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River Adur
The Adur ( or ) is a river in Sussex, England; it gives its name to the Adur district of West Sussex. The river, which is long, was once navigable for large vessels up as far as Steyning, where there was a large Saxon port, but by the 11th century the lower river became silted up and the port moved down to the deeper waters at the mouth of the river in Shoreham-by-Sea. Watercourse The Adur begins as two separate branches, the western Adur and the eastern Adur, which meet west of Henfield. The western Adur rises at Slinfold from where it flows around Coolham and then through Shipley, where it meets Lancing Brook and flows on to West Grinstead and Knepp Castle. The western Adur is tidal as far north as Bines Bridge near Bines Green, south of West Grinstead. The eastern Adur rises at Ditchling Common, in East Sussex, from where it crosses into West Sussex and meets Herrings Stream at Twineham (). At Shermanbury, the eastern Adur is fed by the Cowfold Stream. The Normal Ti ...
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England
England is a country that is part of the United Kingdom. It shares land borders with Wales to its west and Scotland to its north. The Irish Sea lies northwest and the Celtic Sea to the southwest. It is separated from continental Europe by the North Sea to the east and the English Channel to the south. The country covers five-eighths of the island of Great Britain, which lies in the North Atlantic, and includes over 100 smaller islands, such as the Isles of Scilly and the Isle of Wight. The area now called England was first inhabited by modern humans during the Upper Paleolithic period, but takes its name from the Angles, a Germanic tribe deriving its name from the Anglia peninsula, who settled during the 5th and 6th centuries. England became a unified state in the 10th century and has had a significant cultural and legal impact on the wider world since the Age of Discovery, which began during the 15th century. The English language, the Anglican Church, and Engli ...
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East Sussex
East Sussex is a ceremonial and non-metropolitan county in South East England on the English Channel coast. It is bordered by Kent to the north and east, West Sussex to the west, and Surrey to the north-west. The largest settlement in East Sussex is the city of Brighton and Hove. History East Sussex is part of the historic county of Sussex, which has its roots in the ancient kingdom of the South Saxons, who established themselves there in the 5th century AD, after the departure of the Romans. Archaeological remains are plentiful, especially in the upland areas. The area's position on the coast has also meant that there were many invaders, including the Romans and later the Normans. Earlier industries have included fishing, iron-making, and the wool trade, all of which have declined, or been lost completely. Governance Sussex was historically sub-divided into six rapes. From the 12th century the three eastern rapes together and the three western rapes together had separ ...
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Baybridge Canal
The Baybridge Canal was a short canal built entirely within the parish of West Grinstead in the English county of Sussex. It opened in 1826, and closed in 1875. History The River Adur is formed when the Western Adur and the Eastern Adur join near Henfield. The Western branch starts near Slinfold, and flows through Shipley and West Grinstead. The Eastern branch rises on Ditchling Common, and flows through Haywards Heath and Burgess Hill. Below the junction, the combined stream flows for to reach the English Channel at the port of Shoreham-by-Sea. Under an act of Parliament obtained in 1807, the river was improved, to aid both navigation and drainage, and barges could reach Bines Bridge on the Western Adur. In 1824, the civil engineer May Upton produced a plan for extending the navigation northwards to West Grinstead, at a cost of just under £6,000. This formed the basis for another act of Parliament, which was obtained in 1825, and created the Baybridge Canal Company. Seven me ...
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Southwick Ship Canal
The Southwick Ship Canal or Southwick Canal is a canal in Southwick, West Sussex that branches off from the estuary of the River Adur near Hove. The canal is 1.75 miles in length, running east–west and parallel with the shoreline, providing facilities to the port of Shoreham. The canal was once the river channel, but the mouth of the river has been moved further to the west, enabling its former bed to be used for the canal. History Shoreham, Southwick, and Portslade are located side by side on the West Sussex coast. The River Adur flows from the north, and turns to the east near Shoreham, to reach the English Channel. The area has a long history as a centre for shipping. In Roman times, there were ports at Old Shoreham and Beeding on the lower reaches of the River Adur, and a road from London to the port passed through Portus Ladus ("the way to the port"), eventually giving rise to the name Portslade. It was thought that the Roman fort Portus Adurni was located near the mouth ...
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Portslade
Portslade is a western suburb of the city of Brighton and Hove, England. Portslade Village, the original settlement a mile inland to the north, was built up in the 16th century. The arrival of the railway from Brighton in 1840 encouraged rapid development of the coastal area and in 1896 the southern part, formerly known as Copperas Gap, was granted urban district status and renamed Portslade-by-Sea, making it distinct from Portslade Village. After World War II the district of Mile Oak to the north was added. Today, Portslade is bisected from east to west by the old A27 road (now the A270) between Brighton and Worthing, each part having a distinct character. Notable buildings and areas Portslade Village, to the north, nestles in a valley of the South Downs and still retains its rural character with flint buildings, a village green and the small parish church of St Nicolas, which is the second-oldest church in the city, dating from approximately 1150. Another notable building ...
