70-595: Texel ( Dutch pronunciation: [ˈtɛsəl] ; Texels dialect: Tessel ) is a municipality and an island with a population of 13,643 in North Holland , Netherlands . It is the largest and most populated island of the West Frisian Islands in the Wadden Sea . The island is situated north of Den Helder , northeast of Noorderhaaks , and southwest of Vlieland . The name Texel
140-414: A breach may experience flooding similar to a natural event, while damage near a breach can be catastrophic, including carving out deep holes and channels in the nearby landscape. Under natural conditions, floodwaters return quickly to the river channel as water-levels drop. During a levee breach, water pours out into the floodplain and moves down-slope where it is blocked from return to the river. Flooding
210-562: A certain degree of independence in their policy decisions. Municipalities are responsible for a wide variety of public services , which include land-use planning , public housing , management and maintenance of local roads, waste management and social security . After the Dissolution of the Netherlands Antilles in 2010 three special municipalities (officially public bodies ) were formed. These municipalities function
280-537: A density of 6,868/km (17,790/sq mi). As a second level administrative division municipalities are the third tier of public administration in the Netherlands after the central government and the provinces . The Netherlands is a decentralized unitary state , which means that the central government is supreme and delegates certain tasks to lower levels of government by law. The different levels do, however, make work agreements, which give municipalities
350-612: A distance of some 610 km (380 mi). The scope and scale of the Mississippi levees has often been compared to the Great Wall of China . The United States Army Corps of Engineers (USACE) recommends and supports cellular confinement technology (geocells) as a best management practice. Particular attention is given to the matter of surface erosion, overtopping prevention and protection of levee crest and downstream slope. Reinforcement with geocells provides tensile force to
420-553: A dyke may be a field wall, generally made with dry stone . The main purpose of artificial levees is to prevent flooding of the adjoining countryside and to slow natural course changes in a waterway to provide reliable shipping lanes for maritime commerce over time; they also confine the flow of the river, resulting in higher and faster water flow. Levees can be mainly found along the sea, where dunes are not strong enough, along rivers for protection against high floods, along lakes or along polders . Furthermore, levees have been built for
490-677: A flood emergency. Some of the earliest levees were constructed by the Indus Valley civilization (in Pakistan and North India from c. 2600 BCE ) on which the agrarian life of the Harappan peoples depended. Levees were also constructed over 3,000 years ago in ancient Egypt , where a system of levees was built along the left bank of the River Nile for more than 1,000 kilometers (600 miles), stretching from modern Aswan to
560-444: A high suspended sediment fraction and thus are intimately associated with meandering channels, which also are more likely to occur where a river carries large fractions of suspended sediment. For similar reasons, they are also common in tidal creeks, where tides bring in large amounts of coastal silts and muds. High spring tides will cause flooding, and result in the building up of levees. Both natural and man-made levees can fail in
630-419: A land area of 7.01 km (2.71 sq mi) and Súdwest-Fryslân the largest with a land area of 522.7 km (201.8 sq mi). Schiermonnikoog is both the least populated, with 972 people, and the least densely populated municipality at 23/km (60/sq mi). Amsterdam has the highest population with 931,298 residents as of January 2024, whereas The Hague is the most densely populated with
700-428: A number of ways. Factors that cause levee failure include overtopping, erosion, structural failures, and levee saturation. The most frequent (and dangerous) is a levee breach . Here, a part of the levee actually breaks or is eroded away, leaving a large opening for water to flood land otherwise protected by the levee. A breach can be a sudden or gradual failure, caused either by surface erosion or by subsurface weakness in
770-412: A shorter route to the ocean and begin building a new delta. Wave action and ocean currents redistribute some of the sediment to build beaches along the coast. When levees are constructed all the way to the ocean, sediments from flooding events are cut off, the river never migrates, and elevated river velocity delivers sediment to deep water where wave action and ocean currents cannot redistribute. Instead of
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#1732768518592840-421: A shorter time interval means higher river stage (height). As more levees are built upstream, the recurrence interval for high-water events in the river increases, often requiring increases in levee height. During natural flooding, water spilling over banks rises slowly. When a levee fails, a wall of water held back by the levee suddenly pours out over the landscape, much like a dam break. Impacted areas far from
