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130-757: The River Hull is a navigable river in the East Riding of Yorkshire in Northern England . It rises from a series of springs to the west of Driffield , and enters the Humber Estuary at Kingston upon Hull . Following a period when the Archbishops of York charged tolls for its use, it became a free navigation. The upper reaches became part of the Driffield Navigation from 1770, after which they were again subject to tolls, and

260-684: A barrage at the mouth of the Hull where it joins the Humber Estuary to maintain a constant water level as it passes through the city. The idea was first raised by the Abercrombie report , which considered how to redevelop Hull after significant destruction during the Second World War . The estimated cost of such a project was around £195 million in 2007. Because the river was a free river, there are no figures for traffic on

390-475: A tidal barrier at the mouth of the river. The structure spans the river, and a huge steel gate, weighing 202 tonnes, can be lowered into the waterway, effectively sealing the river from the Humber, and preventing tidal surges from moving up the river and flooding parts of the city and the low-lying areas beyond. The gate was initially lowered about twelve times a year, and protects around 17,000 properties. In 2009,

520-602: A tripoint . Various examples are found in the list below. A number of major cities, such as Chongqing , St. Louis , and Khartoum , arose at confluences; further examples appear in the list. Within a city, a confluence often forms a visually prominent point, so that confluences are sometimes chosen as the site of prominent public buildings or monuments, as in Koblenz , Lyon , and Winnipeg . Cities also often build parks at confluences, sometimes as projects of municipal improvement, as at Portland and Pittsburgh . In other cases,

650-669: A 6.6-foot (2.0 m) hole appeared in the river bed, and the entire site flooded. A 3-month investigation took place, which suggested that it would be difficult to finish the tunnel and maintain the integrity of the aquifer. Despite some £10 million having been spent on the project, it was abandoned in 1993. A contract for a replacement bridge was awarded in June 1995 and the river was crossed by twin lift bridges, which were opened in April 1997. The project had cost £30 million, compared to an original budget of just £13 million. A tunnel

780-471: A boat needed to pass, the west end was freed, and the pontoon swung round to lie parallel to the bank, either upstream or downstream, depending on the state of the tide. It would then be winched back into position by a small barrel winch. At night the bridge was closed and moored beside the bank. Responsibility for the bridge was taken over by Beverley Council before the Second World War . Its condition deteriorated, and in 1948, they attempted to replace it with

910-672: A charity, provides a community transport service for North Holderness, taking people to medical appointments in Hull and to the shops. The Humber Bridge , a road-only bridge, part of the A15 , links Hessle , west of Hull, with Barton-upon-Humber in Lincolnshire. West of this, the next crossing of the river (the Ouse at this point) are three bridges near Goole : a railway bridge, the M62 bridge and

1040-554: A city of its size, with the census reporting 97.7% white. Areas of the East Riding show significant signs of affluence, including the Parliamentary constituency of Haltemprice and Howden which consists of middle-class areas such as: the suburb of Willerby , suburb of Kirk Ella , village of North Ferriby , and village of Swanland . Much of the area is affluent and has one of the highest proportions of owner-occupiers in

1170-668: A clause inserted into the Act of Parliament which the Hull Dock Company obtained in 1840, to ensure free passage for vessels, and the removal of tolls for boats not using the docks. The Navigation Company also received complaints from the Beverley and Barmston Drainage Commissioners, who believed that water levels were being kept at a higher level than was good for drainage. In 1980, the Environment Agency constructed

1300-414: A confluence can be divided into six distinct features which are commonly called confluence flow zones (CFZ). These include The broader field of engineering encompasses a vast assortment of subjects which concern confluences. In hydraulic civil engineering , where two or more underground culverted / artificially buried watercourses intersect, great attention should be paid to the hydrodynamic aspects of

1430-630: A confluence is an industrial site, as in Philadelphia or Mannheim . Often a confluence lies in the shared floodplain of the two rivers and nothing is built on it, for example at Manaus , described below. One other way that confluences may be exploited by humans is as sacred places in religions . Rogers suggests that for the ancient peoples of the Iron Age in northwest Europe, watery locations were often sacred, especially sources and confluences. Pre-Christian Slavic peoples chose confluences as

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1560-482: A corresponding shift in habitat characteristics." Another science relevant to the study of confluences is chemistry , because sometimes the mixing of the waters of two streams triggers a chemical reaction, particularly in a polluted stream. The United States Geological Survey gives an example: "chemical changes occur when a stream contaminated with acid mine drainage combines with a stream with near-neutral pH water; these reactions happen very rapidly and influence

1690-450: A density of 1.4 people per hectare. The most populous parishes in the main 2001 census were Bridlington (34,000), Goole (17,000), Beverley (17,000), Cottingham (17,000, by Hull), Hessle (15,000, by Hull), Driffield (11,000), Anlaby with Anlaby Common (10,000, by Hull), Hornsea (8,000) and Willerby (8,000), Pocklington (8,000) and Elloughton-cum-Brough (7,000). Half the district's population reside in these 11 parishes, with

1820-576: A fall in sea level. The lower-lying land was used for stock breeding . During the last years of Roman Britain, Anglo-Saxon raiders were troubling the area. After the Romans, the Brythonic -speaking area became known as Deira . By the second half of the 5th century, the continued settlement by the Angles caused a shift to Old English . Deira merged into Northumbria and village names containing

1950-404: A ferry at Grovehill, and a shipyard on the east bank, owned by Joseph Scarr. To assist his workers to reach the shipyard, Scarr designed and built a ferry bridge, which cost him £300. It consisted of a large rectangular pontoon, above which was fitted a bridge deck with handrails. Two jack screws enabled the deck to be raised or lowered in relation to the pontoon, so that it remained at approximately

2080-566: A footbridge around 400 yards (370 m) further upstream. Because the ferry rights had been in existence for more than 600 years, an Act of Parliament was needed, and this was thwarted by a petition containing 84 signatures, presented by the people of Weel to the House of Lords . Plans for a new lift bridge were drawn up, and it was opened on 19 October 1953. In 1913, the Hull Bridge upstream of Beverley, which had caused so much disagreement in