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Longshore Drift
Longshore drift from longshore current is a geological process that consists of the transportation of sediments (clay, silt, pebbles, sand, shingle) along a coast parallel to the shoreline, which is dependent on the angle incoming wave direction. Oblique incoming wind squeezes water along the coast, and so generates a water current which moves parallel to the coast. Longshore drift is simply the sediment moved by the longshore current. This current and sediment movement occur within the surf zone. The process is also known as littoral drift. Beach sand is also moved on such oblique wind days, due to the swash and backwash of water on the beach. Breaking surf sends water up the beach (swash) at an oblique angle and gravity then drains the water straight downslope (backwash) perpendicular to the shoreline. Thus beach sand can move downbeach in a sawtooth fashion many tens of meters (yards) per day. This process is called "beach drift" but some workers regard it as simply part o ...
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Lancing College
Lancing College is a public school (English independent day and boarding school for pupils aged 13–18) in southern England, UK. The school is located in West Sussex, east of Worthing near the village of Lancing, on the south coast of England. Lancing was founded in 1848 by Nathaniel Woodard and educates c. 600 pupils between the ages of 13 and 18; the co-educational ratio is c. 60:40 boys to girls. Girls were admitted beginning in 1971. The first co-ed, Saints’ House, was established in September 2018, bringing the total number of Houses to 10. There are 5 male houses (Gibbs, School, Teme, Heads, Seconds) and 4 female houses (Fields, Sankeys, Manor, Handford). The college is situated on a hill which is part of the South Downs, and the campus dominates the local landscape. The college overlooks the River Adur, and the Ladywell Stream, a holy well or sacred stream within the College grounds, has pre-Christian significance. Woodard's aim was to provide education "based on soun ...
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South Downs
The South Downs are a range of chalk hills that extends for about across the south-eastern coastal counties of England from the Itchen valley of Hampshire in the west to Beachy Head, in the Eastbourne Downland Estate, East Sussex, in the east. The Downs are bounded on the northern side by a steep escarpment, from whose crest there are extensive views northwards across the Weald. The South Downs National Park forms a much larger area than the chalk range of the South Downs and includes large parts of the Weald. The South Downs are characterised by rolling chalk downland with close-cropped turf and dry valleys, and are recognised as one of the most important chalk landscapes in England. The range is one of the four main areas of chalk downland in southern England. The South Downs are relatively less populated compared to South East England as a whole, although there has been large-scale urban encroachment onto the chalk downland by major seaside resorts, including most notably ...
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Coombes
Coombes is a hamlet and civil parish in the Adur District of West Sussex, England. The village is in the Adur Valley northwest of Shoreham-by-Sea. Coombes Church is an 11th-century Church of England parish church that has lost its dedication. It has some of the most important medieval wall paintings in England, which were painted . There is a single church bell that weighs about and was probably cast in Normandy. It is one of the oldest bells in Sussex, dated to . The church is roofed with Horsham Stone slabs. The civil parish has an area of and has a parish meeting rather than a parish council. The 2001 Census recorded a population of 51 people living in 22 households of whom 23 were economically active. Church Farm is next to the parish church and Applesham Farm is about to the south. See also * Coombs (other) * Coombe (other) References Further reading * * External links Adur District Council
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Bramber
Bramber is a former manor, village and civil parish in the Horsham District of West Sussex, England. It has a ruined mediaeval castle which was the ''caput'' of a large feudal barony. Bramber is located on the northern edge of the South Downs and on the west side of the River Adur. Nearby are the communities of Steyning to the west and Upper Beeding to the east, and the other side of the river. The closest historical connection, however, is with the village of Botolphs to the south. The ecclesiastical parishes of Bramber and Botolphs were united possibly as early as 1526, but certainly by 1534British History Onlinentry here with the priest living at Botolphs. Later the priest's official residence became the imposing Bramber mansion and landmark now called "Burletts" and located on Clays Hill. The union of the civil parish councils followed 400 years later in 1933. Castle Bramber was the ''caput'' of a large feudal barony A feudal baron is a vassal holding a heritable fief ...
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Upper Beeding
Upper Beeding is a village and civil parish in the Horsham District of West Sussex, England. It is located at the northern end of the River Adur gap in the South Downs, four miles (6.4 km) north of Shoreham-by-Sea and has a land area of 1877 hectares (4637 acres). The site is a bridging point over the river: on the opposite bank are Bramber and Steyning, making the whole area somewhat built-up. The civil parish also includes the smaller village of Small Dole to the north (nearer to Henfield), and the village of Edburton to the northeast. Upper Beeding is on the northern edge of the South Downs National Park which was created in 2010. The South Downs Way and Monarch's Way long-distance footpaths run through the parish; the area is popular with walkers, cyclists and equestrians. It is also at the western end of the Beeding Hill to Newtimber Hill Site of Special Scientific Interest. History The community was originally (and for the majority of its history) c ...
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Confluence
In geography, a confluence (also: ''conflux'') occurs where two or more flowing bodies of water join to form a single channel. A confluence can occur in several configurations: at the point where a tributary joins a larger river (main stem); or where two streams meet to become the source of a river of a new name (such as the confluence of the Monongahela and Allegheny rivers at Pittsburgh, forming the Ohio); or where two separated channels of a river (forming a river island) rejoin at the downstream end. Scientific study of confluences Confluences are studied in a variety of sciences. Hydrology studies the characteristic flow patterns of confluences and how they give rise to patterns of erosion, bars, and scour pools. The water flows and their consequences are often studied with mathematical models. Confluences are relevant to the distribution of living organisms (i.e., ecology) as well; "the general pattern ownstream of confluencesof increasing stream flow and decreasing s ...
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