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Waterwolf
Waterwolf, or Water-wolf is a Dutch people, Dutch word that comes from the Netherlands, which refers to the tendency of lakes in low lying peaty land, sometimes previously worn-down by men digging peat for fuel, to enlarge or expand by flooding, thus Erosion, eroding the lake shores, and potentially causing harm to infrastructure, or death. The term waterwolf is an example of zoomorphism, in which a non-living thing is given traits or characteristics of an animal (whereas a non-living thing given human traits or characteristics is personification). The traits of a wolf most commonly given to lakes include "something to be feared", "quick and relentless", "an enemy of man". The Netherlands, meaning 'low countries', is a nation where 18% of the land is below sea level, and half of the land under one meter above sea level, and is prone to flooding. Before modern flood control, severe storms could cause flooding that could wipe out whole villages in the area of the waterwolf. Much of t ...
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Zoomorphism
The word ''zoomorphism'' derives from and . In the context of art, zoomorphism could describe art that imagines humans as non-human animals. It can also be defined as art that portrays one species of animal like another species of animal or art that uses animals as a visual motif, sometimes referred to as "animal style". Depicting deities in animal form (theriomorphism) is an example of zoomorphism in a religious context. It is also similar to the term Shapeshifting, therianthropy; which is the ability to shape shift into animal form, except that with zoomorphism the animal form is applied to a physical object. It means to attribute animal forms or animal characteristics to other animals, or things other than an animal; similar to but broader than anthropomorphism. Contrary to anthropomorphism, which views animal or non-animal behavior in human terms, zoomorphism is the tendency of viewing human behavior in terms of the behavior of animals. It is also used in literature to portray ...
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Carbon Sequestration
Carbon sequestration is the process of storing carbon in a carbon pool. It plays a crucial role in Climate change mitigation, limiting climate change by reducing the amount of Carbon dioxide in Earth's atmosphere, carbon dioxide in the atmosphere. There are two main types of carbon sequestration: biologic (also called ''biosequestration'') and geologic. Biologic carbon sequestration is a naturally occurring process as part of the carbon cycle. Humans can enhance it through deliberate actions and use of technology. Carbon dioxide () is naturally captured from the atmosphere through biological, chemical, and physical processes. These processes can be accelerated for example through changes in land use and agricultural practices, called carbon farming. Artificial processes have also been devised to produce similar effects. This approach is called carbon capture and storage. It involves using technology to capture and sequester (store) that is produced from human activities under ...
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Lakes Of The Netherlands
The Netherlands Environmental Assessment Agency published a map of surface water bodies in the Netherlands in 2010. The map distinguishes over 20 different types of water bodies, including those with salty, brackish and fresh water. These water bodies encompass natural and artificial lakes of varying sizes, peat puddles and fens. The total combined surface area of the lakes larger than is . While a comprehensive list of past and present lakes in the Netherlands is not available, selected lists can be found. Groups of lakes Within the Netherlands, there are several groups of lakes or lake systems that are often referred to as a whole. Examples include: * Frisian Lakes, a group of 24 lakes located in the province of Friesland * Borderling lakes, a body of water surrounding the Flevopolder often divided into ten parts or lakes Lakes The following is a list of lakes of the Netherlands. Ancient lakes The waterscape of the Netherlands undergoes continuous change. The followi ...
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Sea Level Rise
The sea level has been rising from the end of the last ice age, which was around 20,000 years ago. Between 1901 and 2018, the average sea level rose by , with an increase of per year since the 1970s. This was faster than the sea level had ever risen over at least the past 3,000 years. The rate accelerated to /yr for the decade 2013–2022. Climate change due to human activities is the main cause. Between 1993 and 2018, melting ice sheets and glaciers accounted for 44% of sea level rise, with another 42% resulting from thermal expansion of water. Sea level rise lags behind changes in the Earth's temperature by decades, and sea level rise will therefore continue to accelerate between now and 2050 in response to warming that has already happened. What happens after that depends on future human greenhouse gas emissions. If there are very deep cuts in emissions, sea level rise would slow between 2050 and 2100. The reported factors of increase in flood hazard potential are often e ...