2210-699: A four-star rating, which places the authority as one of the best in the country. For representation in the Parliament of the United Kingdom the bulk of the East Riding district is divided into three county constituencies : Beverley and Holderness , Bridlington and the Wolds and Goole and Pocklington . The Kingston upon Hull area is divided into three constituencies; Kingston upon Hull North and Cottingham , Kingston upon Hull East , and Kingston upon Hull West and Haltemprice . Until 1 April 2009,

2340-399: A lot of water was still locked in the northern ice sheets, sea level was much lower than in the present day and an area of land stretched eastwards to the low countries. The Wolds area takes the form of an elevated, gently rolling plateau , cut by numerous deep, steep-sided, flat-bottomed valleys of glacial origin. The chalk formation of the hills provides exceptionally good drainage, with

2470-434: A new bridge on the same site but a different alignment, to eliminate the awkward turn at the west end, which was costed at £2 million. None of these actions have been taken, as the bridge leaves were raised in 1994, and have remained raised ever since. Consideration was given in 2007 to preserving two of the hydraulic rams which operated the bridge, during planning to demolish the structure. The Hull Hydraulic Power Company

2600-403: A person and burglary. Christianity is the religion with the largest following in the area, with 53.3% residents so identifying in the 2021 UK census . These census figures show no other single religion returned affiliation, as a percentage of population, above the national average for England. At the time of the 2021 census the population of the East Riding was 342,215 and its ethnic composition

2730-578: A second opinion, and John Grundy, Jr. suggested a much longer canal, running for 5 miles (8.0 km) from Fisholme on the Frodingham Beck. When fully opened in 1770, the new route was some 3 miles (4.8 km) shorter than the river, which follows an extremely winding course in its upper reaches. The river above Aike was now considered to be part of the Driffield Navigation, and tolls were charged for its use. Also in this period

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2860-479: A second phase in 1805, and the Beverley and Barmston Drain to the west was completed in 1810. Since 1980, the mouth of the river has been protected by a tidal barrier at the estuary, which can be closed to prevent tidal surges entering the river system and causing flooding upriver. Most of the bridges which cross the river are movable, to allow shipping to pass. There are six swing bridges; four bascule bridges , two of which have twin leaves, one for each carriageway of

2990-545: A smaller territorial range and as population levels increased, they started to try to modify or control the natural world. In the Great Wold Valley , pollen samples of Mesolithic date indicate that the forest cover in the area was being disturbed and altered by man, and that open grasslands were being created. The Yorkshire Wolds became a major focus for human settlement during the Neolithic period as they had

3120-402: A tidal barrier has been constructed to prevent tidal surges from entering the river. In the past, these had regularly flooded the town and the flat countryside to the north. The River Hull has served as a navigation and a drainage channel, and has been subject to the conflicts that this usually creates, as water levels need to be raised for navigation, but lowered for efficient drainage. In 1213,

3250-530: A wet and swampy area which became the plain of Holderness . Another ice sheet in the Vale of York retreated at the same time leaving thick glacial deposits and two prominent moraines to the west of the Wolds. These Vale of York deposits also formed wetlands . The Wolds themselves were largely ice-free, well-drained, chalk uplands. Gradually the tundra conditions that had existed as the ice retreated gave way to vegetation that could support grazing fauna. Because

3380-558: A wide range of natural resources. The oldest monuments found on the Wolds are the Neolithic long barrows and round barrows . Two earthen long barrows in the region are found at Fordon , on Willerby Wold, and at Kilham , near Driffield , both of which have radiocarbon dates of around 3700 BC. From around 2000 to 800 BC, the people of the Bronze Age built the 1,400 Bronze Age round barrows that are known to exist on

3510-568: A year. Some of this is transported by longshore drift with about 3% of material being deposited at Spurn Head spit, to the south. The coastline has retreated noticeably in the last 2,000 years, with many former settlements now flooded, particularly Ravenser Odd and Ravenspurn , which was a major port until its destruction in the 14th century. Erosion is an ongoing concern in the area. The East Riding of Yorkshire Council has been carrying out cliff erosion defences between Sewerby and Kilnsea since 1951. The Holderness area drains mostly into

3640-437: A £10 million upgrade of the structure was started, to ensure it would stay operational for a further 30 years. The upgrade included a new drive mechanism, which raises and lowers the gate, and pivots it when it is at the top of the structure, so that it lies horizontally rather than vertically. It also included a new control system. In July 2017 the barrier was granted Grade II listed status. Plans have been considered to build

3770-425: Is a particularly strong deficit in the number of young adults. There is a higher-than-average level of car ownership. 36.4% of all households do not have a car. Less than 5% of the population travel to work by public transport compared with 15% nationally. The district is one of the lowest non-white populations , with the census reporting 98.8% of the inhabitants being white. Hull itself is also quite monoethnic for

3900-556: Is a tour of East Yorkshire churches which were built, rebuilt or restored by the Sykes family of Sledmere House in the 19th century. The East Riding has only a small segment of motorway. Part of the M62 serves to link the Hull area to West Yorkshire and the national motorway network, while the M18 incidentally passes the district border near Goole. Primary roads in the district include

4030-459: Is by far the largest settlement, with population of 267,014, and is a major port and the county's economic and transport centre. The rest of the county is largely rural, and the next largest towns are the seaside resort of Bridlington (35,369) and the historic town of Beverley (30,351), which is also the county town . The county is governed by two unitary authorities, East Riding of Yorkshire Council and Hull City Council . It takes its name from

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4160-480: Is dominated by deposits of till, boulder clays and glacial lake clays . These were deposited during the Devensian glaciation . The glacial deposits form a more or less continuous lowland plain which has some peat filled depressions (known locally as meres) which mark the presence of former lake beds. There are other glacial landscape features such as drumlin mounds, ridges and kettle holes scattered throughout

4290-427: Is less than it once was. The Beverley and Barmston Drain rejoins the river above Scott Street Bridge. Below North Bridge, an unused dry dock on the west bank marks the former entrance to Queens Dock. Below Drypool Bridge, a muddy basin on the east bank was once the entrance to Drypool Basin and Victoria Dock. The river reaches its confluence with the Humber Estuary in the centre of Kingston upon Hull . At its mouth,

