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Slaak Of Volkerak
The Volkerak is a body of water in the Netherlands. It is part of the Rhine–Meuse–Scheldt delta, and is situated between the island Goeree-Overflakkee to the north-west and the Dutch mainland to the south and east. The western part of the Volkerak is also called Krammer. Tributaries of the Volkerak are the Dintel and Steenbergse Vliet. Before 1987, it was a tidal river open to the North Sea, but it was closed off as part of the Delta Works; it is now a fresh water lake. Delta Works The Volkerak is navigable by sea-going ships. On the eastern end are the Volkerak Locks (''Volkeraksluizen'') connecting it to the Hollands Diep. At the western end is the Philipsdam and Krammer Locks (''Krammersluizen'') connecting it to the Eastern Scheldt (''Oosterschelde''), and also the Grevelingendam and Grevelingen Lock (''Grevelingensluis'') connecting it to the Grevelingen Grevelingen. Finally, the Scheldt–Rhine Canal The Scheldt–Rhine Canal (Schelde-Rijnkanaal) in Belgium an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Grevelingen
Grevelingen or Grevelingenmeer ( Lake Grevelingen) is a closed off part of the Rhine- Meuse estuary on the border of the Dutch provinces of South Holland and Zeeland. It is situated between the islands of Goeree-Overflakkee (South Holland) and Schouwen-Duiveland (Zeeland) and was closed off as part of the Delta Works, a huge engineering project designed to protect the southwestern part of the Netherlands from flooding. The Brouwersdam, a dike connecting the two islands on the west, closes off the Grevelingen from the North Sea. The Grevelingendam, the dike on the east, blocks the inflow of Rhine and Meuse water. Since its closure in 1971 the saltwater of the Grevelingen slowly started to become brackish due to rainwater and excess polderwater from the islands, but the Dutch changed their mind and decided that they wanted to preserve the saline biotope. Therefore, in 1978 a sluice was created under the Brouwersdam, partially restoring and maintaining the saline chara ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of South Holland
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, plateau ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tholen
Tholen () is a 25,000 people Municipalities of the Netherlands, municipality in the southwest of the Netherlands. The municipality of Tholen takes its name from the town of Tholen, which is the largest population center in the municipality. The municipality consists of two peninsulas, formerly islands, the larger one on the south also called Tholen, the smaller one on the north called Sint Philipsland (island), Sint Philipsland. The two are separated by the former strait, now bay, of Krabbenkreek. The municipality is bordered on the east by the Eendracht, once a Scheldt branch but now part of the Scheldt-Rhine Canal, crossed by three road bridges, by the Oosterschelde estuary to the south, the straits of Keeten-Mastgat to the west and the Krammer (Netherlands), Krammer strait to the north. The town has a small historical center partly surrounded by a "gracht" and partly bordered by a harbour for fishing boats and yachts. Population centers On the island Sint Philipsland (islan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Steenbergen
Steenbergen () is a municipality and a town in the province of North Brabant in the south of the Netherlands. The municipality had a population of in and covers an area of of which is water. The municipality is mainly agricultural including a strongly growing greenhouse sector, but Steenbergen and the nearby town of Dinteloord also contain some light industry. A new stretch of A4 motorway under construction is expected to further increase the municipality's attractiveness, allowing easy connections with the large cities of Rotterdam to the north and the Belgian city of Antwerp to the south. The connection with the nearby city of Bergen op Zoom will also be improved as a result. Population centres The city of Steenbergen Steenbergen received city rights in 1272. Graves of Guy Gibson and Jim Warwick Guy Gibson, Wing Commander and the first CO of the RAF's 617 Squadron which he led in the " Dam Busters" raid in 1943, crashed with his Mosquito aircraft in this mu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moerdijk
Moerdijk () is a municipality and a town in the South of the Netherlands, in the province of North Brabant. History The municipality of Moerdijk was founded in 1997 following the merger of the municipalities of Fijnaart en Heijningen, Klundert, Standdaarbuiten, Willemstad, and Zevenbergen. At that time the new municipality was called Zevenbergen. The name changed to Moerdijk on 1 April 1998. * List of mayors of Moerdijk Population centres Topography ''Dutch Topographic map of the municipality of Moerdijk, June 2015'' The village of Moerdijk The village of Moerdijk is one of the smaller villages of the municipality. Population as of 2002 is 1,205. ''Moerdijk'' is however a well-known name in the Netherlands, because of the large Moerdijk industrial area, with a large power plant, and because of the well-known Moerdijk bridges (highway and railway bridges) across the Hollands Diep. This was the last bridge available for the retreat from the vital Scheldt Estuary of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Algal Bloom
