can be found in Friesland to the north of the Zuiderzee (also see North Sea).
Discussion
Ask a question about 'Zuider Zee' Start a new discussion about 'Zuider Zee' Answer questions from other users |
Encyclopedia
The Zuiderzee (Dutch: Zuiderzee, ) was a shallow inlet of the North Sea in the northwest of the Netherlands, extending about 100 km inland and at most 50 km wide, with an overall depth of about 4 to 5 meters and a coastline of about 300 km. It covered 5,000 kmē. (2,000 square miles). Its name means "southern sea" in Dutch, indicating that the origin of the name can be found in Friesland to the north of the Zuiderzee (also see North Sea). In the 20th century the majority of the Zuiderzee was closed off from the North Sea (leaving the mouth of the inlet to become part of the Wadden Sea) and the salt water inlet changed into a fresh water lake called the IJsselmeer (IJssel-lake) after the river that drains into it. The river IJssel is an estuary branch of the river Rhine (Dutch: Rijn).
History and disasters
In classical times there was already a body of water in this location, called Lacus Flevo ("Flevo Lake") by Roman authors. It was much smaller than its later forms and its connection to the main sea was much narrower; it may have been a complex of lakes and marshes and channels, rather than one lake. Over time these lakes gradually eroded their soft peat shores and spread. Some part of this area of water was later called the Vlie; it probably flowed into the sea through what is now the Vliestroom channel between the islands of Vlieland and Terschelling. The Marsdiep was once a river (fluvium Maresdeop) which may have been a distributary of the Vlie. During the early Middle Ages this began to change as rising sea levels and storms started to eat away at the coastal areas which consisted mainly of peatlands. In this period the inlet was referred to as the Almere, indicating it was still more of a lake, but when the mouth and size of the inlet were much widened in the 12th century and especially after a disastrous flood in 1282 broke through the barrier dunes near Texel, the name "Zuiderzee"' came into general usage. The disaster was the making of the little village of Amsterdam, for seagoing traffic could now make it a rendezvous for the Baltic trade.
The size of this inland sea remained largely stable from the 15th century onwards due to improvements in dikes, but when storms pushed North Sea water into the inlet, the Zuiderzee became a volatile cauldron of water, frequently resulting in flooding and the loss of ships. For example, on November 18, 1421, a seawall at the Zuider Zee dike broke, which flooded 72 villages and killed about 10,000 people. This was the Second St. Elizabeth's Flood: see Sint-Elisabethsvloed (1421). An even more massive flood occurred December 14, 1287, when the seawalls broke during a storm, killing approximately 50,000 to 80,000 people in the fifth largest flood in recorded history: see St. Lucia's flood.
Geography and development
Around the Zuiderzee many fishing villages grew up and several developed into walled towns with extensive trade connections, in particular Kampen, a town in Overijssel, and later also towns in Holland such as Amsterdam, Hoorn, and Enkhuizen. These towns traded at first with ports on the Baltic Sea, in England, and in the Hanseatic League, but later also with the rest of the world, when the Netherlands established its colonial empire. When that lucrative trade diminished, most of the towns fell back on fishing and some industry until the 20th century when tourism became the major source of income. Contained within the Zuiderzee were four small islands, the remains of what were once larger islands or peninsulas connected to the mainland. These were Wieringen, Urk, Schokland, and Marken. The inhabitants of these islands also subsisted mainly on fishing and related industries and still do in the case of Urk and Wieringen. All of these islands are now part of the mainland or connected to it.
The construction in the early 20th century of a large enclosing dam (the Afsluitdijk) tamed the Zuiderzee. The creation of this dam was a response to the flood of January 1916. Plans for closing the Zuiderzee had been made over thirty years earlier but had not yet passed in parliament. With the completion of the Afsluitdijk in 1932, the Zuiderzee became the IJsselmeer, and large areas of water could be reclaimed for farming and housing. These areas, known as polders, were respectively the Wieringermeer, the Noordoostpolder, and Flevoland. This enormous project under the direction of Cornelis Lely, called the Zuiderzeeworks, ran from 1919 to 1986, culminating in the creation of the new province of Flevoland. The reclamation project was originally intended to reclaim the former southwestern portion of the Zuiderzee, a body of water now known as the Markermeer, but this final stage of the reclamation project was indefinitely postponed in the 1980s.
External links
- , dedicated to the history and culture of the former Zuiderzee.
Multimedia
- Matthew Halton of CBC Radio (April 19th 1945) reports on German destruction of the sea walls.
|
| |
|
|