4420-702: Is the most populous of coastal settlements, others include Flamborough , Hornsea, Withernsea and Aldbrough . Settlements on the flat agricultural area of Holderness are Hedon and Roos and in the Great Wold Valley is Rudston . Beverley , Bishop Burton , Driffield, Cottingham and Lockington lie is the Yorkshire Wolds eastern foot. Low-lying lands close to the Humber Estuary are Goole , Brough , North Ferriby , Hessle and Kirk Ella . Stamford Bridge , Pocklington , Market Weighton , Holme-on-Spalding-Moor , Howden and South Cave all lie to

4550-716: Is the site of the famous battle, and the Yorkshire Wolds Way is a long-distance footpath that takes a winding route through the Yorkshire Wolds to Filey . Most of the East Riding is in the East Riding Archdeaconry of the Church of England Diocese of York . The archdeaconry includes the Yorkshire Wolds and the City of Hull, with a coastline extending from Scarborough and Bridlington in

4680-774: Is used to describe the meeting of tidal or other non-riverine bodies of water, such as two canals or a canal and a lake. A one-mile (1.6 km) portion of the Industrial Canal in New Orleans accommodates the Gulf Intracoastal Waterway and the Mississippi River-Gulf Outlet Canal ; therefore those three waterways are confluent there. The term confluence can also apply to the process of merging or flowing together of other substance. For example, it may refer to

4810-555: The A614 . Confluence 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 [downstream of confluences] of increasing stream flow and decreasing slopes drives

4940-721: The A63 , A164 , A165 , A1034 , A166 , A1033 and the A1079 . Hull Paragon Interchange is a large railway station, served by the Selby Line to the west and the Yorkshire Coast Line to the north. See Railway stations in the East Riding of Yorkshire . Train operators active in the area are Hull Trains , London North Eastern Railway , Northern and TransPennine Express . Bus services are provided by several operators including First York , which provides services from

5070-561: The Archbishops of York laid claim to the river, and declared their right to navigate on a 24-foot (7.3 m) channel. A number of fish-weirs made navigation difficult, and the Archbishop negotiated their removal in 1296, so that a wharf could be established at Grovehill to serve the town of Beverley . By 1321, river rights had been extended to the charging of tolls. One-third of a shilling (4d equivalent to 1.7p decimal currency)

5200-538: The Conservative Party gained a majority of seats, including those of the Liberal Democrat and Labour Party leaders. The council has a leader-and-executive system , led by Steven Parnaby of the Conservative Party since its creation until his retirement at the 2019 election , when Richard Burton was elected as his replacement. On 13 May 2021, Jonathan Owen was elected as the new leader of

5330-495: The East Riding or East Yorkshire , is a ceremonial county in the Yorkshire and the Humber region of England. It borders North Yorkshire to the north and west, South Yorkshire to the south-west, and Lincolnshire to the south across the Humber Estuary . The city of Kingston upon Hull is the largest settlement. The county has an area of 2,479 km (957 sq mi) and a population of 600,259. Kingston upon Hull

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5460-536: The East Riding , a historic subdivision of Yorkshire . In the east of the county the low-lying plain of Holderness is enclosed by a crescent of low chalk hills, the Yorkshire Wolds . The Wolds meet the sea at Flamborough Head, a chalk headland, while the Holderness coast to the south is characterised by clay cliffs. The west of the county is part of the Vale of York , the wide plain of the River Ure / Ouse ;

5590-750: The Local Government Act 1888 , administrative counties were formed on the existing historic county boundaries in England, but in Yorkshire, given the vast size of the county area, three administrative county councils were created, based on the historic boundaries of the three Ridings. A county council for the East Riding of Yorkshire (the East Riding County Council ) was set up in 1889, covering an administrative county local government area centred on Beverley and which had

5720-485: The Local Government Act 1972 , the historic established Lieutenancy and the local government administrative county were disbanded, being replaced by the newly created Humberside County Council which included most of the East Riding and additional parts of the West Riding and parts of Lincolnshire. The creation of this cross-Humber authority was unpopular on both banks of the Humber. Due to this local unpopularity with

5850-657: The North Sea , and to the south drains into the Humber Estuary. South of Flamborough Head is Bridlington, which features several beaches, and at the far south-east of the district is the Spurn peninsula. Before the last ice age the eastern coastline of the area was located along the eastern foot of the Yorkshire Wolds where remnants of beaches have been discovered. The North Sea ice sheet deposited huge amounts of boulder clay as it retreated and this subsequently formed

5980-526: The River Hull , which was also improved to aid navigation. The Market Weighton Canal connected the town directly to the Humber Estuary . The canals and canalisation of the county's rivers helped aid drainage to low-lying and ill-drained areas. The 19th century saw a rail network created. An early rail link was constructed between Filey and Bridlington in 1847 and the Malton to Driffield railway

6110-532: The enclosure of the open fields in the 18th and 19th centuries, except for some hedgerows removed to allow for the use of large agricultural machinery in the 20th century. The traditional cultural and historic geographic county, the East Riding of Yorkshire borders the North Sea to the east of the county. To the north across the River Derwent is the North Riding of Yorkshire , and to

6240-482: The 1870 bridge was accepted. The bridge was contracted in 1927 for £86,100 to the Widnes Foundry (1295) Ltd , who constructed as a Scherzer rolling lift bridge ( or "Walking lift bridge"). The bridge was Grade II listed in 1994. Replaced an earlier swing bridge, also known as Drypool Bridge or Salthouse Lane Bridge, sanctioned 1885, with construction beginning 1887, and opening 1889, at a cost of £18,550, with

6370-645: The 18th century until it had been replaced in 1801, was demolished by the County Council, who installed a steel rolling bridge in its place. Once the Tickton Bypass bridge had been built a short distance upstream, it no longer needed to carry road traffic, and it was replaced by a footbridge in 1976. At the other end of the river, the Millennium Bridge was opened in 2001. There was once a ferry at this point, before 1865, which gave access to