910-410: A time by the crown and the alderman are elected by the municipal council, typically after each municipal election. The mayor is responsible for public order and is the first in command during emergencies, all other tasks are distributed freely between mayor and aldermen. The exact portfolio for each person differs between each municipality. Official municipal boundaries were first drawn up in 1832 in
980-459: Is Frisian , but because of historical sound-changes in Dutch , where all -x- sounds have been replaced with -s- sounds (compare for instance English fox , Frisian fokse , German Fuchs with Dutch vos ), the name is typically pronounced Tessel in Dutch. The All Saints' Flood (1170) created the islands of Texel and Wieringen from North Holland . In the 13th century Ada, Countess of Holland
1050-537: Is electrical resistivity tomography (ERT). This non-destructive geophysical method can detect in advance critical saturation areas in embankments. ERT can thus be used in monitoring of seepage phenomena in earth structures and act as an early warning system, e.g., in critical parts of levees or embankments. Large scale structures designed to modify natural processes inevitably have some drawbacks or negative impacts. Levees interrupt floodplain ecosystems that developed under conditions of seasonal flooding. In many cases,
1120-527: Is a protected nature reserve. A wetland called Utopia has been designed for birds to nest in. Texel has an oceanic climate ( Köppen Cfb ) that is heavily influenced by its offshore position. The annual average high oscillation is between 5 °C (41 °F) and 21 °C (70 °F). While winters are similar to mainland areas, summers remain cooler. The relative proximity to the mainland still renders heat bursts to reach Texel with five months having recorded temperatures above 30 °C (86 °F). While
1190-546: Is below mean sea level. These typically man-made hydraulic structures are situated to protect against erosion. They are typically placed in alluvial rivers perpendicular, or at an angle, to the bank of the channel or the revetment , and are used widely along coastlines. There are two common types of spur dyke, permeable and impermeable, depending on the materials used to construct them. Natural levees commonly form around lowland rivers and creeks without human intervention. They are elongated ridges of mud and/or silt that form on
1260-405: Is elected every four years. Municipal mergers have reduced the total number of municipalities by two-thirds since the first official boundaries were created in the mid 19th century. Municipalities themselves are informally subdivided into districts and neighbourhoods for administrative and statistical purposes. These municipalities come in a wide range of sizes, Westervoort is the smallest with
1330-420: Is important in order to design stable levee and floodwalls . There have been numerous studies to investigate the erodibility of soils. Briaud et al. (2008) used Erosion Function Apparatus (EFA) test to measure the erodibility of the soils and afterwards by using Chen 3D software, numerical simulations were performed on the levee to find out the velocity vectors in the overtopping water and the generated scour when
1400-451: Is permanently diverted through the gap. Sometimes levees are said to fail when water overtops the crest of the levee. This will cause flooding on the floodplains, but because it does not damage the levee, it has fewer consequences for future flooding. Among various failure mechanisms that cause levee breaches, soil erosion is found to be one of the most important factors. Predicting soil erosion and scour generation when overtopping happens
1470-573: Is prolonged over such areas, waiting for floodwater to slowly infiltrate and evaporate. Natural flooding adds a layer of sediment to the floodplain. The added weight of such layers over many centuries makes the crust sink deeper into the mantle , much like a floating block of wood is pushed deeper into the water if another board is added on top. The momentum of downward movement does not immediately stop when new sediment layers stop being added, resulting in subsidence (sinking of land surface). In coastal areas, this results in land dipping below sea level,
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#17327685185921540-456: Is the dune "Bertusnol" (also "Nol van Bertus"), which is situated in the Dunes of Texel National Park , at 19.6 m. The dune landscape on Texel is an important habitat for wildlife. Notable areas include De Slufter , where the tide comes in and meets the dunes, forming a marshy environment rich in both fauna and flora. In winter, birds of prey and geese take up residence. About a third of Texel
1610-700: The First World War in 1914, the Battle off Texel took place off the coast of Texel. On the night of 31 August 1940, the sea to the northwest of Texel was the scene of the sinking of two Royal Navy destroyers and the severe damage of a third by German mines in what is known as the Texel Disaster . At the end of the Second World War in 1945, the Georgian uprising on Texel took place on
