Dyke (construction)
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Dyke (construction)
A levee (), dike (American English), dyke (Commonwealth English), embankment, floodbank, or stop bank is a structure that is usually earthen and that often runs parallel to the course of a river in its floodplain or along low-lying coastlines. The purpose of a levee is to keep the course of rivers from changing and to protect against flooding of the area adjoining the river or coast. Levees can be naturally occurring ridge structures that form next to the bank of a river, or be an artificially constructed fill or wall that regulates water levels. Ancient civilizations in 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. Etymology Speakers of American English (notably in the Midwest and Deep South) use the word ''levee'', from the French word (from the feminine past participle of the French verb , 'to raise'). It originated i ...
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River Levee Cross Section Figure
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 creek, brook, rivulet, and rill. There are no official definitions for the generic term river as applied to 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" 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 through a drainage basin from surface runoff and other sources such as groundwater recharge, springs, a ...
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Batavi (Germanic Tribe)
The Batavi were an ancient Germanic tribe that lived around the modern Dutch Rhine delta in the area that the Romans called Batavia, from the second half of the first century BC to the third century AD. The name is also applied to several military units employed by the Romans that were originally raised among the Batavi. The tribal name, probably a derivation from ''batawjō'' ("good island", from Germanic ''bat-'' "good, excellent," which is also in the English "better," and ''awjō'' "island, land near water"), refers to the region's fertility, today known as the ''fruitbasket of the Netherlands'' (the Betuwe). Finds of wooden tablets show that at least some were literate . Location The Batavi themselves are not mentioned by Julius Caesar in his commentary ''Commentarii de Bello Gallico'', although he is often thought to have founded his dynasty's Germanic bodyguard, which was at least in later generations dominated by Batavi. But he did mention the "Batavian island" in the ...
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Twenty, Lincolnshire
Twenty is a hamlet in the South Kesteven district of Lincolnshire, England. It is situated approximately east from the market town of Bourne, and west from Spalding. Agriculture is the major industry. Location Twenty is situated on the A151 road, possibly originally a Roman road or Norman causeway, a road today notable for the very deep drainage dyke that runs alongside it. Nearby are Guthram Gowt and West Pinchbeck. Immediately to the south is the River Glen. No separate population statistic is available for Twenty. The best available report lumps together Dyke, Twenty, South Fen and Spalding Road outside Bourne, with a total of 495, with Dyke being the largest. Modern drainage The area falls within the drainage area of the Black Sluice Internal Drainage Board. They maintain a small electric pumping station to the west of the crossroads, called ''Twenty Pumping Station'' See also * List of places with numeric names This is a list of places with numeric names. 0 ...
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Bourne, Lincolnshire
Bourne is a market town and civil parish in the South Kesteven district of Lincolnshire, England. It lies on the eastern slopes of the limestone Kesteven Uplands and the western edge of the Fens, 11 miles (18 km) north-east of Stamford, 12 miles (19 km) west of Spalding and 17 miles (27 km) north of Peterborough. The population at the 2011 census was 14,456. A 2019 estimate put it at 16,780. History The Ancient Woodland of Bourne Woods is still extant, although much reduced. It originally formed part of the ancient Forest of Kesteven and is now managed by the Forestry Commission. The earliest documentary reference to ''Brunna'', meaning stream, is from a document of 960, and the town appeared in Domesday Book of 1086 as ''Brune''. Bourne Abbey, (charter 1138), formerly held and maintained land in Bourne and other parishes. In later times this was known as the manor of Bourne Abbots. Whether the canons knew that name is less clear. The estate was given by the founder of the ...
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Soak Dike
Soak may refer to: * Steeping * Bathing * Soakage (source of water), a source of water in Australian deserts * Soak dike, ditch or drain * Soak testing, a method of system testing in computing and electronics * Soak (singer), Irish singer-songwriter * ''Soak'' (album), 2013 album by Foetus * SOAK, a Burning Man regional event in Portland, Oregon, USA See also * Soak City (other) * Soaked (other) * Soaking (other) * Soke (other) Soke may refer to: * Soke (legal), an early Western jurisdictional concept * Soke (dance) or ''eke'', a Tongan stick dance, originating from Wallis and Futuna * , a Japanese title meaning "head of the family," and is usually used to denote the hea ... * Souq, a marketplace consisting of multiple small stalls or shops {{Disambiguation ...
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Lincolnshire
Lincolnshire (abbreviated Lincs.) is a county in the East Midlands of England, with a long coastline on the North Sea to the east. It borders Norfolk to the south-east, Cambridgeshire to the south, Rutland to the south-west, Leicestershire and Nottinghamshire to the west, South Yorkshire to the north-west, and the East Riding of Yorkshire to the north. It also borders Northamptonshire in the south for just , England's shortest county boundary. The county town is Lincoln, where the county council is also based. The ceremonial county of Lincolnshire consists of the non-metropolitan county of Lincolnshire and the area covered by the unitary authorities of North Lincolnshire and North East Lincolnshire. Part of the ceremonial county is in the Yorkshire and the Humber region of England, and most is in the East Midlands region. The county is the second-largest of the English ceremonial counties and one that is predominantly agricultural in land use. The county is fourth-larg ...
