Fischland-Darß-Zingst
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Fischland-Darß-Zingst
Fischland-Darß-Zingst or Fischland-Darss-Zingst''Fischland-Darss-Zingst - a sleepy and gorgeously natural peninsula''
at www.fischland-darss-zingst.net. Accessed on 18 Dec 2011. is a long in the coastal district of , in the German state of . The three parts of the peninsula, from west to ...
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Fischland-Darß-Zingst
Fischland-Darß-Zingst or Fischland-Darss-Zingst''Fischland-Darss-Zingst - a sleepy and gorgeously natural peninsula''
at www.fischland-darss-zingst.net. Accessed on 18 Dec 2011. is a long in the coastal district of , in the German state of . The three parts of the peninsula, from west to ...
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Mecklenburg-Vorpommern
Mecklenburg-Vorpommern (MV; ; nds, Mäkelborg-Vörpommern), also known by its anglicized name Mecklenburg–Western Pomerania, is a state in the north-east of Germany. Of the country's sixteen states, Mecklenburg-Vorpommern ranks 14th in population; it covers an area of , making it the sixth largest German state in area; and it is 16th in population density. Schwerin is the state capital and Rostock is the largest city. Other major cities include Neubrandenburg, Stralsund, Greifswald, Wismar, and Güstrow. It was named after the 2 regions of Mecklenburg and Vorpommern (which means West Pomerania). The state was established in 1945 after World War II through the merger of the historic regions of Mecklenburg and the Prussian Western Pomerania by the Soviet military administration in Allied-occupied Germany. It became part of the German Democratic Republic in 1949, but was dissolved in 1952 during administrative reforms and its territory divided into the districts of R ...
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Zingst
Zingst ( Polabian ''Sgoni'') is the easternmost portion of the three-part Fischland-Darß-Zingst Peninsula, located in Mecklenburg-Vorpommern, Germany, between the cities of Rostock and Stralsund on the southern shore of the Baltic Sea. The area is part of the Pomeranian coast. The Zingst Peninsula forms an eastward-running spit, nearly in length, and has a width of just . Zingst separates the Baltic Sea from the lagoon of Barther Bodden, which is part of the Darss-Zingst Bodden Chain, a large estuary. The shallow waters of the inlet are a major stopover for the migratory European crane. In spring and autumn, up to 3,000 birds gather here on their migration route to and from Spain. Most of the estuary and the eastern end of the peninsula are part of the Western Pomerania Lagoon Area National Park. Until the early 1870s, Zingst was an island, separated from Darß by the Prerowstrom, a narrow inlet. A storm tide in 1874 closed the inlet, which had connected the ''bodden'' ...
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Prerower Strom
The Prerower Strom, Prerow Strom
at www.ostseeferieninfo.de. Retrieved 27 Jun 2019. or Prerowstrom is an arm of the in northeast Germany. It begins near the island of Schmidtbülten in the and winds its way through the countryside of the peninsula of , where it separates from the < ...
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Fischland
Fischland (literally "fish land") is an isthmus on the southern Baltic Sea coast on the Bay of Mecklenburg in northeastern Germany. It is part of the peninsula of Fischland-Darß-Zingst. Fischland was an island until the 14th century and was bounded by the navigable estuarine branches of the River Recknitz: the Permin in the south and the Loop in the north. In more recent times its southern boundary has usually been considered to be the Recknitz Meadowland (''Recknitzer Stadtwiesen'') and the Rostock Heath (''Rostocker Heide''). To the west and east its boundaries are more obvious: on the one side is its active cliffed coast on the Baltic, and on the other the coastline alongside the Saaler Bodden, only a few centimetres above sea level. Fischland is about 5 km long, between 500 metres and 2 km wide and runs from southwest to northeast. The Pleistocene island core, which is subjected to marked changes as a result of water and wind action, consists of glacial sand ...
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Darß
The Darß or Darss is the middle part of the peninsula of Fischland-Darß-Zingst on the southern shore of the Baltic Sea in the German state of Mecklenburg-Western Pomerania. The peninsula's name is of Slavic origin. There is a large forest in the Darß. In recent times, the name "Darß" has also been used to refer to the entire peninsula. The Darß is famous for being a resting place for tens of thousands of migrating cranes and geese. Tourism has long been a source of income and has increased since German reunification, but the Darß is still far from being a crowded tourist place. Location and character The Darß lies northeast of Fischland and west of the peninsula of Zingst, its boundary with the latter being formed by the inlet of the Prerower Strom. To the north lies the Baltic Sea; to the south the lagoons of Saaler Bodden and Bodstedter Bodden, which belong to the Darss-Zingst Bodden Chain. The Darß measures between from north to south and from east to west and is ...
