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Koog
A ''koog'' (plural: ''köge'') or ''groden'' is a type of polder found on the North Sea coast of Germany that is established by the construction of dykes enclosing the land which is then drained to form marshland. This type of land reclamation is also used along rivers. In general, a ''koog'' is protected by embankments known as dykes (''Deiche''). Etymology Unlike the meaning in modern German, Ingvaeonic ''*kāg'', Old Dutch ''*kōg'', modern Dutch ''koog'' and West Frisian Dutch ''kaag'' all designate "land outside the dike". In the Netherlands, it primarily survives in place names (e.g. De Koog, Koog aan de Zaan, Kaag). From the Dithmarschen word ''koch'' (15th and 16th centuries), it went into Danish as ''kog''. In North Frisian it is ''kuch''. The spelling ''koog'' was used by the poet Michael Richey in 1755 and around 1700, what is now the port of Cuxhaven was still called ''Koogshaven''. Polders In the Netherlands and in the adjacent regions of East Frisia the wo ...
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Koog Aan De Zaan
Koog aan de Zaan () is a town in the Dutch province of North Holland. It is a part of the municipality of Zaanstad, and lies about 11 km northwest of Amsterdam. History Koog aan de Zaan developed in the 16th century on the western bank of the Zaan River from Westzaan. In 1867, the Koog aan de Zaan railway station opened and in the 1870s, it started to industrialise and fill-in the area before the river and the station. The Dutch Reformed church is an aisleless cruciform church which was built in 1685. The tower burnt down in 1920, and the church was restored between 1920 and 1922. Koog aan de Zaan was a separate municipality until 1974, when the municipality of Zaanstad was created. Koog aan de Zaan is one of the smallest submunicipalities in Zaanstad, having a surface area of 320 hectare. A8ernA, an urban renewal project for the space under the A8 motorway as it passes through Koog aan de Zaan, was a joint winner of the 2006 European Prize for Urban Public Space. Tra ...
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De Koog
De Koog is a village in the Dutch province of North Holland. It is a part of the municipality of Texel, and lies about 17 km north of Den Helder. It is the chief centre of tourism on the island, surrounded with many hotels and campgrounds. The village is located on the North Sea coast of the island. Only two narrow lines of dunes separate the village from the beach. South of the village is a wooded area which is also popular with tourists. The information centre and museum about the Wadden Sea The Wadden Sea ( nl, Waddenzee ; german: Wattenmeer; nds, Wattensee or ; da, Vadehavet; fy, Waadsee, longname=yes; frr, di Heef) is an intertidal zone in the southeastern part of the North Sea. It lies between the coast of northwestern conti ..., , are located here. History The village was first mentioned in 1436 as Cogersdyck, and means "land on water". De Koog is a road village which developed in the dunes during the 14th century. It used to be a fishing village up to the mi ...
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Dithmarschen
Dithmarschen (, Low Saxon: ; archaic English: ''Ditmarsh''; da, Ditmarsken; la, label=Medieval Latin, Tedmarsgo) is a district in Schleswig-Holstein, Germany. It is bounded by (from the north and clockwise) the districts of Nordfriesland, Schleswig-Flensburg, Rendsburg-Eckernförde, and Steinburg, by the state of Lower Saxony (district of Stade, from which it is separated by the Elbe river), and by the North Sea. From the 13th century up to 1559 Dithmarschen was an independent peasant republic within the Holy Roman Empire and a member of the Hanseatic League. Geography The district is located on the North Sea. It is embraced by the Elbe estuary to the south and the Eider estuary to the north. Today it forms a kind of artificial island, surrounded by the Eider river in the north and the Kiel Canal in both the east and southeast. It is a rather flat countryside that was once full of fens and swamps. To the north it borders on Nordfriesland and Schleswig-Flensburg, to the east o ...
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Polder
A polder () is a low-lying tract of land that forms an artificial hydrological entity, enclosed by embankments known as dikes. The three types of polder are: # Land reclaimed from a body of water, such as a lake or the seabed # Flood plains separated from the sea or river by a dike # Marshes separated from the surrounding water by a dike and subsequently drained; these are also known as '' koogs'', especially in Germany The ground level in drained marshes subsides over time. All polders will eventually be below the surrounding water level some or all of the time. Water enters the low-lying polder through infiltration and water pressure of groundwater, or rainfall, or transport of water by rivers and canals. This usually means that the polder has an excess of water, which is pumped out or drained by opening sluices at low tide. Care must be taken not to set the internal water level too low. Polder land made up of peat (former marshland) will sink in relation to its previous ...