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Catchwater Drain
A catchwater drain is a land drain, a ditch cut across the fall of the land, typically just above the level of low-lying, level ground such as The Fens of eastern England, where some land, tens of kilometres from the sea is at about sea level. Its purpose is to gather water draining from the higher, sloping ground before it reaches the flat land whence it would be difficult or expensive to remove. The water may be on the surface, in streams or in the ground before it is gathered, perhaps to be led away across the lowland by an embanked river. There are other circumstances in which a catchwater may be employed. A hill-top or hillside may be used to trap rainwater which is then gathered by the catchwater and fed to a reservoir. From this a house, village or town may be supplied. Catchwater may be used to slow down runoff before running on impervious surfaces to reduce runoff. See also *Nullah A nullah or nala ( Hindustani or "nallah" in Punjabi) is an 'arm of the sea', st ...
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Ditch
A ditch is a small to moderate divot created to channel water. A ditch can be used for drainage, to drain water from low-lying areas, alongside roadways or fields, or to channel water from a more distant source for plant irrigation. Ditches are commonly seen around farmland, especially in areas that have required drainage, such as The Fens in eastern England and much of the Netherlands. Roadside ditches may provide a hazard to motorists and cyclists, whose vehicles may crash into them and get damaged, flipped over, or stuck and cause major injury, especially in poor weather conditions and rural areas. Etymology In Anglo-Saxon, the word ''dïc'' already existed and was pronounced "deek" in northern England and "deetch" in the south. The 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 ''dïc'' was given to either the excavation or the bank, and evolved to both the words "dike"/"dyke" and ...
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East Anglia
East Anglia is an area in the East of England, often defined as including the counties of Norfolk, Suffolk and Cambridgeshire. The name derives from the Anglo-Saxon kingdom of the East Angles, a people whose name originated in Anglia, in what is now Northern Germany. Area Definitions of what constitutes East Anglia vary. The Anglo-Saxon Kingdom of East Anglia, established in the 6th century, originally consisted of the modern counties of Norfolk and Suffolk and expanded west into at least part of Cambridgeshire, typically the northernmost parts known as The Fens. The modern NUTS 3 statistical unit of East Anglia comprises Norfolk, Suffolk and Cambridgeshire (including the City of Peterborough unitary authority). Those three counties have formed the Roman Catholic Diocese of East Anglia since 1976, and were the subject of a possible government devolution package in 2016. Essex has sometimes been included in definitions of East Anglia, including by the London Society o ...
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Midlands
The Midlands (also referred to as Central England) are a part of England that broadly correspond to the Kingdom of Mercia of the Early Middle Ages, bordered by Wales, Northern England and Southern England. The Midlands were important in the Industrial Revolution of the 18th and 19th centuries. They are split into the West Midlands and East Midlands. The region's biggest city, Birmingham often considered the social, cultural, financial and commercial centre of the Midlands, is the second-largest city and metropolitan area in the United Kingdom. Symbolism A saltire (diagonal cross) may have been used as a symbol of Mercia as early as the reign of Offa. By the 13th century, the saltire had become the attributed arms of the Kingdom of Mercia. The arms are blazoned ''Azure, a saltire Or'', meaning a gold (or yellow) saltire on a blue field. The saltire is used as both a flag and a coat of arms. As a flag, it is flown from Tamworth Castle, the ancient seat of the Mercian Kings, to t ...
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Car Dyke
The Car Dyke was, and to a large extent still is, an long ditch which runs along the western edge of the Fens in eastern England. It is generally accepted as being of Roman invasion of Britain, Roman age and, for many centuries, to have been taken as marking the western edge of the Fens. There, the consensus begins to break down. Likely purpose In the eighteenth century, William Stukeley described it as a canal used for transporting goods and his idea is still promulgated: For example, excavations at Waterbeach in the 1990s by the archaeology unit of Cambridgeshire, Cambridgeshire County Council found what were seen as the remains of a Roman Britain, Roman-era boat and cargo of pottery from Horningsea. This stretch has been protected as a scheduled monument. Other archaeological investigations near Boston, Lincolnshire, Boston have given an indication of the dimensions: a navigable width of and a depth of were found during excavation. Other excavations have found coal from th ...
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Offa's Dyke
Offa's Dyke ( cy, Clawdd Offa) is a large linear earthwork that roughly follows the border between England and Wales. The structure is named after Offa, the Anglo-Saxon king of Mercia from AD 757 until 796, who is traditionally believed to have ordered its construction. Although its precise original purpose is debated, it delineated the border between Anglian Mercia and the Welsh kingdom of Powys. The earthwork, which was up to wide (including its flanking ditch) and high, traversed low ground, hills and rivers. Today it is protected as a scheduled monument. Some of its route is followed by the Offa's Dyke Path, a long-distance footpath that runs between Liverpool Bay in the north and the Severn Estuary in the south. Although the Dyke has conventionally been dated to the Early Middle Ages of Anglo-Saxon England, research in recent decades – using techniques such as radioactive carbon dating – has challenged the conventional historiography and theories about the earth ...
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