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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 exp ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North Frisia
North Frisia (; ; ) is the northernmost portion of Frisia, located in Schleswig-Holstein, Germany between the rivers Eider and Wiedau. It also includes the North Frisian Islands and Heligoland. The region is traditionally inhabited by the North Frisians. History Ancient settlements The geestland islands along the North Frisian coastline were already densely settled in the time of the early Roman Empire while the marshes further inland were not suited for settling. Only a few ancient marshland settlements have been found during archaeological excavations, namely in the modern area of southern Sylt, the Wiedingharde and along the southern Eiderstedt peninsula. With the beginning of the Migration Period, the number of settlements in North Frisia became ever lesser and many were totally abandoned. A new increase in population in the 8th century has been attributed to immigration but it is thought that the area had not been completely depopulated before.Kühn, Hans Joachim, "Archà ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
European Windstorm
European windstorms are powerful extratropical cyclones which form as cyclonic windstorms associated with areas of low atmospheric pressure. They can occur throughout the year, but are most frequent between October and March, with peak intensity in the winter months. Deep areas of low pressure are common over the North Atlantic, and occasionally start as nor'easters off the New England coast. They frequently track across the North Atlantic Ocean towards the north of Scotland and into the Norwegian Sea, which generally minimizes the impact to inland areas; however, if the track is further south, it may cause adverse weather conditions across Central Europe, Northern Europe and especially Western Europe. The countries most commonly affected include the United Kingdom, Ireland, the Netherlands, Norway, Germany, the Faroe Islands and Iceland. The strong wind phenomena intrinsic to European windstorms, that give rise to "damage footprints" at the surface, can be placed into thr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Büsum
Büsum () is a fishing and tourist town in the district of Dithmarschen, in Schleswig-Holstein, Germany. It is situated on the North Sea coast, approx. 18 km southwest of Heide. Büsum is also the administrative seat of the ''Amt'' ("collective municipality") Büsum-Wesselburen. History and geography The first documented mention of Büsum (as an island) dates from the year 1140. The island's name on medieval documents changed several times from the original Bivsne (1140) to Busin (1208), Busen (1281), and Buzen (1447). Büsum's medieval history has been documented through the chronicles of Neocorus (Johannes Adolph Köster), a pastor and teacher in Büsum during the 16th century. Geographical history During medieval times, Büsum was an island with three villages, Süderdorp, Middeldorp and Norddorp. Devastating floods in 1362 ( Grote Mandrenke), 1436, and 1570 ( All Saint's Flood) drowned most of the island and destroyed the two settlements Süderdorp and Middeldorp. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eiderstedt
Eiderstedt (german: Eiderstedt, ; da, Ejdersted; North Frisian: ''Ääderstää'') is a peninsula in the district of Nordfriesland in the German federal state of Schleswig-Holstein. Overview It is approximately 30 km in length and 15 km in width and has been created through diking (polders) from three islands: Eiderstedt around Tönning, Utholm around Tating, and Evershop around Garding. The diking started around the year 1000 AD. Since these three islands were administrative districts of their own, the area was originally called ''Dreilande'' - "Three Lands". Alluvial soil won from the North Sea makes the area well-suited for agriculture. At present, tourism dominates, particularly in the city of Sankt Peter-Ording on the peninsula's western tip. The Westerhever lighthouse is the peninsula's main emblem and the most prominent lighthouse in Germany. The Wadden Sea, the Eider Barrage on the Eider River and the Katinger Watt, marshlands won from the se ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Halligen
The ''Halligen'' (German, singular ''Hallig'', ) or the ''halliger'' (Danish, singular ''hallig'') are small islands without protective dikes. They are variously pluralized in English as the Halligen, Halligs, Hallig islands, or Halligen islands. There are ten German ''halligen'' in the North Frisian Islands on Schleswig-Holstein's Wadden Sea-North Sea coast in the district of Nordfriesland and one hallig at the west coast of Denmark ( Mandø). The name is cognate to Old-English ''halh'', meaning "slightly raised ground isolated by marsh". The very existence of the ''halligen'' is a result of frequent floods and poor coastal protection. The floods were much more common in the Middle Ages and coastal protection was much poorer. The ''halligen'' have areas ranging from 7 to 956 ha, and are often former parts of the mainland, separated therefrom by storm tide erosion. Some are also parts of once much bigger islands sundered by the same forces. Sometimes, owing to sediment depositi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Parish Register