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Bodden
Bodden are briny bodies of water often forming lagoons, along the southwestern shores of the Baltic Sea, primarily in Germany's state of Mecklenburg-Vorpommern. These lagoons can be found especially around the island of Rügen, Usedom and the Fischland-Darss-Zingst peninsula. Some of them are protected reserves, forming the Western Pomerania Lagoon Area National Park. They have a distinctive geological origin and are enclosed by peninsulae, spits and islands, leaving only narrow connections to adjacent bodden or the open sea. Freshwater inflow from the mainland and saltwater inflow from the open sea, which depends on wind direction and force as well as the proximity of the bodden to the sea, result in fluctuating salt gradients and distinctive ecosystems. During the Littorina Sea transgression, an island archipelago was formed by the carving of narrow glacial basins and channels resulting from meltwater. Bodden were formed in a comparatively short period between spits and ...
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Ahrenshoop
Ahrenshoop is a municipality in the Vorpommern-Rügen district, in Mecklenburg-Vorpommern, Germany on the Fischland-Darß-Zingst peninsula of the Baltic Sea. It used to be a small fishing village, but is today known for its tourism and as a holiday resort. Early history Ahrenshoop was first mentioned in 1311 as the defining point of the border of the town of Ribnitz´s property. In 1328 Duke Heinrich II of Mecklenburg donated the area east of this border to the monastery of Ribnitz. In 1395 forces of the City of Rostock destroyed a stronghold, built by Bogislaw VI. of Pomerania, and the harbour of Ahrenshoop. In 1591 the border between Mecklenburg and Pomerania was defined, which runs through the village, still existing today as the "Grenzweg" (border road). After the Treaty of Westphalia in 1648 the Eastern part of the village became part of Swedish Pomerania until 1815, when Sweden ceded Pomerania to Prussia. Until the Grand Duchy of Mecklenburg-Schwerin joined the German Zo ...
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West Pomeranian Lagoon Area National Park
The Western Pomerania Lagoon Area National Park
at www.naturefund.de. Accessed on 27 June 2012. (''Nationalpark Vorpommersche Boddenlandschaft'') is 's largest national park, situated at the coast of the . It consists of several peninsulas, islands and lagoon shore areas in the , belonging to the district of

Western Pomerania Lagoon Area National Park
The Western Pomerania Lagoon Area National Park
at www.naturefund.de. Accessed on 27 June 2012. (''Nationalpark Vorpommersche Boddenlandschaft'') is Mecklenburg-Vorpommern's largest national park, situated at the coast of the Baltic Sea. It consists of several peninsulas, islands and lagoon shore areas in the Baltic Sea, belonging to the district of Vorpommern-Rügen. The national park includes: * the Darss, Darß peninsula * the western coast of the island of Rügen * the island of Hiddensee * the island of Ummanz * several tiny islets between the above places * the multiple lagoons in between the land masses The national park is characterised by very shallow water housing a unique coastal fauna. All portions of the national park are famous for being a resting place for tens of thousands of crane (b ...
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Sea Cliffs
A cliffed coast, also called an abrasion coast, is a form of coast where the action of marine waves has formed steep cliffs that may or may not be precipitous. It contrasts with a flat or alluvial coast. Formation In coastal areas in which the land surface dips at a relatively steep angle below the water table, the continuous action of marine waves on the coastline, known as abrasion, may create a steep declivity known as a cliff, the slope angle of which depends on a variety of factors including the jointing, bedding and hardness of the materials making up the cliff as well as the erosional processes themselves.Herbert Louis and Klaus Fischer: ''Allgemeine Geomorphologie'', de Gruyter, 4th ed., Berlin 1979, pp. 532-537 The slope is constantly being eroded. The waves attacking the cliff-foot form a wave-cut notch by constant abrasion action producing an overhang. This overhang grows in size as the cliff is undercut, until it collapses under its own weight. The loose ...
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