6500-567: The Anglian elements -ing, -ingham or -ham started to be found in settlement names. As Christianity was established in the area from the 7th century onwards, several cemeteries like the one at Garton on the Wolds show evidence of the abandonment of pagan burial practices. In AD 867, the Great Danish Army captured the Anglian town of York. The remnants of the army settled from AD 876 as their leader Halfdan shared out

6630-460: The Beverley and Barmston Drain, which collects water from the catchwater drains on either side of the main channel, flows under the navigation in a tunnel, and runs just to the west of the river almost to its mouth. Below the lock, the surrounding land is almost at sea level, and the river is constrained by flood banks on both sides. On its route southwards, the river passes the former junction with Aike Beck , once navigable to Lockington Landing, but

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6760-514: The Driffield Navigation was relatively steady between 1871 and 1905, falling slightly from 35,654 to 32,666 tons. Goods carried included coal, linseed, cottonseed, wheat, flour and artificial manures. In 1922, £7 of income was received from pleasure craft using the navigation. Traffic declined during the 1930s, with commercial traffic finally ceasing in 1944. The Leven Canal carried 4,242 tons in 1888 and 4,546 in 1905, but then succumbed to road competition, and closed in 1935. The problems of flooding of

6890-592: The Driffield Trout Stream. After the junction, it becomes the River Hull or the West Beck and flows to the east, before turning south to reach Corps Landing. For much of the route below Driffield, the Driffield Navigation runs parallel to the river. The river from Corps Landing to its mouth is navigable. At Emmotland , it is joined by the Frodingham Beck, which is also navigable, and leads to

7020-444: The East Riding into York, Goole Town Service and also services from Goole to Doncaster. Stagecoach in Hull provides services from the East Riding to Hull and into Lincolnshire, and East Yorkshire Motor Services , historically the dominant area operator, provides a wide variety of bus services throughout the East Riding. Yorkshire Coastliner provides services from Bridlington to Malton, York and Leeds. Holderness Area Rural Transport,

7150-473: The East Riding was the largest district and the largest unitary authority in England by area and the second-largest non-metropolitan district in England by population. Following the 2009 structural changes to local government in England it fell to fifth place by area and sixth place by population. The East Riding of Yorkshire covers 240,768 hectares (930 sq mi) and has a population of 335,049 (2008 Office for National Statistics mid-year estimates),

7280-516: The Ennerdale Link road included a tunnel under the river. Initial investigations suggested that there was a layer of boulder clay below the alluvium of the river bed, and that a chalk aquifer was below the clay. Construction work started in July 1991. A cofferdam was built on the east bank, and the cutting which would have provided access to the twin-bore tunnel was nearly excavated when

7410-420: The Hull area which cross the River Hull. Details of them are shown in the following table, starting from that furthest north and moving south to the river mouth. Grade II listed in 1994. This is the oldest river bridge in the city, and connects the areas of Wilmington, Kingston upon Hull and Sculcoates A double bascule bridge. The bridge, bridgemasters hut, railings and lamps were Grade II listed in 1994. It

7540-503: The Humber and the eponymous River Hull drains the area north of Hull. The western part of the district in the Vale of York borders on and is drained by the River Derwent . The landscape is generally low-lying and flat although minor ridges and glacial moraines provide some variations in topography. Where there are dry sandy soils there are remnants of historic heathlands and ancient semi-natural woodlands. Arable fields dominate

7670-481: The Leven Canal and Hull once a week. Between 1848 and 1905, traffic on Beverley Beck more than trebled, from 33,498 tons to 101,540 tons. Coal and other minerals accounted for around one quarter of the traffic in 1905, while goods carried in 1906 included fertiliser, burnt ore, flour and scrap metal. Commercial traffic continued into the 1970s, when tolls of £2,365 were collected on 28,169 tons of cargo. Traffic on

7800-541: The River Hull is in the Yorkshire Wolds . It rises from a series of springs to the west of Driffield, near the site of the medieval village of Elmswell . The Elmswell Beck flows eastwards from these, and is joined by the Little Driffield Beck, which flows southwards from Little Driffield. It continues as the Driffield Beck, flowing around the south-western edge of Driffield , where it is joined by

7930-593: The Vale of York were also being used for animal rearing at this time. In the Iron Age there were further cultural changes in the area. There emerged a distinctive local tradition known as the Arras Culture , named after a site at Arras, near Market Weighton . There are similarities between the chariot burials of the Arras Culture and groups of La Tène burials in northern Europe, where the burial of carts

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8060-565: The Victoria Dock, opened in 1850. South Bridge replaced the ferry in 1865, making it easier for workers to reach the dock. The swing footbridge was closed in 1934, but was not demolished until 1944. The Environment Agency measure the water quality of the river systems in England. Each is given an overall ecological status, which may be one of five levels: high, good, moderate, poor and bad. There are several components that are used to determine this, including biological status, which looks at

8190-406: The Yorkshire Wolds. These are found both in isolation and grouped together to form cemeteries. Many of these sites can still be seen as prominent features in the present-day landscape. By the later Bronze Age, an open, cleared, landscape predominated on the Wolds. It was used for grazing and also for arable cultivation. The wetlands on either side of the Wolds in the River Hull valley, Holderness and

8320-479: The anticyclones tend to bring dry settled conditions which can lead to drought, particularly on the Wolds. For its latitude this area is mild in winter and cooler in summer due to the influence of the Gulf Stream in the northern Atlantic Ocean. Air temperature varies on a daily and seasonal basis. The temperature is usually lower at night, and January is the coldest time of the year. The two dominant influences on

8450-399: The area in which the Lord Lieutenant of the East Riding of Yorkshire represents the Crown , was re-established the same day, covering the City of Kingston upon Hull as well as the East Riding of Yorkshire Council area as did predecessor authorities. The East Riding of Yorkshire is entirely parished ; the City of Hull has no parishes. From 1996 Beverley had Charter Trustees to maintain

