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Braakman
The Braakman was a large tidal inlet in the middle of the Dutch region of Zeelandic Flanders, on the south bank of the Westerschelde west of Terneuzen. It was created by a succession of storm surges in the 14th and 15th centuries, including the St. Elizabeth's flood (1404) and the St. Elizabeth's flood (1421). For a long time the Braakman was a natural barrier between east and west Zeelandic Flanders, and also access to the ports of Boekhoute, Philippine, Axel and Sas van Gent. Over the centuries it steadily spread, drowning at least 15 villages between 1200 and 1601. Then, people fought back. Successive empolderings shrank the Braakman to a remnant, which was finally closed off from the sea in 1952. During the North Sea flood of 1953, this dam proved its worth: it resisted the flood and prevented flooding in the hinterland. The remaining body of water A body of water or waterbody (often spelled water body) is any significant accumulation of water on the surface of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Settlements Lost To Floods In The Netherlands
This list of settlements lost to floods in the Netherlands is an adapted translation ofrom Dutch, plus some additions from other sources. "Oud-" is Dutch for "Old". If you cannot find a name, look for it under "Oud-". Drowned villages and places in Zeeland and West-Brabant Drowned villages and places in Noord-Beveland Drowned villages and places in Zuid-Beveland Drowned villages and places in the Verdronken land van Saeftinghe Drowned villages in Schouwen (mostly in its drowned south part) Drowned villages in the Drowned Land of Reimerswaal Drowned villages in the Braakman Zeeland and West Brabant: doubtful cases Zeeland and West Brabant: drowned islands in the delta region 11 villages west of the Grote Hollandse Waard, east of the current gully of De Striene 4 or 5 drowned villages east of the Schelde Drowned villages in the Grote Hollandse Waard alias South Hollandse Waard 9 villages on the south bank of the Maas, in Brabant and South Holland, in order ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Braakman
The Braakman was a large tidal inlet in the middle of the Dutch region of Zeelandic Flanders, on the south bank of the Westerschelde west of Terneuzen. It was created by a succession of storm surges in the 14th and 15th centuries, including the St. Elizabeth's flood (1404) and the St. Elizabeth's flood (1421). For a long time the Braakman was a natural barrier between east and west Zeelandic Flanders, and also access to the ports of Boekhoute, Philippine, Axel and Sas van Gent. Over the centuries it steadily spread, drowning at least 15 villages between 1200 and 1601. Then, people fought back. Successive empolderings shrank the Braakman to a remnant, which was finally closed off from the sea in 1952. During the North Sea flood of 1953, this dam proved its worth: it resisted the flood and prevented flooding in the hinterland. The remaining body of water A body of water or waterbody (often spelled water body) is any significant accumulation of water on the surface of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Axel (Netherlands)
Axel is a city in the southwest Netherlands. It is located in the municipality of Terneuzen, Zeeland, about 31 km southeast of Vlissingen. Axel received city rights in 1213. History The city was first between 987 and 994 as Axla. The etymology is unclear. Axel was located on the former creek Axelse Gat which had its mouth in the former Braakman inlet. A church was built around 1100, and a castle around 1200. It was a gateway to Ghent, and received city rights in 1213. The city was plundered around 1380 and in 1452 by Ghent. The All Saints' Flood of 1570 resulted in Axel finding itself on an island. Axel was conquered by Maurice, Prince of Orange in 1586 and was fortified. In 1601, eight bastions and one ravelin were constructed around the city. Axel was a strategically important place, because it controlled access to Antwerp and Ghent which were in Spanish hands. In 1789, Axel was reattached to the mainland. The fortifications were removed in 1816. In 1851, Axel lost its ha ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Zeelandic Flanders
Zeelandic Flanders ( ; zea, Zeêuws-Vlaonderen; vls, Zêeuws-Vloandern)''Vlaanderen'' in isolation: . is the southernmost region of the province of Zeeland in the south-western Netherlands. It lies south of the Western Scheldt that separates the region from the remainder of Zeeland and the Netherlands to the north. Zeelandic Flanders is bordered to the south and to the east by Belgium. Geography Zeelandic Flanders is the north-eastern part of the large historical region of Flanders which today lies mostly in Belgium. It shares a land border with the Belgian provinces of East and West Flanders. It is a latitudinally oriented strip of land along the Western Scheldt, a North Sea estuary, and has no land access to the rest of the Netherlands. The area of Zeelandic Flanders is of which is land and is water. The region is bordered by the Zwin nature reserve in the West and the Drowned Land of Saeftinghe in the East. Since local government boundary reforms in 2003, Z ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North Sea Flood Of 1953