1680-535: The Indus Valley , ancient Egypt, Mesopotamia and China all built levees. Today, levees can be found around the world, and failures of levees due to erosion or other causes can be major disasters, such as the catastrophic 2005 levee failures in Greater New Orleans that occurred as a result of Hurricane Katrina . Speakers of American English use the word levee , from the French word levée (from
1750-541: The Netherlands . The latter is the status of three of the six island territories that make up the Dutch Caribbean . Municipalities are the second-level administrative division, or public bodies ( Dutch : openbare lichamen ), in the Netherlands and are subdivisions of their respective provinces . Their duties are delegated to them by the central government and they are ruled by a municipal council that
1820-525: The Nile Delta on the shores of the Mediterranean . The Mesopotamian civilizations and ancient China also built large levee systems. Because a levee is only as strong as its weakest point, the height and standards of construction have to be consistent along its length. Some authorities have argued that this requires a strong governing authority to guide the work and may have been a catalyst for
1890-457: The bank . It closely parallels the English verb to dig . In Anglo-Saxon , the word dic already existed and was pronounced as dick in northern England and as ditch in the south. Similar to Dutch, the English origins of the word lie in digging a trench and forming the upcast soil into a bank alongside it. This practice has meant that the name may be given to either the excavation or to
1960-791: The catchwater drain , Car Dyke, to the South Forty Foot Drain in Lincolnshire (TF1427). The Weir Dike is a soak dike in Bourne North Fen , near Twenty and alongside the River Glen , Lincolnshire . In the Norfolk and Suffolk Broads , a dyke may be a drainage ditch or a narrow artificial channel off a river or broad for access or mooring, some longer dykes being named, e.g., Candle Dyke. In parts of Britain , particularly Scotland and Northern England ,
2030-638: The Mississippi, stretching from Cape Girardeau , Missouri , to the Mississippi delta . They were begun by French settlers in Louisiana in the 18th century to protect the city of New Orleans . The first Louisiana levees were about 90 cm (3 ft) high and covered a distance of about 80 km (50 mi) along the riverside. The U.S. Army Corps of Engineers, in conjunction with the Mississippi River Commission, extended
2100-605: The Netherlands after a cadastre was formed. The Municipalities Act of 1851, written by prime minister Thorbecke , led to the disappearance of small municipalities. Throughout the years, less populous municipalities have been merged . They were either added to the larger neighbouring cities or multiple smaller municipalities merged into a larger new municipality with a new name. The number of municipalities reduced from 1,209 in 1850 to 537 in 2000; since 2024 there have been 342 municipalities. During this time, multiple mergers occurred simultaneously in large parts of individual provinces;
2170-614: The bank. Thus Offa's Dyke is a combined structure and Car Dyke is a trench – though it once had raised banks as well. In the English Midlands and East Anglia , and in the United States, a dike is what a ditch is in the south of England, a property-boundary marker or drainage channel. Where it carries a stream, it may be called a running dike as in Rippingale Running Dike , which leads water from
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2240-637: The city of Vancouver , British Columbia , there are levees (known locally as dikes, and also referred to as "the sea wall") to protect low-lying land in the Fraser River delta, particularly the city of Richmond on Lulu Island . There are also dikes to protect other locations which have flooded in the past, such as the Pitt Polder, land adjacent to the Pitt River , and other tributary rivers. Coastal flood prevention levees are also common along
2310-407: The construction of dikes well attested as early as the 11th century. The 126-kilometer-long (78 mi) Westfriese Omringdijk , completed by 1250, was formed by connecting existing older dikes. The Roman chronicler Tacitus mentions that the rebellious Batavi pierced dikes to flood their land and to protect their retreat (70 CE ). The word dijk originally indicated both the trench and
2380-488: The development of systems of governance in early civilizations. However, others point to evidence of large-scale water-control earthen works such as canals and/or levees dating from before King Scorpion in Predynastic Egypt , during which governance was far less centralized. Another example of a historical levee that protected the growing city-state of Mēxihco-Tenōchtitlan and the neighboring city of Tlatelōlco,
2450-672: The districts are called Dutch : stadsdelen , as well as Rotterdam , where the districts are called Dutch : deelgemeenten , consist of such formal subdivisions. The Hague , Almere , Breda , Eindhoven , Enschede , Groningen , Nijmegen , Tilburg and Utrecht have instituted Dutch : stadsdelen as well, although they do not have the same legal submunicipal status. For administrative use by municipalities and data collection by Statistics Netherlands all municipalities are subdivided into districts ( Dutch : wijken ), which in turn are subdivided into neighbourhoods ( Dutch : buurten ). These subdivisions have, in contrast to