8580-449: The area. The well-drained glacial deposits provide fertile soils that can support intensive arable cultivation. Fields are generally large and bounded by drainage ditches . There is very little woodland in the area, and this leads to a landscape that is essentially rural but very flat and exposed. The Holderness coastline suffers the highest rate of coastal erosion in Europe: 2 metres a year on average or 2 million tonnes of material

8710-400: The canal into Driffield, which forms the major part of the Driffield Navigation. Scurf Dyke joins from the west and is followed by Struncheon Hill lock, which marks the end of the Navigation, and the official start of the navigable River Hull. Below here, the river is tidal. The tidal range of tides can be up to 7 feet (2.1 m) in winter and 4 feet (1.2 m) in summer. Just above the lock,

8840-403: The charter of the borough of Beverley : these were replaced by a Beverley Town Council in 1999, and Bridlington was parished in 1999. The unparished area consisting of the urban district of Haltemprice was divided into various parishes in 1999 and 2000. The East Riding of Yorkshire Council is based at County Hall in Beverley , in the former headquarters of Humberside County Council , and

8970-534: The city of Hull . Beverley , a market town, is generally associated with affluence but, like any other town of its size, it also has areas that face disadvantage. Other areas of the East Riding of Yorkshire face significant deprivation. The seaside towns of Withernsea and Bridlington face similar challenges with unemployment, low educational attainment, and socioeconomic inequality. South East Holderness, consisting of small rural communities, deals with limited access to services, inadequate public transportation, and

9100-399: The climate of the area are the shelter against the worst of the moist westerly winds provided by the Pennines and the proximity of the North Sea. The East Riding of Yorkshire is divided into two council areas: Kingston upon Hull is managed by Hull City Council , and the rest of the county is managed by the East Riding of Yorkshire Council . A non-mayoral devolution deal was proposed for

9230-403: The council. Following the 2023 election the Conservative Party elected former deputy, Anne Handley, to be leader of the group. At the annual general meeting of the council on 18 May 2023 Handley was elected as leader of the council, with the Conservative Party running a minority administration with support of the independents. In the Audit Commission report covering 2007 the council was given

9360-410: The country. Other parts of the county are more diverse, including the suburbs of Hessle , Cottingham and Anlaby with Anlaby Common . These areas consist of a mix of housing tenures in a real range of properties, from small ex-authority estates, to grand period homes. Hessle and Cottingham in particular have seen a considerable amount of home building, supporting the regeneration and development of

9490-562: The county, a mayoral deal received approval from the Secretary of State as of September 2024. This would lead to the establishment of an East Yorkshire combined authority with powers over housing, job creation and public transport, including bus franchising. The administrative division of the East Riding of Yorkshire originated in antiquity. Unlike most counties in Great Britain, which were divided anciently into hundreds , Yorkshire

9620-413: The decline of traditional industries. Goole , an inland port town, has experienced a decline in its socioeconomic characteristic. Akin to much of the West Riding, this has coincided with the decline of industry over the latter half of the 20th century. The crime rate in the East Riding is lower than the national average in robbery, sexual offences, theft of a vehicle, theft from a vehicle, violence against

9750-459: The east side of the river. John Hoggard acted as Superintendent for the scheme, while Joseph Page was appointed as resident engineer, to oversee the construction of the drains and the outfall sluice. Grundy made regular visits until October 1767, by which time the sluice and the main drainage channels were completed, at which point he and Page moved on, while Hoggard oversaw additional work on the drains and banks, which lasted for several more years. By

9880-531: The engine had been altered and an express steam packet service would commence. Three boats were recorded as trading between Driffield and Hull every other day in a directory of Yorkshire published in 1823. Traffic for 1832 included 7,394 chaldrons of coal, 18,173 quarters of wheat, 7,745 quarters of oats, 19,396 quarters of barley and 4,555 sacks of flour. An additional 1,564 quarters of wheat and 8,194 sacks of flour were carried to or from Foston Mill, reached from Frodingham Beck. A regular carrier also operated between

10010-508: The export of their carpets in the downstream direction. The factory later became a corn mill. Toll rentals continued to increase on the Beverley Beck, rising from £190 to £435 between 1793 and 1835. Some 31,185 tons of cargo were carried in 1838. In 1817, a steam packet service started to run between Driffield and Hull. Three return trips each week were made, but the journey times were too long, and an advertisement in 1825 indicated that

10140-412: The fens in the twelfth and thirteenth centuries by the monks of Meaux Abbey , primarily to enable travel by boat, but these gradually became part of the drainage system. John Smeaton , when asked by the merchants of Driffield to advise on ways to allow keels to reach their town, suggested a small cut of about 1.2 miles (1.9 km) including one lock, from the river near Wansford . The merchants sought

10270-579: The first cut of the Holderness Drain was made, enabled by an act of 1764, originally outfalling onto the river. In addition to the drainage works to the east of the river, the banks were raised for 17 miles (27 km) on the east side, to prevent flooding. Although beyond their jurisdiction, the Navigation commissioners attempted to extend their powers, to improve the river below the junction with Aike Beck. They particularly wanted to replace

10400-587: The form of structural bracing. The velocities and hydraulic efficiencies should be meticulously calculated and can be altered by integrating different combinations of geometries, components such a gradients, cascades and an adequate junction angle which is sympathetic to the direction of the watercourse’s flow to minimise turbulent flow, maximise evacuation velocity and to ultimately maximise hydraulic efficiency. Since rivers often serve as political boundaries, confluences sometimes demarcate three abutting political entities, such as nations, states, or provinces, forming

10530-412: The former headquarters of East Riding County Council before that. There are 26 wards electing a total of 67 councillors in the district. The council elects on a four-yearly cycle with all seats up for election at the same time. It first had elections in 1995—a year before it came into its powers—as a shadow authority. Between 1995 and 2007 the council had No overall control . In the 2007 local elections

10660-499: The fort of Eboracum . There is evidence of extensive use of the light soils of the Wolds for grain farming in the Roman era. Several Roman villas which were the centres of large agricultural estates have been identified around Langton and Rudston . In the low-lying lands on either side of the Wolds there was an increase in the number of settlements between 500 BC and AD 500, as the land became drier and more accessible due to