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Flood Control In The Netherlands
Flood control is an important issue for the Netherlands, as due to its low elevation, approximately two thirds of its area is vulnerable to flooding, while the country is densely populated. Natural sand dunes and constructed Dike (construction), dikes, dams, and floodgates provide defense against storm surges from the sea. River dikes prevent flooding from water flowing into the country by the major rivers Rhine and Meuse (river), Meuse, while a complicated system of drainage ditches, canals, and pumping stations (historically: windmills) keep the low-lying parts dry for habitation and agriculture. Water board (Netherlands), Water control boards are the independent local government bodies responsible for maintaining this system. In modern times, Floods in the Netherlands, flood disasters coupled with technological developments have led to large construction works to reduce the influence of the sea and prevent future floods. These have proved essential over the course of Dutch his ...
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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 ...
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Levee
A levee ( or ), dike (American English), dyke (British English; see American and British English spelling differences#Miscellaneous spelling differences, spelling differences), embankment, floodbank, or stop bank is an elevated ridge, natural or artificial, alongside the river banks, banks of a river, often intended to flood control, protect against flooding of the area adjoining the river. It is usually soil, earthen and often runs parallel (geometry), parallel to the course of a river in its floodplain or along low-lying coastlines. Naturally occurring levees form on river floodplains following flooding. Sediment and alluvium are deposition (geology), deposited on the banks and settle, forming a ridge that increases the river channel's capacity. Alternatively, levees can be artificially constructed from fill dirt, fill, designed to regulate water levels. In some circumstances, artificial levees can be environmental degradation, environmentally damaging. Ancient civilization ...
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Water Table
The water table is the upper surface of the phreatic zone or zone of saturation. The zone of saturation is where the pores and fractures of the ground are saturated with groundwater, which may be fresh, saline, or brackish, depending on the locality. It can also be simply explained as the depth below which the ground is saturated. The portion above the water table is the vadose zone. It may be visualized as the "surface" of the subsurface materials that are saturated with groundwater in a given vicinity. In coarse soils, the water table settles at the surface where the water Hydraulic head, pressure head is equal to the atmospheric pressure (where gauge pressure = 0). In soils where capillary action is strong, the water table is pulled upward, forming a capillary fringe. The groundwater may be from precipitation or from more distant groundwater flowing into the aquifer. In areas with sufficient precipitation, water infiltrates through pore spaces in the soil, passing through t ...
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Polder
A polder () is a low-lying tract of land that forms an artificial hydrology, hydrological entity, enclosed by embankments known as levee, dikes. The three types of polder are: # Land reclamation, Land reclaimed from a body of water, such as a lake or the seabed # Floodplain, 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 subsidence, 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 (hydrology), 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. Pold ...
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Windmills In The Netherlands
Windmills are known worldwide as an iconic symbol of Dutch culture. Some 1,200 historic windmills survive, most of which are gristmills or polder mills. Many remain fully functional, and their upkeep and operation is promoted by a number of civic organizations, including ''De Hollandsche Molen'', '' Gilde van Vrijwillige Molenaars'' and ''Stichting De Fryske Mole''. Several Dutch villages are known for their concentration of windmills, including Kinderdijk, Zaanse Schans, and Schiedam, home to the tallest windmill in the world. Tjaskers, a kind of windmill native to Friesland, were also used for water management. This list of windmills in the Netherlands is grouped by province. Types of Dutch windmills include: File:Sprang - molen Dye Sprancke.jpg, ''Standerdmolen'' (post mill) File:Wipmolen.jpg, ''Wipmolen'' File:Molen Heechhiem 01.JPG, ''Spinnenkopmolen'' ("Spider's head") File:20080606 Tjasker Meestersveen Zeijen NL.jpg, ''Tjasker'' File:Paltrokmolen zijaanzicht.jpg, ''Paltrok ...
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