2520-479: The earth together. On the land side of high levees, a low terrace of earth known as a banquette is usually added as another anti-erosion measure. On the river side, erosion from strong waves or currents presents an even greater threat to the integrity of the levee. The effects of erosion are countered by planting suitable vegetation or installing stones, boulders, weighted matting, or concrete revetments . Separate ditches or drainage tiles are constructed to ensure that
2590-579: The feminine past participle of the French verb lever , 'to raise'). It originated in New Orleans a few years after the city's founding in 1718 and was later adopted by English speakers. The name derives from the trait of the levee's ridges being raised higher than both the channel and the surrounding floodplains. The modern word dike or dyke most likely derives from the Dutch word dijk , with
2660-589: The final battle of the Second World War in Europe. Hundreds of Georgians who died fighting against the Germans are buried in a special cemetery on Texel commonly known as the "Russian cemetery". The municipality lies north of the mainland of the province of North Holland and west of the mainland of the province of Friesland . The island of Texel is situated north of the city of Den Helder , northeast of
2730-879: The foundation does not become waterlogged. Prominent levee systems have been built along the Mississippi River and Sacramento River in the United States , and the Po , Rhine , Meuse River , Rhône , Loire , Vistula , the delta formed by the Rhine, Maas/Meuse and Scheldt in the Netherlands and the Danube in Europe . During the Chinese Warring States period , the Dujiangyan irrigation system
2800-450: The impact is two-fold, as reduced recurrence of flooding also facilitates land-use change from forested floodplain to farms. In a natural watershed, floodwaters spread over a landscape and slowly return to the river. Downstream, the delivery of water from the area of flooding is spread out in time. If levees keep the floodwaters inside a narrow channel, the water is delivered downstream over a shorter time period. The same volume of water over
2870-404: The inland coastline behind the Wadden Sea , an area devastated by many historic floods. Thus the peoples and governments have erected increasingly large and complex flood protection levee systems to stop the sea even during storm floods. The biggest of these are the huge levees in the Netherlands , which have gone beyond just defending against floods, as they have aggressively taken back land that
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2940-675: The island is relatively rainy, the precipitation is generally quite even and moderate throughout most of the year although there is a dry peak in late spring and a rain peak in autumn. The tourism industry forms a substantial part of the economy in Texel. Approximately 70% of activities on Texel are in some way related to tourism. Popular forms of tourism on Texel include cycling, walking, swimming and horse riding. Farming (sheep, potatoes, dairy, tulips, and grain) and fishing (primarily from Oudeschild ) are traditional. The municipal council of Texel consists of 15 seats, which are divided as follows (from
3010-405: The island. Following a German decision to redeploy Georgian soldiers to the mainland, they revolted and killed hundreds of their German comrades while they slept. The uprising lasted from 5 April 1945 until 20 May 1945, two weeks after V-E Day . At that point, Canadian troops arrived and arranged for the two sides to separately leave the island. For that reason, the uprising is often referred to as
3080-549: The laboratory tests, empirical correlations related to average overtopping discharge were derived to analyze the resistance of levee against erosion. These equations could only fit to the situation, similar to the experimental tests, while they can give a reasonable estimation if applied to other conditions. Osouli et al. (2014) and Karimpour et al. (2015) conducted lab scale physical modeling of levees to evaluate score characterization of different levees due to floodwall overtopping. Another approach applied to prevent levee failures
3150-528: The levee system beginning in 1882 to cover the riverbanks from Cairo, Illinois to the mouth of the Mississippi delta in Louisiana. By the mid-1980s, they had reached their present extent and averaged 7.3 m (24 ft) in height; some Mississippi levees are as high as 15 m (50 ft). The Mississippi levees also include some of the longest continuous individual levees in the world. One such levee extends southwards from Pine Bluff , Arkansas , for
3220-420: The levee. A breach can leave a fan-shaped deposit of sediment radiating away from the breach, described as a crevasse splay . In natural levees, once a breach has occurred, the gap in the levee will remain until it is again filled in by levee building processes. This increases the chances of future breaches occurring in the same location. Breaches can be the location of meander cutoffs if the river flow direction