10790-519: The land adjacent to the river were addressed by the construction of catchwater drains to both sides of it. The east side of the river was protected by the Holderness Drainage scheme. John Grundy worked on plans for the scheme which would protect 11,000 acres (4,500 ha) of low-lying land to the north-east of Hull. John Smeaton was also involved, although the final report was largely Grundy's work, and an Act of Parliament to authorise

10920-531: The land already belonging to lay owners, they formed some of the vast estate holdings which continued to exist in the Riding until the 20th century. The 18th century saw a canal network form, the River Derwent was canalised as far upstream as Malton and was linked to Pocklington by the cutting of the Pocklington Canal . Other canals were cut to join the towns of Beverley and Driffield to

11050-690: The land cover of the area and grasslands are infrequent. There are very few flood meadows left, although some significant areas remain on the lower reaches of the River Derwent. The East Riding generally has cool summers and relatively mild winters. Weather conditions vary from day to day as well as from season to season. The latitude of the area means that it is influenced by predominantly westerly winds with depressions and their associated fronts, bringing with them unsettled and windy weather, particularly in winter. Between depressions there are often small mobile anticyclones that bring periods of fair weather. In winter, anticyclones bring cold dry weather. In summer

11180-728: The land. The Danish consolidated the area into the Kingdom of Jorvik , Danelaw then the Norse North Sea Empire . Scandinavian settlement names started to be found, such as -by and -thorpe. Scandinavian rule in the area came to an end in AD ;954 with the death of Eric Bloodaxe . After the Norman Conquest of England by William the Conqueror in AD 1066, land across England was granted to followers of

11310-404: The lower river. However, it connected to a number of waterways on which tolls were collected, and so an indication of the traffic can be gained from the figures for these waterways. The main cargoes on Beverley Beck in 1730 were coal, bricks, turfs and wool, together with cereal crops, consisting of wheat, barley, oats and malt. Receipts from tolls more than doubled between 1732 and 1748, after which

11440-555: The main ironwork assembled by J. Butler and Co., of Stanningley, Leeds; the river walls and approaches by T.B Mather of Hull. The bridge was hydraulically powered from a supply provided by the Hull Hydraulic Power Company . Image. The present Drypool Bridge was designed by W. Morris, the Hull City Engineer, and it was built in Hull. The previous wrought iron swing bridge, which had opened in 1888,

11570-767: The monasteries, continued to improve and drain their holdings throughout the Middle Ages to maximise the rents they could charge for them. The governance structure in the Domesday survey of 1086 was Yorkshire , its ridings and Wapentakes —the latter two remnants of the Norse structure. In the mid-16th century Henry VIII of England dissolved the monasteries , resulting in the large areas of land owned by Meaux Abbey , Bridlington Priory and other monastic holdings being confiscated. The Crown subsequently sold these large tracts of land into private ownership. Along with

11700-613: The new Norman king and ecclesiastical institutions. When some of the northern earls rebelled, William retaliated with the Harrying of the North which laid waste to many northern villages. The land was then distributed among powerful barons, such as the Count of Aumale in Holderness and the Percy family in the Wolds and the Vale of York. These lay lords and ecclesiastical institutions, including

11830-422: The new county council name, two of the nine districts formed in the 1972 Act included East Yorkshire in their titles, though they only covered a fraction of the geographical East Yorkshire area ( East Yorkshire district , East Yorkshire Borough of Beverley ). Continued disquiet culminated in a number of local government reviews in the 1980s and 1990s. Twenty-two years after being set up, Humberside County Council

11960-607: The north and west of the area, between the River Derwent and the scarp slope of the Wolds. There are a wide range of interesting places to visit in the East Riding. These include historic buildings such as Burnby Hall , Burton Agnes Manor House , Burton Agnes Hall , Sewerby Hall , Skipsea Castle and the gun battery of Fort Paull . The religious edifices of the Rudston Monolith , Beverley Minster , Beverley Friary and Howden Minster can be visited at all seasons. The sails of Skidby Windmill can be seen providing

12090-435: The north to Spurn Point. The Middlesbrough Roman Catholic diocese covers Yorkshire's historic east and north ridings as well as the historic City of York. Notable religious sites include Beverley Minster , Howden Minster , Hull Minster and Bridlington Priory along with the historic parish church of St Augustine, Hedon , known as the 'King of Holderness', which is a Grade I listed building . The Sykes Churches Trail

12220-460: The other half living in the other 160 parishes. In comparison, Hull's population according to the same census was 243,589. The population density of the district was around 135 people per square km, which made it the least densely populated unitary authority after the Isles of Scilly , Rutland and Herefordshire . The East Riding has a larger than average number of residents aged 40 and above. There

12350-530: The power to grind flour on certain days, and natural sites provide interest at Spurn , Bempton Cliffs , Hornsea Mere , Humber Estuary , River Hull , Watton Beck , River Derwent , River Ouse , River Aire , River Trent and River Don , some of which are owned or run by the Yorkshire Wildlife Trust . The Driffield Navigation , Leven Canal , Market Weighton Canal and Pocklington Canal offer glimpses of tranquillity. Stamford Bridge

12480-510: The quantity and varieties of invertebrates , angiosperms and fish. Chemical status, which compares the concentrations of various chemicals against known safe concentrations, is rated good or fail. The water quality of the River Hull system was as follows in 2016. The reasons for the quality being less than good include sewage discharge and physical modification of the channel. Download coordinates as: East Riding of Yorkshire The East Riding of Yorkshire , often abbreviated to

12610-518: The result that most of these valleys are dry. Surface water is quite scarce throughout the Wolds. At Flamborough Head the Wolds rise up to form high chalk cliffs, where there are water-worn caves and stacks along the shore. Flamborough Headland is designated a Heritage Coast . Coastal erosion around Flamborough Head has led to visitors being warned by the Humber Coastguard to be very careful on coastal paths. The Holderness landscape

12740-493: The river onto the Humber is thought to have changed in the early medieval period. The original outlet has been identified at a place called Limekiln creek . A second channel Sayers Creek was cut or widened, with both outlets existing simultaneously at one point. Limekiln creek was subsequently reduced in flow to the level of a drain. The lower river was bordered by salt marshes in medieval times, when efforts were first made to drain them. Further upstream, channels were cut through

