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Lee-over-Sands
Lee-over-Sands is a small coastal hamlet in the civil parish of St Osyth, in the Tendring District, Tendring district of Essex, England. It is located close to the mouth of the River Colne, Essex, River Colne into the North Sea. A Spit (landform), sandspit called Colne Point is offshore from the hamlet. Colne Point Nature Reserve, a shingle ridge enclosing a saltmarsh, is to the west of the hamlet on the site of a World War I gravel works. Jaywick Martello Tower is east of Lee-over-Sands. The area is subject to flooding, and was severely affected by the North Sea flood of 1953, when the seawall was breached in many locations near the village. Thirty-seven people died in nearby Jaywick, east of Lee-over-Sands. In January 2017 following a threat of coastal flooding, an evacuation of 2,500 homes in Lee-over-Sands and nearby Jaywick was planned, but in the event not required. A number of houses are on the seaward side of the seawall, on Beach Road. One house on Beach Road won the ...
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St Osyth
St Osyth is an English village and civil parishes in England, civil parish in the Tendring District of north-east Essex, about west of Clacton-on-Sea and southeast of Colchester. It lies on the B1027, Colchester–Clacton road. The village is named after Osgyth, a seventh-century saint and princess. Locally, the name is sometimes pronounced "Toosey". It is claimed to be the driest recorded place in the United Kingdom. In 2011 it had a population of 4,277. History Before being renamed after the Abbey of St Osgyth built there in the 12th century, the village was called ''Chich'' (also spelt ''Chiche'' or ''Chick''), from an Old English word ''cic'' meaning "bend", a reference to St Osyth Creek. Under Canute, King Canute/Cnut (reigned 1018–1035), Chich was assumed as part of the royal demesne and granted to Godwin, Earl of Wessex, Earl Godwin. By him it was given to Canterbury Cathedral, Christ Church, Canterbury. After the Norman Conquest in 1066 it was transferred to the Bish ...
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Jaywick
Jaywick is a coastal village in the Tendring District, Tendring district of Essex, England, west of Clacton-on-Sea. It lies on the North Sea coast of England, from London and from Colchester. It was constructed in the 1930s as a Seaside resort, holiday resort for Londoners but has, over time, been officially named the most deprived area in the country. The land on which the village is built was originally fields and salt marsh unsuitable for agriculture. It was purchased by the entrepreneur Frank Stedman in 1928 to build low cost, affordable holiday homes for working-class families, and became a popular holiday destination throughout the 1930s. After the Second World War, a shortage of housing meant the properties became permanently inhabited despite not being built for this purpose. Many holiday homes are now in a state of disrepair, and the local community have resisted demolition. Jaywick has significant problems with unemployment and is at risk of flooding, despite sever ...
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Jaywick Martello Tower
Jaywick Martello Tower is a renovated Martello tower at Jaywick, south-west of Clacton-on-Sea, Essex. It now functions as an arts, heritage and community venue. It is a Grade II listed building and a scheduled monument. History The tower was one of several Martello towers on the east coast of England. They were constructed to defend the country against invasion by Napoleon Bonaparte and his armies. In total, 103 Martello towers were built between 1804 and 1812, 74 were built between 1804 and 1808 along the Kent and Sussex coast from Folkestone to Seaford, and 29 along the east coast between Point Clear near St Osyth and Aldeburgh from 1809 to 1812. The south coast towers were numbered 1 – 74 and the east coast towers were lettered A – Z. Three other east coast towers are known as AA, BB and CC. The tower at Jaywick is Tower D. The tower was constructed from around 750,000 London Clay bricks manufactured at Grays and transported by barge. The brick walls are thick and aro ...
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Hamlets In Essex
A hamlet is a human settlement that is smaller than a town or village. This is often simply an informal description of a smaller settlement or possibly a subdivision or satellite entity to a larger settlement. Sometimes a hamlet is defined for official or administrative purposes. The word and concept of a hamlet can be traced back to Norman England, where the Old French came to apply to small human settlements. Etymology The word comes from Anglo-Norman ', corresponding to Old French ', the diminutive of Old French ' meaning a little village. This, in turn, is a diminutive of Old French ', possibly borrowed from (West Germanic languages">West Germanic) Franconian languages. It is related to the modern French ', Dutch language, Dutch ', Frisian languages, Frisian ', German ', Old English ', and Modern English ''home''. By country Afghanistan In Afghanistan, the counterpart of the hamlet is the qala (Dari: قلعه, Pashto: کلي) meaning "fort" or "hamlet". The A ...
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Royal Institute Of British Architects
The Royal Institute of British Architects (RIBA) is a professional body for architects primarily in the United Kingdom, but also internationally, founded for the advancement of architecture under its royal charter granted in 1837, three supplemental charters and a new charter granted in 1971. Founded as the Institute of British Architects in London in 1834, the RIBA retains a central London headquarters at 66 Portland Place as well as a network of regional offices. Its members played a leading part in promotion of architectural education in the United Kingdom; the RIBA Library, also established in 1834, is one of the three largest architectural libraries in the world and the largest in Europe. The RIBA also played a prominent role in the development of UK architects' registration bodies. The institute administers some of the oldest architectural awards in the world, including RIBA President's Medals Students Award, the Royal Gold Medal, and the Stirling Prize. It also man ...
