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Eendracht
The Eendracht is a former tidal branch of river Scheldt that has been channelised to form the northern stretch of the Scheldt-Rhine Canal. It flows from the Zoommeer lake (formerly part of the Oosterschelde) near Bergen op Zoom past the town and eponymous island of Tholen towards the former island of Sint Philipsland, where it used to end in the Krabbenkreek estuary. The passage to the estuary has been closed off, however, and an additional stretch of canal was dug to connect the Eendracht to the Krammer lake, itself a former estuary closed off from the sea during the Delta Works. The Eendracht is probably the last remaining remnant of the Striene De Striene was a water channel that ran between the Schelde near Tholen and the Maas rivers in Zeeland in the Netherlands. In the St. Elizabeth's Flood of 1421 the watercourses in the Maas and Rhine delta were drastically changed, and the Striene ... river. {{Rhine–Meuse–Scheldt delta Canals in the Rhine–Meuse–Scheld ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tholen
Tholen () is a 25,000 people 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. 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 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 there are three villages: On the island Tholen there are seven population centers: ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sint Philipsland (island)
Sint Philipsland is a former island in the Dutch province of Zeeland. Nowadays it is part of the municipality of Tholen. It contains the villages of Sint Philipsland and Anna Jacobapolder Anna Jacobapolder is a village in the Dutch province of Zeeland. It is a part of the municipality of Tholen, and lies about 20 km north west of Bergen op Zoom. History The village was first mentioned between 1838 and 1857 as AandenNoordweg ..., and also the hamlet of De Sluis. Peninsulas of the Netherlands Former islands of Zeeland Regions of Zeeland Tholen {{Zeeland-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canals In North Brabant
Canals or artificial waterways are waterways or engineered channels built for drainage management (e.g. flood control and irrigation) or for conveyancing water transport vehicles (e.g. water taxi). They carry free, calm surface flow under atmospheric pressure, and can be thought of as artificial rivers. In most cases, a canal has a series of dams and locks that create reservoirs of low speed current flow. These reservoirs are referred to as ''slack water levels'', often just called ''levels''. A canal can be called a ''navigation canal'' when it parallels a natural river and shares part of the latter's discharges and drainage basin, and leverages its resources by building dams and locks to increase and lengthen its stretches of slack water levels while staying in its valley. A canal can cut across a drainage divide atop a ridge, generally requiring an external water source above the highest elevation. The best-known example of such a canal is the Panama Canal. Many ca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canals In The Rhine–Meuse–Scheldt Delta
Canals or artificial waterways are waterways or engineered channels built for drainage management (e.g. flood control and irrigation) or for conveyancing water transport vehicles (e.g. water taxi). They carry free, calm surface flow under atmospheric pressure, and can be thought of as artificial rivers. In most cases, a canal has a series of dams and locks that create reservoirs of low speed current flow. These reservoirs are referred to as ''slack water levels'', often just called ''levels''. A canal can be called a ''navigation canal'' when it parallels a natural river and shares part of the latter's discharges and drainage basin, and leverages its resources by building dams and locks to increase and lengthen its stretches of slack water levels while staying in its valley. A canal can cut across a drainage divide atop a ridge, generally requiring an external water source above the highest elevation. The best-known example of such a canal is the Panama Canal. Ma ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Striene
De Striene was a water channel that ran between the Schelde near Tholen and the Meuse (river), Maas rivers in Zeeland in the Netherlands. In the St. Elizabeth's flood (1421), St. Elizabeth's Flood of 1421 the watercourses in the Maas and Rhine delta were drastically changed, and the Striene disappeared. However, the current Scheldt-Rhine Canal mostly follows the ancient path of the Striene. The place names Strijen, Cromstrijen, and Strijenham on Tholen are probably derived from ''Striene''. The name Strienestad used for Steenbergen in North Brabant during the Carnival, also refers to the Striene. References History of South Holland History of Zeeland Tholen Former rivers {{Zeeland-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Delta Works
The Delta Works ( nl, Deltawerken) 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, locks, dykes, levees, and storm surge barriers located in the 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 The estuaries of the rivers Rhine, Meuse and Schelde have been subject to flooding over the centuries. After building the Afsluitdijk (19271932), the Dutch started studying the damming of the Rhine-Meuse Delta. Plans were developed to shorten the coastline and turn the delta into a group of freshwater ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Krammer (Netherlands)
The Krammer is a body of fresh water located in the western part of Volkerak in the Netherlands. It is part of the Rhine–Meuse–Scheldt delta, and is situated between the islands Goeree-Overflakkee and Sint Philipsland. To the west, it continues into the Grevelingen, from which it is separated by the Grevelingendam. Before 1967, it was a tidal river, but it was closed off as part of the Delta Works The Delta Works ( nl, Deltawerken) 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 con .... Goeree-Overflakkee Tholen Delta Works Landforms of South Holland Landforms of Zeeland {{Netherlands-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canal
Canals or artificial waterways are waterways or engineered channels built for drainage management (e.g. flood control and irrigation) or for conveyancing water transport vehicles (e.g. water taxi). They carry free, calm surface flow under atmospheric pressure, and can be thought of as artificial rivers. In most cases, a canal has a series of dams and locks that create reservoirs of low speed current flow. These reservoirs are referred to as ''slack water levels'', often just called ''levels''. A canal can be called a ''navigation canal'' when it parallels a natural river and shares part of the latter's discharges and drainage basin, and leverages its resources by building dams and locks to increase and lengthen its stretches of slack water levels while staying in its valley. A canal can cut across a drainage divide atop a ridge, generally requiring an external water source above the highest elevation. The best-known example of such a canal is the Panama Canal. Many ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Estuary
An estuary is a partially enclosed coastal body of brackish water with one or more rivers or streams flowing into it, and with a free connection to the open sea. Estuaries form a transition zone between river environments and maritime environments and are an example of an ecotone. Estuaries are subject both to marine influences such as tides, waves, and the influx of saline water, and to fluvial influences such as flows of freshwater and sediment. The mixing of seawater and freshwater provides high levels of nutrients both in the water column and in sediment, making estuaries among the most productive natural habitats in the world. Most existing estuaries formed during the Holocene epoch with the flooding of river-eroded or glacially scoured valleys when the sea level began to rise about 10,000–12,000 years ago. Estuaries are typically classified according to their geomorphological features or to water-circulation patterns. They can have many different names, such as bays, ... [...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 gravity, 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, 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, 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 cycle, diurnal tide—one high and low tide each day. A "mixed tide"—two uneven magnitude ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River
A river is a natural flowing watercourse, usually freshwater, flowing towards an ocean, sea, lake or another river. In some cases, a river flows into the ground and becomes dry at the end of its course without reaching another body of water. Small rivers can be referred to using names such as Stream#Creek, creek, Stream#Brook, brook, rivulet, and rill. There are no official definitions for the generic term river as applied to Geographical feature, geographic features, although in some countries or communities a stream is defined by its size. Many names for small rivers are specific to geographic location; examples are "run" in some parts of the United States, "Burn (landform), burn" in Scotland and northeast England, and "beck" in northern England. Sometimes a river is defined as being larger than a creek, but not always: the language is vague. Rivers are part of the water cycle. Water generally collects in a river from Precipitation (meteorology), precipitation through a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