12870-575: The roads which they carry; and three Scherzer lift bridges, which are a type of rolling bascule bridge. The former Scott Street Bridge (taken out of use 1994 and dismantled 2020) was originally powered from a high pressure water main maintained by the first public power distribution company in the world. The name Hull is probably of Brittonic origin. The name may derive from *hūl , an element related to *hū- meaning "boil, soak, seethe" (< Old Celtic *seu-; c.f. River Sill in Europe). The source of

13000-418: The same boundaries as the historic riding. It also acted as the ceremonial county (Lieutenancy) area established for the area. At the same date a separate county borough of Kingston upon Hull , was created. The East Riding County Council and the county borough of Kingston upon Hull remained in place for eighty-six years until being removed for new administrative tiers of local government. In 1974 under

13130-399: The same height, whatever the state of the tide. On the eastern bank, Scarr constructed a variable-height landing, but the landing on the west bank was constructed by Beverley Council, and was fixed. Scarr campaigned to have a variable landing here as well, and was prepared to fund it, but his requests were always rejected. The fixed landing made access to the bridge difficult at high tides. When

13260-464: The section within the city of Hull came under the jurisdiction of the Port of Hull , with the same result. Most of its course is through low-lying land that is at or just above sea level, and regular flooding has been a long-standing problem along the waterway. Drainage schemes to alleviate it were constructed on both sides of the river. The Holderness Drainage scheme to the east was completed in 1772, with

13390-453: The sites for fortified triangular temples, where they practiced human sacrifice and other sacred rites. In Hinduism , the confluence of two sacred rivers often is a pilgrimage site for ritual bathing. In Pittsburgh, a number of adherents to Mayanism consider their city's confluence to be sacred. Mississippi basin Atlantic watersheds Pacific watersheds Occasionally, "confluence"

13520-409: The south and forms part of the ceremonial county area. Other councils areas adjacent to the unitary authority include North East Lincolnshire , beyond the Humber Estuary; North Lincolnshire , beyond the Humber and on land; Hull, Doncaster , North Yorkshire and York . Geologically the East Riding district is split into three parts. The western part is the eastern section of the Vale of York with

13650-721: The south-west is part of the Humberhead Levels . When the last glacial period ended, the hunter gatherers of the Palaeolithic period followed the animal herds across the land between continental Europe and Britain. Then, as conditions continued to improve and vegetation could support a greater diversity of animals, the annual range of seasonal movement by Mesolithic communities decreased, and people became more fixed to particular localities. Until about 6000 BC, Mesolithic people appear to have exploited their environment as they found it. As communities came to rely on

13780-494: The southern extension into the Humberhead Levels . In this area there is a belt of sandstones overlain by glacial and lake deposits formed at the close of the last ice age. The middle part is the Yorkshire Wolds , a chalk formation which extends from the Humber at North Ferriby to the coast at Flamborough Head , a chalk headland . The south-east of the district is the low-lying coastal plain of Holderness , which faces east to

13910-426: The stone Hull Bridge, near Beverley, with a swing bridge, which would make it easier for keels to reach Frodingham bridge. The Corporation of Beverley objected, because the bridge was the main route of communication between Beverley and Holderness , and the commissioners instead dredged parts of the river to improve access. Plans to improve Hull Bridge were again resisted by Beverley Corporation in 1799, but an agreement

14040-551: The stream was subsequently re-routed to join the Arram Beck . The Leven Canal used to join on the east bank, but the entrance lock has been replaced by a sluice. The Arram Beck flows in from the west, and then the river is crossed by Hull Bridge, the cause of repeated disagreement between the owners of the Driffield Navigation and the Corporation of Beverley , who owned the bridge. Just above Beverley Beck , which joins from

14170-399: The subsequent survey work on Jessop's behalf, although Jessop surveyed the River Hull in 1787, to identify how the outfall could be improved. Jessop visited the works from time to time, making seven visits between 1789 and 1792, while the day to day oversight of the scheme was handled by Plummer as resident engineer. Plummer was succeeded by Anthony Bower, who was engineer from 1792 to 1795, and

14300-613: The subsequent transport of metals downstream of the mixing zone." A natural phenomenon at confluences that is obvious even to casual observers is a difference in color between the two streams; see images in this article for several examples. According to Lynch, "the color of each river is determined by many things: type and amount of vegetation in the watershed, geological properties, dissolved chemicals, sediments and biologic content – usually algae ." Lynch also notes that color differences can persist for miles downstream before they finally blend completely. Hydrodynamic behaviour of flow in

14430-401: The system to ensure the longevity and efficiency of the structure. Engineers have to design these systems whilst considering a list of factors that ensure the discharge point is structurally stable as the entrance of the lateral culvert into the main structure may compromise the stability of the structure due to the lack of support at the discharge, this often constitutes additional supports in

14560-441: The time of its completion in 1772, the scheme had cost £24,000. Despite the Holderness scheme, there were still problems near Leven and Weel, and William Jessop spent a month inspecting the area before writing a report in July 1786. His plan advocated separating the water which fell on the uplands to the north and flowed through the low-lying areas, from the local drainage of those low-lying areas. George Plummer carried out most of

14690-421: The tolls for passing through it were reduced significantly. Passage through Hull had long been difficult, because of the number of ships which used the river for loading and unloading goods. In 1794, the merchants of Beverley had advocated the building of docks at Hull, with a separate entrance, so that traffic to the upper river would not be impeded, while the Driffield Navigation had unsuccessful attempted to get

14820-479: The tolls were let to an independent collector. The annual rent charged for this privilege doubled again between 1748 and 1792. There was a steady expansion of trade on the Driffield Navigation during the same period, as the dividends paid to shareholders rose from 1.5 to 4 per cent. In 1789, Bainton, Boyes and Co negotiated a lump sum payment to cover coal from the Aire and Calder Navigation to their new carpet factory and

