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Merwede Canal
The Merwede (; etymology uncertain, possibly derived from the Old Dutch ''merwe'' or ''merowe'', a word meaning "wide water") is the name of several connected stretches of river in the Netherlands, between the cities of Woudrichem, Dordrecht and Papendrecht. The river is part of the Rhine–Meuse–Scheldt delta and is mostly fed by the river Rhine. At first, a disconnected branch of the Meuse joins the Waal at Woudrichem to form the Boven Merwede (Upper Merwede). A few kilometers downstream it splits into the Beneden Merwede (Lower Merwede) on the right and the Nieuwe Merwede (New Merwede) on the left. All these rivers are tidal. The Nieuwe Merwede joins the Bergse Maas near Lage Zwaluwe to form the Hollands Diep estuary, and separates the Island of Dordrecht from the Biesbosch National Park. The Beneden Merwede splits into the Noord River and Oude Maas near Papendrecht. History In medieval times the name Merwede (or "Merwe" in Middle Dutch) was the name of a continuous stretch ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rijn Maas Delta
The Rhine ( ) is one of the major rivers in Europe. The river begins in the Swiss canton of Graubünden in the southeastern Swiss Alps. It forms part of the Swiss-Liechtenstein border, then part of the Swiss-Austrian border. From Lake Constance downstream, it forms part of the Swiss-German border. After that the Rhine defines much of the Franco-German border. It then flows in a mostly northerly direction through the German Rhineland. Finally, the Rhine turns to flow predominantly west to enter the Netherlands, eventually emptying into the North Sea. It drains an area of 185,000 km2. Its name derives from the Gaulish ''Rēnos''. There are two German states named after the river, North Rhine-Westphalia and Rhineland-Palatinate, in addition to several districts (e.g. Rhein-Sieg). The departments of Bas-Rhin and Haut-Rhin in Alsace (France) are also named after the river. Some adjacent towns are named after it, such as Rheinau, Stein am Rhein, Rheineck, Rheinfelden (S ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oude Maas
The Oude Maas (; ) is a distributary of the river Rhine, and a former distributary of the river Maas, in the Dutch province of South Holland. It begins at the city of Dordrecht where the Beneden Merwede river splits into the Noord and the Oude Maas. It ends when it joins the Nieuwe Maas to form Het Scheur. Geography The Oude Maas forms the southern boundary of the IJsselmonde island. Soon after Dordrecht the Dordtsche Kil forks off and after that the Oude Maas forms the northern boundary of the Hoeksche Waard island, flowing west until the Spui river forks off at the town of Oud-Beijerland. The Oude Maas then heads northwest between the towns/cities of Spijkenisse and Hoogvliet and joins the river Nieuwe Maas opposite the city of Vlaardingen. The combined river is known as Het Scheur and flows to the North Sea. The river is tidal and has nature and recreation areas. History During the early Middle Ages the main flow of the Maas followed the current Oude Maas. D ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alblasserwaard
The Alblasserwaard () is a polder in the province of South Holland, Netherlands. It is mainly known for the windmills of Kinderdijk, located near the village of Kinderdijk in the polder's northwestern part. History The first human inhabitants of the Alblasserwaard settled there after the last ice age, around 10.000 years ago. The ice had not reached the area itself, but eolian deposits created high points in the wet environment. These high points were places where hunter-gatherers settled, as archaeological investigations in the area have shown. During the Middle Ages, several canals and dikes were created to reclaim the land. The last part was diked in the second half of the 14th century, following the permanent flooding of Woude and Donkersloot. However, numerous floods continued to happen throughout the history of the area, as it is bound by rivers and watercourses on all sides. During World War II, the Bombing of Rotterdam also damaged the Alblasserwaard, when both th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rivers Of The Netherlands
These are the main rivers of the Netherlands. All of the Netherlands is drained into the North Sea, partly via the IJsselmeer lake. In the list below, rivers that flow into the sea are sorted following the North Sea coast (including IJsselmeer) from the Belgian border near Knokke to the German border near Emden. Rivers that flow into other rivers are sorted by the proximity of their points of confluence to the sea. At the end of this article the rivers of the Netherlands are given alphabetically. See also :Rivers of the Netherlands and :Rhine-Meuse-Scheldt delta. Note for additions: please remember to add the city where the river meets for each river. *Western Scheldt/Westerschelde (at Vlissingen) **Scheldt/Schelde (near Antwerp, Zandvliet, Belgium) *Oosterschelde (at Schouwen-Duiveland, Westenschouwen) **Keeten-Mastgat (at Tholen, Stavenisse) ***branch of Krammer (at Schouwen-Duiveland, Bruinisse) *Grevelingen (at Schouwen-Duiveland, Scharendijke) **Krammer (at Schouwen-Duivelan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rivers Of South Holland
A river is a natural stream of fresh water that flows on land or inside caves towards another body of water at a lower elevation, such as an ocean, lake, or another river. A river may run dry before reaching the end of its course if it runs out of water, or only flow during certain seasons. Rivers are regulated by the water cycle, the processes by which water moves around the Earth. Water first enters rivers through precipitation, whether from rainfall, the runoff of water down a slope, the melting of glaciers or snow, or seepage from aquifers beneath the surface of the Earth. Rivers flow in channeled watercourses and merge in confluences to form drainage basins, or catchments, areas where surface water eventually flows to a common outlet. Rivers have a great effect on the landscape around them. They may regularly overflow their banks and flood the surrounding area, spreading nutrients to the surrounding area. Sediment or alluvium carried by rivers shapes the landscape aro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Distributaries Of Europe