The 1953 North Sea flood was a major flood caused by a heavy storm surge that struck the Netherlands, north-west Belgium, England and Scotland. Most sea defences facing the surge were overwhelmed, causing extensive flooding. The storm and flooding occurred at the end of Saturday, 31 January 1953 and morning of the next day. A combination of a high spring tide and a severe European windstorm over the North Sea caused a storm tide. The combination of wind, high tide, and low pressure caused the sea to flood land up to above mean sea level. Flooding summary In the Netherlands 20% of the land was below mean sea level (subsequently with the expansion of Flevoland this proportion has increased); the next-highest 30% sat at less than above sea level. Such land relies heavily on sea defences and was worst affected, recording 1,836 deaths and widespread damage. Most of the casualties occurred in the southern province of Zeeland. In England, 307 people were killed in the counties of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Former Bays
A former is an object, such as a template, gauge or cutting die, which is used to form something such as a boat's hull. Typically, a former gives shape to a structure that may have complex curvature. A former may become an integral part of the finished structure, as in an aircraft fuselage, or it may be removable, being using in the construction process and then discarded or re-used. Aircraft formers Formers are used in the construction of aircraft fuselage, of which a typical fuselage has a series from the nose to the empennage, typically perpendicular to the longitudinal axis of the aircraft. The primary purpose of formers is to establish the shape of the fuselage and reduce the column length of stringers to prevent instability. Formers are typically attached to longerons, which support the skin of the aircraft. The "former-and-longeron" technique (also called stations and stringers) was adopted from boat construction, and was typical of light aircraft built until the ad ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Zeeland
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are the fo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sea Port
A port is a maritime facility comprising one or more wharves or loading areas, where ships load and discharge cargo and passengers. Although usually situated on a sea coast or estuary, ports can also be found far inland, such as Hamburg, Manchester and Duluth; these access the sea via rivers or canals. Because of their roles as ports of entry for immigrants as well as soldiers in wartime, many port cities have experienced dramatic multi-ethnic and multicultural changes throughout their histories. Ports are extremely important to the global economy; 70% of global merchandise trade by value passes through a port. For this reason, ports are also often densely populated settlements that provide the labor for processing and handling goods and related services for the ports. Today by far the greatest growth in port development is in Asia, the continent with some of the world's largest and busiest ports, such as Singapore and the Chinese ports of Shanghai and Ningbo-Zhou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Body Of Water
A body of water or waterbody (often spelled water body) is any significant accumulation of water on the surface of Earth or another planet. The term most often refers to oceans, seas, and lakes, but it includes smaller pools of water such as ponds, wetlands, or more rarely, puddles. A body of water does not have to be still or contained; rivers, streams, canals, and other geographical features where water moves from one place to another are also considered bodies of water. Most are naturally occurring geographical features, but some are artificial. There are types that can be either. For example, most reservoirs are created by engineering dams, but some natural lakes are used as reservoirs. Similarly, most harbors are naturally occurring bays, but some harbors have been created through construction. Bodies of water that are navigable are known as waterways. Some bodies of water collect and move water, such as rivers and streams, and others primarily hold water, such as lakes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hinterland
Hinterland is a German word meaning "the land behind" (a city, a port, or similar). Its use in English was first documented by the geographer George Chisholm in his ''Handbook of Commercial Geography'' (1888). Originally the term was associated with the area of a port in which materials for export and import are stored and shipped. Subsequently, the use of the word expanded to include any area under the influence of a particular human settlement. Geographic region * An area behind a coast or the shoreline of a river. Specifically, by the ''doctrine of the hinterland,'' the hinterland is the inland region lying behind a port and is claimed by the state that owns the coast. * In shipping usage, a port's hinterland is the area that it serves, both for imports and for exports. * The term is also used to refer to the area around a city or town. * More generally, ''hinterland'' can refer to the rural area economically tied to an urban catchment area. The size of a hinterland can depe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 l ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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