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Eendracht Aalst Ladies
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] |
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] |
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] |