14950-554: The west across the River Ouse is the West Riding of Yorkshire . In terms of neighbouring local government administration, the East Riding of Yorkshire unitary authority adjoins North Yorkshire to the north, north-west and to the west, South Yorkshire metropolitan area to the south-west and Lincolnshire across the Humber Estuary to the south. The City of Kingston upon Hull is a separate unitary authority immediately to

15080-433: The west of the river. The project included the construction of 23 miles (37 km) of drainage cuts, and building embankments along 20 miles (32 km) of the river. At Hull, an outfall sluice was constructed, and the drain passed through tunnels under eleven waterways, including the Beverley Beck. 27 bridges were built to carry roads over the drain, and the whole project was finished in 1810. There are several bridges in

15210-546: The west, is Grovehill Bridge, now a lift bridge but once a ferry bridge. Once the river reaches the outskirts of Hull, its course is marked by a series of bridges, most of which open to allow boats to pass. There are swing bridges, lift bridges and bascule bridges, and the river becomes part of the Port of Hull. The river, which is the dividing line between West and East Hull, bisects the city's industrial area. The bridges can cause traffic delays during high tides, though river traffic

15340-438: The whole scheme was completed in 1805, having cost £16,000. In 1796, Robert Chapman was asked to report on possible solutions for flooding to the west. His report formed the basis for the Beverley and Barmston Drainage Act, which was passed by Parliament in June 1798. Chapman was appointed as engineer for the scheme, which would cost £115,000, and would provide flood defences and drainage for 12,600 acres (5,100 ha) of land to

15470-483: The work was passed on 5 April 1764. The Trustees for the scheme wrote to Grundy and Smeaton in May 1764, asking them to work on the project. Grundy's wife had died only a fortnight previously, and the two engineers corresponded, but besides valuable comment on Grundy's plans for the outfall sluice, Smeaton had no further involvement, and it was Grundy who ran the project, which included 17 miles (27 km) of barrier bank along

15600-472: Was 97.4% white, compared with the English average of 81.0%. The area has a slightly higher elderly population, of 26.4% in 2021, than the national average. By population, the largest settlements in the ceremonial county are: Kingston upon Hull is administered separately from the East Riding of Yorkshire. Anlaby and Willerby are suburban villages, almost contiguous with the Hull urban area. Bridlington

15730-602: Was abolished on 1 April 1996. The area north of the Humber Estuary (i.e. the city of Hull, whose boundaries would remain unchanged, the former districts of East Yorkshire , Beverley , and Holderness , and the northern part of the former Boothferry district, including the Goole area) formed two unitary authorities . The East Riding of Yorkshire Council unitary authority and the Kingston upon Hull City Council unitary authority were formed on 1 April 1996. The ceremonial county,

15860-622: Was also practiced. The area became the kingdom of the tribe known as the Parisi . After invading Britain in AD 43, the Romans crossed the Humber Estuary in AD 71 to invade the Parisi tribe's territory. From their bridgehead at Petuaria they travelled northwards and built roads along the Wolds to Derventio, present-day Malton , and then westwards to the River Ouse where they built

15990-436: Was charged for each bushel carried on the river between Emmotland and the Humber, but the merchants of Hull were unhappy with this; eventually the river had free navigation, and goods could be carried on it without toll. The Arram Beck was also exempt from all tolls. It has remained free, except for 1 mile (1.6 km) from the mouth, which is part of the Port of Hull and is under the control of Hull Corporation. The outlet of

16120-644: Was divided first into three ridings and then into numerous wapentakes within each riding. The separate Lieutenancy for the riding was established after the Restoration , and the ridings each had separate Quarter Sessions . For statistical purposes in the 19th century an East Riding of Yorkshire registration county was designated, consisting of the entirety of the Poor Law Unions of Beverley, Bridlington, Driffield, Howden, Hull , Patrington, Pocklington, Sculcoates, Skirlaugh and York. In 1889 under

16250-483: Was finally reached in 1801, and an Act of Parliament was obtained in July of that year. William Chapman acted as engineer, as the act authorised the construction of towpaths, a new cut between Bethels Bridge and the lock at Struncheon Hill, to avoid a long loop in the river, and rebuilding of the bridge. The bridge cost £500, half of which was met by Richard Bethell, the owner of the Leven Canal , on condition that

16380-459: Was permanently raised in 1994 as the structure was too weak to carry traffic, and the cost of full repair was estimated at £5 million. In 2018, Banksy visited this bridge and left a piece of graffiti to honour Hull's year as City of Culture. Scott Street Bridge was finally removed in 2020. In 1925 plans were submitted for a new bridge; of which one costed at £275,000 with a straightened approach road approximately 30 yards (27 m) north of

16510-433: Was set up in 1872, and by 1876 was operating a pumping station on Machell Street. This supplied water to a high pressure main which ran from Wellington Street to Sculcoates Bridge, and was used by local industries to power machinery, including the bridge when it was constructed. Although the power company closed in the 1940s, it made Hull the first city in the world to have a public system of power distribution. The design for

16640-502: Was successfully constructed under the river in 2001. The 6.2-mile (10.0 km) long sewer runs from the city centre to a treatment works at Salt End . It was excavated using two tunnelling machines, which were manufactured in Canada and were named Maureen and Gloria . The tunnel was officially opened on 21 August 2001, when a Mini car was driven through it, recreating scenes from the film The Italian Job . Before 1897, there had been

16770-414: Was the first to cross the Wolds in 1853. Holidaymakers on the rail network expanded the coastal resorts of Bridlington, Hornsea and Withernsea . These routes also served the agricultural community in helping to get products to the expanding industrial markets to the port of Hull for export and the West Riding of Yorkshire for further production. The landscape in the East Riding has changed little since

16900-620: Was too narrow, with a carriageway which was 16 feet (4.9 m) wide. It was closed in May 1959, so that it could be demolished and Morris's new bridge opened in March 1961. Scott Street Bridge had gradually deteriorated, and a public consultation was held in 1986, to determine its future. By that time a 10-ton weight limit had been imposed on traffic using the bridge, because of its poor structural state. Three suggestions were made as to its future. These were to close and demolish it, to refurbish it at an estimated cost of £1.6 million, and to build

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