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North Sea
The North Sea lies between Great Britain, Norway, Denmark, Germany, the Netherlands and Belgium. An epeiric sea, epeiric sea on the European continental shelf, it connects to the Atlantic Ocean through the English Channel in the south and the Norwegian Sea in the north. It is more than long and wide, covering . It hosts key north European shipping lanes and is a major fishery. The coast is a popular destination for recreation and tourism in bordering countries, and a rich source of energy resources, including wind energy, wind and wave power. The North Sea has featured prominently in geopolitical and military affairs, particularly in Northern Europe, from the Middle Ages to the modern era. It was also important globally through the power northern Europeans projected worldwide during much of the Middle Ages and into the modern era. The North Sea was the centre of the Viking Age, Vikings' rise. The Hanseatic League, the Dutch Golden Age, Dutch Republic, and the Kingdom of Grea ...
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Wilhelmshaven
Wilhelmshaven (, ''Wilhelm's Harbour''; Northern Low Saxon: ''Willemshaven'') is a coastal town in Lower Saxony, Germany. It is situated on the western side of the Jade Bight, a bay of the North Sea, and has a population of 76,089. Wilhelmshaven is the centre of the "Jade Bay" business region (which has around 330,000 inhabitants) and is Germany's main military port. The adjacent Lower Saxony Wadden Sea National Park (part of the Wattenmeer UNESCO World Natural Heritage Site) provides the basis for the major tourism industry in the region. History The , built before 1383, operated as a pirate stronghold; the Hanseatic League destroyed it in 1433. Four centuries later, the Kingdom of Prussia planned a fleet and a harbour on the North Sea. In 1853, Prince Adalbert of Prussia, a cousin of the Prussian King Frederick William IV, arranged the Jade Treaty (''Jade-Vertrag'') with the Grand Duchy of Oldenburg, in which Prussia and the Grand Duchy entered into a contract whereby Old ...
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Netherlands
) , anthem = ( en, "William of Nassau") , image_map = , map_caption = , subdivision_type = Sovereign state , subdivision_name = Kingdom of the Netherlands , established_title = Before independence , established_date = Spanish Netherlands , established_title2 = Act of Abjuration , established_date2 = 26 July 1581 , established_title3 = Peace of Münster , established_date3 = 30 January 1648 , established_title4 = Kingdom established , established_date4 = 16 March 1815 , established_title5 = Liberation Day , established_date5 = 5 May 1945 , established_title6 = Kingdom Charter , established_date6 = 15 December 1954 , established_title7 = Caribbean reorganisation , established_date7 = 10 October 2010 , official_languages = Dutch , languages_type = Regional languages , languages_sub = yes , languages = , languages2_type = Recognised languages , languages2_sub = yes , languages2 = , demonym = Dutch , capital = Amsterdam , largest_city = capital , ...
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Mud Flat
Mudflats or mud flats, also known as tidal flats or, in Ireland, slob or slobs, are coastal wetlands that form in intertidal areas where sediments have been deposited by tides or rivers. A global analysis published in 2019 suggested that tidal flat ecosystems are as extensive globally as mangroves, covering at least of the Earth's surface. / They are found in sheltered areas such as bays, bayous, lagoons, and estuaries; they are also seen in freshwater lakes and salty lakes (or inland seas) alike, wherein many rivers and creeks end. Mudflats may be viewed geologically as exposed layers of bay mud, resulting from deposition of estuarine silts, clays and aquatic animal detritus. Most of the sediment within a mudflat is within the intertidal zone, and thus the flat is submerged and exposed approximately twice daily. A recent global remote sensing analysis estimated that approximately 50% of the global extent of tidal flats occurs within eight countries (Indonesia, China, Australia, ...
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Oldenburg Land
Oldenburg Land (german: Oldenburger Land) is a region and regional association in the German state of Lower Saxony in the area of the former Grand Duchy of Oldenburg (1815–1918), the later Free State of Oldenburg (1918–1946) and administrative district of Oldenburg (1946 to 1978), without its exclaves, along the rivers Hunte and Hase. In the region between Waterkant, Dümmer and Damme Hills some of the population still speak Low German today and, in Saterland also Saterland Frisian. The region is rich in old Lower Saxon customs such as ''Schützenfests'' or '' Kohlfahrten''. Typical country sports include '' Klootschießen'' and '' Boßeln''. The mainly Catholic southern part of the Oldenburg Land is known as Oldenburg Münsterland, the mainly Lutheran northern part is known as Oldenburg Land (''Old Oldenburg'') in its narrower sense. In terms of Germany's modern administrative districts, Oldenburg Land roughly corresponds to Ammerland, Cloppenburg, Delmenhorst, Frie ...
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