A distributary, or a distributary channel is a stream channel that branches off and flows a main stream channel. It is the opposite of a ''tributary'', a stream that flows another stream or river. Distributaries are a result of river bifurcation and are often found where a river approaches a lake or an ocean and divides into distributary networks; as such they are a common feature of river deltas. They can also occur inland, on alluvial fans, or where a tributary stream bifurcates as it nears its confluence with a larger stream. In some cases, a minor distributary can divert so much water from the main channel that it can later become the main route. Related terms Common terms to name individual river distributaries in English-speaking countries are ''arm'' and ''channel''. These terms may refer to a distributary that does not rejoin the channel from which it has branched (e.g., the North, Middle, and South Arms of the Fraser River, or the West Channel of the Mackenzie River) ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rivers Of The Rhine–Meuse–Scheldt Delta
A river is a natural stream of fresh water that flows on land or inside caves towards another body of water at a lower elevation, such as an ocean, lake, or another river. A river may run dry before reaching the end of its course if it runs out of water, or only flow during certain seasons. Rivers are regulated by the water cycle, the processes by which water moves around the Earth. Water first enters rivers through precipitation, whether from rainfall, the runoff of water down a slope, the melting of glaciers or snow, or seepage from aquifers beneath the surface of the Earth. Rivers flow in channeled watercourses and merge in confluences to form drainage basins, or catchments, areas where surface water eventually flows to a common outlet. Rivers have a great effect on the landscape around them. They may regularly overflow their banks and flood the surrounding area, spreading nutrients to the surrounding area. Sediment or alluvium carried by rivers shapes the landscape ar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Merovingian Dynasty
The Merovingian dynasty () was the ruling family of the Franks from around the middle of the 5th century until Pepin the Short in 751. They first appear as "Kings of the Franks" in the Roman army of northern Gaul. By 509 they had united all the Franks and northern Gallo-Romans under their rule. They conquered most of Gaul, defeating the Visigoths (507) and the Burgundians (534), and also extended their rule into Raetia (537). In Germania, the Alemanni, Bavarii and Saxons accepted their lordship. The Merovingian realm was the largest and most powerful of the states of western Europe following the breakup of the empire of Theodoric the Great. The dynastic name, medieval Latin or ("sons of Merovech"), derives from an unattested Frankish language, Frankish form, akin to the attested Old English , with the final -''ing'' being a typical Germanic languages, Germanic patronymic suffix. The name derives from Salian Franks, Salian King Merovech, who is at the center of many legends. Unl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Delta Works
The Delta Works () is a series of construction projects in the southwest of the Netherlands to protect a large area of land around the Rhine–Meuse–Scheldt delta from the sea. Constructed between 1954 and 1997, the works consist of dams, sluices, Lock (water transport), locks, Levee, dykes, levees, and floodgate, storm surge barriers located in the provinces of the Netherlands, provinces of South Holland and Zeeland. The aim of the dams, sluices, and storm surge barriers was to shorten the Dutch coastline, thus reducing the number of dikes that had to be raised. Along with the Zuiderzee Works, the Delta Works have been declared one of the Seven Wonders of the Modern World by the American Society of Civil Engineers. History Due to indecision and the World War II, Second World War, little action was taken. In 1950 two small estuary mouths, the Brielse Gat near Brielle and the Botlek near Vlaardingen were dammed. After the North Sea flood of 1953, a Delta Works Commission w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Zuiderzee Works
The Zuiderzee Works () is a system of dams and Levee, dikes, land reclamation and water drainage work, which was the largest hydraulic engineering project undertaken by the Netherlands during the twentieth century. The project involved the damming of the Zuiderzee, a large, shallow inlet of the North Sea, and the reclamation of land in the newly enclosed water using polders. Its main purposes are to improve flood protection and create additional land for agriculture. The enormous scale of the works required the creation of a joint venture company comprising several large Dredging, dredging contractors, known as the Maatschappij tot Uitvoering van Zuiderzeewerken. The American Society of Civil Engineers declared the works, together with the Delta Works in the South-West of the Netherlands, as among the Wonders of the World#Wonders of the modern world, Seven Wonders of the Modern World. Background The Low Countries have low flat topography, with half the land area below or less t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Haringvliet
The Haringvliet is a large inlet of the North Sea, in the province of South Holland in the Netherlands. It is an important estuary of the Rhine-Meuse delta. Near Numansdorp, the Hollands Diep splits into the Haringvliet and the Volkerak estuaries. It is closed off near Goedereede from the North Sea by the Haringvlietdam, which provides a road connection between the island of Voorne to the north and the island of Goeree-Overflakkee to the south. The dam with its sluices was built as part of the Delta Works sea barrier protection works. The Haringvliet estuary contains the island of Tiengemeten, which is separated from the river island of Hoeksche Waard by the Vuile Gat strait. History The Haringvliet was formed as a result of the extensive flooding event of 1216, which breached the dunes of Voorne and created a deep saltwater inlet. During a second flooding event, the St. Elizabeth floods of 1421, this inlet connected to the Merwede and became an important estuary of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