An algal bloom or algae bloom is a rapid increase or accumulation in the population of algae in freshwater or marine water systems. It is often recognized by the discoloration in the water from the algae's pigments. The term ''algae'' encompasses many types of aquatic photosynthetic organisms, both macroscopic multicellular organisms like seaweed and microscopic unicellular organisms like cyanobacteria. ''Algal bloom'' commonly refers to the rapid growth of microscopic unicellular algae, not macroscopic algae. An example of a macroscopic algal bloom is a kelp forest. Algal blooms are the result of a nutrient, like nitrogen or phosphorus from various sources (for example fertilizer runoff or other forms of nutrient pollution), entering the aquatic system and causing excessive growth of algae. An algal bloom affects the whole ecosystem. Consequences range from the benign feeding of higher trophic levels to more harmful effects like blocking sunlight from reaching other ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eutrophication
Eutrophication is the process by which an entire body of water, or parts of it, becomes progressively enriched with minerals and nutrients, particularly nitrogen and phosphorus. It has also been defined as "nutrient-induced increase in phytoplankton productivity". Water bodies with very low nutrient levels are termed oligotrophic and those with moderate nutrient levels are termed mesotrophic. Advanced eutrophication may also be referred to as dystrophic and hypertrophic conditions. Eutrophication can affect freshwater or salt water systems. In freshwater ecosystems it is almost always caused by excess phosphorus. In coastal waters on the other hand, the main contributing nutrient is more likely to be nitrogen, or nitrogen and phosphorus together. This depends on the location and other factors. When occurring naturally, eutrophication is a very slow process in which nutrients, especially phosphorus compounds and organic matter, accumulate in water bodies. These nutrients de ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Port Of Antwerp
The Port of Antwerp-Bruges is the port of the City of Antwerp. It is located in Flanders (Belgium), mainly in the province of Antwerp but also partially in the province of East Flanders. It is a seaport in the heart of Europe accessible to capesize ships. It is Europe’s second-largest seaport, after Rotterdam. Antwerp stands at the upper end of the tidal estuary of the Scheldt. The estuary is navigable by ships of more than 100,000 Gross Tons as far as 80 km inland. Like the Port of Hamburg, the Port of Antwerp's inland location provides a more central location in Europe than the majority of North Sea ports. Antwerp's docks are connected to the hinterland by rail, road, and river and canal waterways. As a result, the port of Antwerp has become one of Europe's largest seaports, ranking second behind Rotterdam by total freight shipped. Its international rankings vary from 11th to 20th ( AAPA). In 2012, the Port of Antwerp handled 14,220 sea trade ships (190.8 milli ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scheldt–Rhine Canal
The Scheldt–Rhine Canal (Schelde-Rijnkanaal) in Belgium and the Netherlands connects Antwerp with the Volkerak, and thereby the Scheldt with the Rhine. Route The canal starts close to the Scheldt river, at the port of Antwerp, and generally runs north. After it passes the Dutch-Belgian border, it serves as the border between the Dutch provinces of North Brabant and Zeeland. Just north of Zuid-Beveland ships have to pass the to enter the lower part of the canal. Just north of the sluices the canal enters the artificial and leaves this lake again as a canalised section of the former Eendracht strait, before terminating in the Volkerak estuary. Here, the provide access to the Rhine-Meuse Delta and the port of Rotterdam. History During the 1920s the Belgian government demanded a replacement for the Canal through Zuid-Beveland, to keep the port of Antwerp accessible for the lucrative Rhine trade. According to the original plan, the new canal was supposed to connect Antwerp di ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eastern Scheldt
The Eastern Scheldt ( nl, Oosterschelde) is a former estuary in the province of Zeeland, Netherlands, between Schouwen-Duiveland and Tholen on the north and Noord-Beveland and Zuid-Beveland on the south. It also features the largest national park in the Netherlands, founded in 2002. Landscape and history During the Roman Era it was the major mouth of the Scheldt River. Before the St. Felix's Flood of 1530, it flowed north as a river from the east end of the Westerschelde, turned west a little west of Bergen op Zoom, and then west along the north edge of what is now the Verdronken Land van Reimerswaal, and after that widened into an estuary. Later parts of that lost land were reclaimed, restricting part of the connection to the Scheldt River to a narrow channel called the Kreekrak, which silted up and became unnavigable. In 1867 the Kreekrak was closed off with a railway embankment, connecting in the process the island of Zuid-Beveland to the mainland of North Brabant. Fr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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