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Nordfriesland (district)
Nordfriesland (; da, Nordfrisland; frr, Nordfraschlönj ), also known as North Frisia, is the northernmost Districts of Germany, district of Germany, part of the state of Schleswig-Holstein. It includes almost all of traditional North Frisia (with the exception of the island of Heligoland), as well as adjacent parts of the Schleswig Geest to the east and Stapelholm to the south, and is bounded (from the east and clockwise) by the districts of Schleswig-Flensburg and Dithmarschen, the North Sea and the Denmark, Danish county of South Jutland County, South Jutland. The district is called ''Kreis Nordfriesland'' in German language, German, ''Kreis Noordfreesland'' in Low German language, Low German, ''Kris Nordfraschlönj'' in Mooring (North Frisian dialect), Mooring North Frisian, ''Kreis Nuurdfresklun'' in Fering, Fering North Frisian and ''Nordfrislands amt'' in Danish language, Danish. As of 2008, Nordfriesland was the Tourism in Germany, most visited rural district in Germa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Husum, Germany
Husum (, frr, Hüsem) is the capital of the ''Kreis'' (district) Nordfriesland in Schleswig-Holstein, Germany. The town was the birthplace of the novelist Theodor Storm, who coined the epithet "the grey town by the sea". It is also the home of the annual international piano festival ''Raritäten der Klaviermusik'' (Rarities of Piano Music) founded in 1986. History Husum was first mentioned as ''Husembro'' in 1252, when king Abel was murdered. Like most towns on the North Sea, Husum was always strongly influenced by storm tides. In 1362 a disastrous storm tide, the "Grote Mandrenke" flooded the town and carved out the inland harbour. Before this date Husum was not situated directly on the coast. The people of the city took advantage of this opportunity and built a marketplace, which led to a great economic upturn. Between 1372 and 1398 the population of Husum grew rapidly, and two villages, ''Oster-Husum'' (East-Husum) and ''Wester-Husum'' (West-Husum), were founded. The name ' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North Frisian Language
North Frisian (''nordfriisk'') is a minority language of Germany, spoken by about 10,000 people in North Frisia. The language is part of the larger group of the West Germanic Frisian languages. The language comprises 10 dialects which are themselves divided into an insular and a mainland group. North Frisian is closely related to the Saterland Frisian language of Northwest Germany and West Frisian which is spoken in the Netherlands. All of these are also closely related to the English language forming the Anglo-Frisian group. The phonological system of the North Frisian dialects is strongly being influenced by Standard German and is slowly adapting to that of the German language. With a number of native speakers probably even less than 10,000 and decreasing use in mainland North Frisia, the North Frisian language is endangered. It is protected as a minority language and has become an official language in the Nordfriesland district and on Heligoland island. Classification The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Low German
: : : : : (70,000) (30,000) (8,000) , familycolor = Indo-European , fam2 = Germanic , fam3 = West Germanic , fam4 = North Sea Germanic , ancestor = Old Saxon , ancestor2 = Middle Low German , dia1 = West Low German , dia2 = East Low German , iso2 = nds , iso3 = nds , iso3comment = (Dutch varieties and Westphalian have separate codes) , lingua = 52-ACB , map = Nds Spraakrebeet na1945.svg , mapcaption = Present day Low German language area in Europe. , glotto = lowg1239 , glottoname = Low German , notice = IPA Low German or Low Saxon (in the language itself: , and other names; german: Plattdeutsch, ) is a West Germanic language variety spoken mainly in Northern Germany and the northeastern part of the Netherlands. The dialect of Plautdietsch is also spoken in the Russian Mennonite diaspora worldwi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Multilingualism
Multilingualism is the use of more than one language, either by an individual speaker or by a group of speakers. It is believed that multilingual speakers outnumber monolingual speakers in the world's population. More than half of all Europeans claim to speak at least one language other than their mother tongue; but many read and write in one language. Multilingualism is advantageous for people wanting to participate in trade, globalization and cultural openness. Owing to the ease of access to information facilitated by the Internet, individuals' exposure to multiple languages has become increasingly possible. People who speak several languages are also called polyglots. Multilingual speakers have acquired and maintained at least one language during childhood, the so-called first language (L1). The first language (sometimes also referred to as the mother tongue) is usually acquired without formal education, by mechanisms about which scholars disagree. Children acquirin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Duchy Of Schleswig
The Duchy of Schleswig ( da, Hertugdømmet Slesvig; german: Herzogtum Schleswig; nds, Hartogdom Sleswig; frr, Härtochduum Slaswik) was a duchy in Southern Jutland () covering the area between about 60 km (35 miles) north and 70 km (45 mi) south of the current border between Germany and Denmark. The territory has been divided between the two countries since 1920, with Northern Schleswig in Denmark and Southern Schleswig in Germany. The region is also called Sleswick in English. Unlike Holstein and Lauenburg, Schleswig was never a part of the German Confederation. Schleswig was instead a fief of Denmark, and its inhabitants spoke Danish, German, and North Frisian. Both Danish and German National Liberals wanted Schleswig to be part of a Danish or German national state in the 19th century. A German uprising in March 1848 caused the First Schleswig War which ended in 1852. The Second Schleswig War (1864) ended with the three duchies being governed jointly by Austria ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Burchardi Flood