A parish register in an ecclesiastical parish is a handwritten volume, normally kept in the parish church in which certain details of religious ceremonies marking major events such as baptisms (together with the dates and names of the parents), marriages (with the names of the partners), children, and burials (that had taken place within the parish) are recorded. Along with these vital details, church goods, the parish's response to briefs, and notes on various happenings in the parish were also recorded. These elaborate records existed for the purpose of preventing bigamy and consanguineous marriage. The information recorded in registers was also considered significant for secular governments’ own recordkeeping, resulting in the churches supplying the state with copies of all parish registers. A good register permits the family structure of the community to be reconstituted as far back as the sixteenth century. Thus, these records were distilled for the definitive study of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Artificial Dwelling Hill
A ''terp'', also known as a ''wierde, woerd, warf, warft, werf, werve, wurt'' or ''værft'', is an artificial dwelling mound found on the North European Plain that has been created to provide safe ground during storm surges, high tides and sea or river flooding. The various terms used reflect the regional dialects of the North European region. In English sources, ''terp'' appears to be by far the most common term used. These mounds occur in the coastal parts of the Netherlands (in the provinces of Zeeland, Friesland and Groningen), in southern parts of Denmark and in the north-western parts of Germany where, before dykes were made, floodwater interfered with daily life. These can be found especially in the region Ostfriesland and Kreis Nordfriesland in Germany. In Kreis Nordfriesland on the Halligen, people still live on terps unprotected by dykes. Terps also occur in the Rhine and Meuse river plains in the central part of the Netherlands. Furthermore, terps can be found m ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Husum
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 n ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tide
Tides are the rise and fall of sea levels caused by the combined effects of the gravitational forces exerted by the Moon (and to a much lesser extent, the Sun) and are also caused by the Earth and Moon orbiting one another. Tide tables can be used for any given locale to find the predicted times and amplitude (or " tidal range"). The predictions are influenced by many factors including the alignment of the Sun and Moon, the phase and amplitude of the tide (pattern of tides in the deep ocean), the amphidromic systems of the oceans, and the shape of the coastline and near-shore bathymetry (see '' Timing''). They are however only predictions, the actual time and height of the tide is affected by wind and atmospheric pressure. Many shorelines experience semi-diurnal tides—two nearly equal high and low tides each day. Other locations have a diurnal tide—one high and low tide each day. A "mixed tide"—two uneven magnitude tides a day—is a third regular category. Tid ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Koldenbüttel
Koldenbüttel ( North Frisian: ''Koolnbütel'', nds, Kombüddel, da, Koldenbøl, Koldenbyttel) is a municipality in the district of Nordfriesland, in Schleswig-Holstein, Germany. Geography und infrastructure Koldenbüttel lies in the Eider Treene-Losiny about 8 miles south of Husum and just west of Friedrichstadt at the confluence of the Eider and the Treene in the Marsh. Koldenbüttel applies as Eiderstedt's most eastern village. Until the Treene's damming up in 1570 the village was suspended by Storm surges from North Sea-water flowing in the Eider and the Treene. Now there is a road at the dike's top leading from Koldenbüttel to Friedrichstadt The Bundesstraße 202 runs through the town; it connects the village with Friedrichstadt. At the Railway Tönning-Husum, which was opened in 1854, there was a small train station called "Büttel". After finishing the "Marschbahn" this breakpoint was closed down because of a central train station in Friedrichstadt. History Kol ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Creek (tidal)
A tidal creek or tidal channel is a narrow inlet or estuary that is affected by the ebb and flow of ocean tides. Thus, it has variable salinity and electrical conductivity over the tidal cycle, and flushes salts from inland soils. Tidal creeks are characterized by slow water velocity, resulting in buildup of fine, organic sediment in wetlands. Creeks may often be a dry to muddy channel with little or no flow at low tide, but with significant depth of water at high tide. Due to the temporal variability of water quality parameters within the tidally influenced zone, there are unique biota associated with tidal creeks which are often specialised to such zones. Nutrients and organic matter are delivered downstream to habitats normally lacking these, while the creeks also provide access to inland habitat for salt-water organisms. Terminology A "creek" normally refers to a tidal water channel in British English and in other parts of the Anglosphere. This is the case in many countries ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