3290-475: The levees in the area, created for the purpose of farming the fertile tidal marshlands. These levees are referred to as dykes. They are constructed with hinged sluice gates that open on the falling tide to drain freshwater from the agricultural marshlands and close on the rising tide to prevent seawater from entering behind the dyke. These sluice gates are called " aboiteaux ". In the Lower Mainland around
3360-543: The main channel, this will make levee overtopping more likely again, and the levees can continue to build up. In some cases, this can result in the channel bed eventually rising above the surrounding floodplains, penned in only by the levees around it; an example is the Yellow River in China near the sea, where oceangoing ships appear to sail high above the plain on the elevated river. Levees are common in any river with
3430-445: The majority of The Lake being drained in the 17th century. Levees are usually built by piling earth on a cleared, level surface. Broad at the base, they taper to a level top, where temporary embankments or sandbags can be placed. Because flood discharge intensity increases in levees on both river banks , and because silt deposits raise the level of riverbeds , planning and auxiliary measures are vital. Sections are often set back from
3500-464: The mid-nineteenth century a polder completed the northern half of the island. Today, Texel forms the largest natural barrier between the North Sea and the Wadden Sea . The dune landscape along the western coast of the island is protected as Dunes of Texel National Park . The island is 23.7 km long and 9.6 km wide, its surface is 162.00 square kilometres. The highest point of the island
3570-642: The most recent election results in 2022 : Transport around the island is typically by bicycle, bus (Texelhopper) or car. The island has an extensive cycle path network. It is connected to the mainland via a ferry operated by Royal TESO from Den Helder , and by air via Texel International Airport . The ferry Texelstroom uses 80% compressed natural gas . Municipalities of the Netherlands Since 1 January 2023, there have been 342 regular municipalities ( Dutch : gemeenten ) and three special municipalities ( Dutch : bijzondere gemeenten ) in
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#17327685185923640-466: The municipal boundaries were basically redrawn in these regions. In the 19th and large parts of the 20th century, municipal mergers were forced by the central government. This policy changed in the end of the 20th century; local support for the merger is now a large part of the decision-making process. The larger, merged municipalities are intended to handle an increasing workload because more public services are delegated from higher levels of government to
3710-439: The municipalities. Another reason for municipal mergers is the assumption that larger municipalities are more efficient in performing their tasks than smaller ones. Municipalities have the right to decentralise themselves and form submunicipalities as an additional level of government. This right and the submunicipalities will cease to exist in the near future to reduce the number of levels of government. Only Amsterdam , where
3780-399: The ocean migrating inland, and salt-water intruding into freshwater aquifers. Where a large river spills out into the ocean, the velocity of the water suddenly slows and its ability to transport sand and silt decreases. Sediments begin to settle out, eventually forming a delta and extending to the coastline seaward. During subsequent flood events, water spilling out of the channel will find
3850-484: The overtopping water impinges the levee. By analyzing the results from EFA test, an erosion chart to categorize erodibility of the soils was developed. Hughes and Nadal in 2009 studied the effect of combination of wave overtopping and storm surge overflow on the erosion and scour generation in levees. The study included hydraulic parameters and flow characteristics such as flow thickness, wave intervals, surge level above levee crown in analyzing scour development. According to
3920-458: The purpose of impoldering, or as a boundary for an inundation area. The latter can be a controlled inundation by the military or a measure to prevent inundation of a larger area surrounded by levees. Levees have also been built as field boundaries and as military defences . More on this type of levee can be found in the article on dry-stone walls . Levees can be permanent earthworks or emergency constructions (often of sandbags ) built hastily in
3990-413: The river floodplains immediately adjacent to the cut banks. Like artificial levees, they act to reduce the likelihood of floodplain inundation. Deposition of levees is a natural consequence of the flooding of meandering rivers which carry high proportions of suspended sediment in the form of fine sands, silts, and muds. Because the carrying capacity of a river depends in part on its depth, the sediment in
4060-440: The river to form a wider channel, and flood valley basins are divided by multiple levees to prevent a single breach from flooding a large area. A levee made from stones laid in horizontal rows with a bed of thin turf between each of them is known as a spetchel . Artificial levees require substantial engineering. Their surface must be protected from erosion, so they are planted with vegetation such as Bermuda grass in order to bind