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Seawall
A seawall (or sea wall) is a form of coastal defense constructed where the sea, and associated coastal processes, impact directly upon the landforms of the coast. The purpose of a seawall is to protect areas of human habitation, conservation, and leisure activities from the action of tides, waves, or tsunamis. As a seawall is a static feature, it will conflict with the dynamic nature of the coast and impede the exchange of sediment between land and sea. Seawall designs factor in local climate, coastal position, wave regime (determined by wave characteristics and effectors), and value (morphological characteristics) of landform. Seawalls are hard engineering shore-based structures that protect the coast from erosion. Various environmental issues may arise from the construction of a seawall, including the disruption of sediment movement and transport patterns. Combined with a high construction cost, this has led to increasing use of other soft engineering coastal management ...
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Coastal Flooding
Coastal flooding occurs when dry and low-lying land is submerged (flooded) by seawater. The range of a coastal Flood, flooding is a result of the elevation of floodwater that penetrates the inland which is controlled by the topography of the coastal land exposed to flooding. The seawater can flood the land via several different paths: direct flooding, overtopping or breaching of a barrier. Coastal flooding is largely a natural event. Due to the effects of climate change (e.g. sea level rise and an increase in extreme weather events) and an increase in the population living in coastal areas, the damage caused by coastal flood events has intensified and more people are being affected. Coastal plain, Coastal areas are sometimes flooded by unusually high tides, such as spring tides, especially when compounded by high winds and storm surges. This was the cause of the North Sea flood of 1953 which flooded large swathes of the Netherlands and the East coast of England. When humans modif ...
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North Sea Flood Of 1953
The 1953 North Sea flood () was a major flood caused by a heavy storm surge that struck the Netherlands, north-west Belgium, England and Scotland. Most sea defences facing the surge were overwhelmed, resulting in extensive flooding. The storm and flooding occurred during the night of Saturday, 31 January to the morning of 1 February 1953. A combination of a high spring tide and a severe European windstorm caused a storm tide of the North Sea. The combination of wind, high tide, and low pressure caused the sea to flood land up to above mean sea level. Realising that such infrequent events could reoccur, the Netherlands and the United Kingdom carried out large studies on strengthening of coastal defences. The Netherlands developed the Delta Works, an extensive system of dams and storm surge barriers. The UK constructed storm surge barriers on the Thames Estuary and on the Hull where it meets the Humber Estuary. Flooding summary At the time of the flood, 20% of the lan ...
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World War I
World War I or the First World War (28 July 1914 – 11 November 1918), also known as the Great War, was a World war, global conflict between two coalitions: the Allies of World War I, Allies (or Entente) and the Central Powers. Fighting took place mainly in European theatre of World War I, Europe and the Middle Eastern theatre of World War I, Middle East, as well as in parts of African theatre of World War I, Africa and the Asian and Pacific theatre of World War I, Asia-Pacific, and in Europe was characterised by trench warfare; the widespread use of Artillery of World War I, artillery, machine guns, and Chemical weapons in World War I, chemical weapons (gas); and the introductions of Tanks in World War I, tanks and Aviation in World War I, aircraft. World War I was one of the List of wars by death toll, deadliest conflicts in history, resulting in an estimated World War I casualties, 10 million military dead and more than 20 million wounded, plus some 10 million civilian de ...
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Tendring District
Tendring District is a Non-metropolitan district, local government district in north-east Essex, England. Its council is based in Clacton-on-Sea, the largest town. Other towns are Brightlingsea, Harwich, Frinton-on-Sea and Walton-on-the-Naze. The district borders the City of Colchester to the west and the Babergh District of Suffolk, across the estuary of the River Stour, Suffolk, River Stour, to the north. To the east and south, it faces the North Sea, with the estuary of the River Colne, Essex, River Colne to the south-west. The area is sometimes referred to as the ''Tendring Peninsula''. The modern local government district was formed in 1974. The name ''Tendring'' comes from the ancient Tendring Hundred (division), Hundred which was named after the small village of Tendring. History The district was formed on 1 April 1974 under the Local Government Act 1972, covering the whole area of five former districts, which were all abolished at the same time: *Brightlingsea Urban di ...
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Saltmarsh
A salt marsh, saltmarsh or salting, also known as a coastal salt marsh or a tidal marsh, is a coastal ecosystem in the upper coastal intertidal zone between land and open saltwater or brackish water that is regularly flooded by the tides. It is dominated by dense stands of salt-tolerant plants such as herbs, grasses, or low shrubs. These plants are terrestrial in origin and are essential to the stability of the salt marsh in trapping and binding sediments. Salt marshes play a large role in the aquatic food web and the delivery of nutrients to coastal waters. They also support terrestrial animals and provide coastal protection. Salt marshes have historically been endangered by poorly implemented coastal management practices, with land reclaimed for human uses or polluted by upstream agriculture or other industrial coastal uses. Additionally, sea level rise caused by climate change is endangering other marshes, through erosion and submersion of otherwise tidal marshes. Howeve ...
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Spit (landform)
A spit (cognate with the word for a rotisserie bar) or sandspit is a deposition (geology), deposition shoal, bar or beach landform off coasts or lake shores. It develops in places where re-entrance occurs, such as at a cove's headlands, by the process of longshore drift by longshore currents. The drift occurs due to waves meeting the beach at an oblique angle, moving sediment down the beach in a zigzag pattern. This is complemented by longshore currents, which further sediment transport, transport sediment through the water alongside the beach. These currents are caused by the same waves that cause the drift. Hydrology and geology Where the direction of the shore inland ''re-enters'', or changes direction, for example at a headland, the longshore current spreads out or dissipates. No longer able to carry the full load, much of the sediment is dropped. This is called deposition. This submerged bar of sediment allows longshore drift or littoral drift to continue to transport sed ...
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