The Burchardi flood (also known as the second Grote Mandrenke) was a storm tide that struck the North Sea coast of North Frisia and Dithmarschen (in modern-day Germany) on the night between 11 and 12 October 1634. Overrunning dikes, it shattered the coastline and caused thousands of deaths (8,000 to 15,000 people drowned) and catastrophic material damage. Much of the island of Strand washed away, forming the islands Nordstrand, Pellworm and several ''halligen''. Background The Burchardi flood hit Schleswig-Holstein during a period of economic weakness. In 1603 a plague epidemic spread across the land, killing many. The flooding occurred during the Thirty Years' War, which also did not spare Schleswig-Holstein. Fighting had occurred between locals and the troops of Frederick III, Duke of Holstein-Gottorp, especially on Strand Island. The people of Strand were resisting changes to their old defence treaties and the forced accommodation of troops. Supported by a Danish expediti ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Strand (island)
Strand was an island on the west coast of Nordfriesland in Schleswig, which was a fiefdom of the Danish crown. The area now belongs to Schleswig-Holstein in northern Germany. Coastlines along the Dutch-German-Danish coasts were significantly changed during and by a huge storm tide, the Saint Marcellus' flood – also referred to as the Grote Mandrenke – that occurred on 16 January 1362. Many villages and towns were lost. The outlines of Strand changed significantly, nowadays legendary Rungholt reportedly being amongst the now sunken places. The island of Südfall was separated from the mainland. In 1634 the Burchardi flood finally split Strand island into Nordstrand, Pellworm and Nordstrandischmoor Nordstrandischmoor ( da, Nordstrand Mor or Nordstrandmose, North Frisian: ''Lätj Möör''; also known locally as ''Lüttmoor'') is a ''Hallig'' (undyked islet) off the North Frisian coast in Germany and lies within the Schleswig-Holstein Wadden .... References * * Exter ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Grote Mandrenke
Saint Marcellus's flood or (Low Saxon: ; da, Den Store Manddrukning, 'Great Drowning of Men') was an intense extratropical cyclone, coinciding with a new moon, which swept across the British Isles, the Netherlands, northern Germany, and Denmark (including Schleswig/Southern Jutland) around 16 January 1362 ( OS), causing at least 25,000 deaths. The storm tide is also called the "Second St. Marcellus flood" because it peaked on 16 January, the feast day of St. Marcellus. A previous "First St. Marcellus flood" drowned 36,000 people along the coasts of West Friesland and Groningen on 16 January 1219. An immense storm tide from the North Sea swept far inland from England and the Netherlands to Denmark and the German coast, breaking up islands, making parts of the mainland into islands, and wiping out entire towns and districts. These included Rungholt, said to have been located on the island of Strand in North Frisia, Ravenser Odd in East Yorkshire, and the harbour of Dunwich. This ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rungholt
Rungholt was a settlement in North Frisia, in what was then the Danish Duchy of Schleswig. The area is today located in Germany. Rungholt reportedly sank beneath the waves of the North Sea when a storm tide (known as ''Grote Mandrenke'' or ''Den Store Manddrukning'') hit the coast on 15 or 16 January 1362. Location The exact location of Rungholt remains unclear. It is likely that Rungholt was situated on the island of Strand, which was overwhelmed by the Burchardi Flood of 1634, and of which the islets of Pellworm and Nordstrandischmoor and the Nordstrand peninsula are the only remaining fragments. One possible location is west of the Hallig Südfall, where in 1921 significant ruins were discovered: wells, trenches and part of a tidal lock. Another theory places Rungholt to the north of the Hallig Südfall. History Today it is widely accepted that Rungholt existed and was not just a local legend. Documents support this, although they mostly date from much later times (16th c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dike (construction)
A levee (), dike ( American English), dyke ( Commonwealth English), embankment, floodbank, or stop bank is a structure that is usually earthen and that often runs parallel to the course of a river in its floodplain or along low-lying coastlines. The purpose of a levee is to keep the course of rivers from changing and to protect against flooding of the area adjoining the river or coast. Levees can be naturally occurring ridge structures that form next to the bank of a river, or be an artificially constructed fill or wall that regulates water levels. Ancient civilizations in the Indus Valley, ancient Egypt, Mesopotamia and China all built levees. Today, levees can be found around the world, and failures of levees due to erosion or other causes can be major disasters. Etymology Speakers of American English (notably in the Midwest and Deep South) use the word ''levee'', from the French word (from the feminine past participle of the French verb , 'to raise'). It ori ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Storm Tides Of The North Sea
Storm tides of the North Sea are coastal floods associated with extratropical cyclones crossing over the North Sea, the severity of which are affected by the shallowness of the sea and the orientation of the shoreline relative to the storm's path, as well as the timing of tides. The water level can rise to more than 5 metres (17 ft) above the normal tide as a result of storm tides. Northern Germany and Denmark are particularly susceptible to storm tides. The coastline of the German Bight forms an L-shape facing northwest. Also vulnerable are the United Kingdom and the Netherlands, where the sea shallows and is funnelled toward the English Channel. Storm tides are a regular occurrence in the North Sea basin; several form each year. Although most do not cause significant damage, the impact of some has been devastating. During one, the February flood of 1825, the Danish coastline changed, as the North Jutlandic Island became separated from the Jutland Peninsula. Major s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