4130-538: The river. It is usually earthen and often runs parallel to the course of a river in its floodplain or along low-lying coastlines. Naturally occuring levees form on river floodplains following flooding, where sediment and alluvium is deposited and settles, forming a ridge and increasing the river channel's capacity. Alternatively, levees can be artificially constructed from fill , designed to regulate water levels. In some circumstances, artificial levees can be environmentally damaging . Ancient civilizations in
4200-575: The riverbed, even up to a point where the riverbed is higher than the adjacent ground surface behind the levees, are found for the Yellow River in China and the Mississippi in the United States. Levees are very common on the marshlands bordering the Bay of Fundy in New Brunswick and Nova Scotia , Canada . The Acadians who settled the area can be credited with the original construction of many of
4270-479: The same as regular municipalities and are grouped together as the Caribbean Netherlands and are not part of a province. The municipalities are governed by both a board of mayor and aldermen and a municipal council. The municipal council , which is titled island council in the special municipalities, is elected every four years. The number of members in the council ranges from nine members for
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#17327685185924340-414: The smallest municipalities to forty-five members for the largest. It is the highest administrative body in the municipality and controls public policy. The executive power lies with the executive board , which consists of a mayor , titled lieutenant governor in the special municipalities, and multiple aldermen, titled island deputies in the special municipalities. The mayor is appointed for six years at
4410-404: The soil to better resist instability. Artificial levees can lead to an elevation of the natural riverbed over time; whether this happens or not and how fast, depends on different factors, one of them being the amount and type of the bed load of a river. Alluvial rivers with intense accumulations of sediment tend to this behavior. Examples of rivers where artificial levees led to an elevation of
4480-401: The submunicipalities, no formal status. Levee A levee ( / ˈ l ɛ v i / or / ˈ l ɛ v eɪ / ), dike ( American English ), dyke ( British English ; see spelling differences ), embankment , floodbank , or stop bank is an elevated ridge , natural or artificial, alongside the banks of a river , often intended to protect against flooding of the area adjoining
4550-478: The uninhabited island of Noorderhaaks , which is part of the municipality, and southwest of the island of Vlieland . The island of Texel was originally made up of two islands, Texel proper to the south and Eierland to the northeast, which were connected by shoals . In the early seventeenth century, the islands were connected by a dyke to keep the North Sea from ravaging the coastal areas of Texel proper. In
4620-494: The water which is over the flooded banks of the channel is no longer capable of keeping the same number of fine sediments in suspension as the main thalweg . The extra fine sediments thus settle out quickly on the parts of the floodplain nearest to the channel. Over a significant number of floods, this will eventually result in the building up of ridges in these positions and reducing the likelihood of further floods and episodes of levee building. If aggradation continues to occur in
4690-642: Was built by the Qin as a water conservation and flood control project. The system's infrastructure is located on the Min River , which is the longest tributary of the Yangtze River , in Sichuan , China . The Mississippi levee system represents one of the largest such systems found anywhere in the world. It comprises over 5,600 km (3,500 mi) of levees extending some 1,000 km (620 mi) along
4760-488: Was constructed during the early 1400s, under the supervision of the tlahtoani of the altepetl Texcoco, Nezahualcoyotl. Its function was to separate the brackish waters of Lake Texcoco (ideal for the agricultural technique Chināmitls ) from the fresh potable water supplied to the settlements. However, after the Europeans destroyed Tenochtitlan, the levee was also destroyed and flooding became a major problem, which resulted in
4830-721: Was held prisoner on Texel by her uncle, William I, Count of Holland . Texel received city rights in 1415. The first Dutch expedition to the Northwest Passage departed from the island on the 5th of June, 1594. Texel was involved in the Battle of Scheveningen (1653) during the First Anglo-Dutch War and the Battle of Texel (1673) during the Third Anglo-Dutch War . During the American Revolutionary War , Texel
4900-687: Was used as a port by Continental Navy officer John Paul Jones after the battle of Flamborough Head off the Yorkshire coast in September 1779. In the battle, Jones captured the Royal Navy frigate Serapis , which he sailed to Texel for desperately needed repairs. This event further complicated Anglo-Dutch relations. In 1797, Texel was involved in the Battle of Camperdown during the French Revolutionary Wars . During
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