76-685: Woldgate is a minor road in the East Riding of Yorkshire , England, which follows the line of a Roman road . It runs for a distance of 10 miles (16 km) from a junction with the A165 on the western edge of Bridlington , through the village of Kilham , to a junction with the B1249 4 miles (6 km) north of Driffield . For most of its length Woldgate follows a low ridge of the Yorkshire Wolds , with extensive views to north and south. The Roman road ran from
152-652: 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
228-541: 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
304-450: 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
380-563: 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
456-682: 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,
532-399: 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
608-403: 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
684-476: A prehistoric landscape and four Neolithic cursus converge on the village area. Argham Dyke , a prehistoric earthwork dating from the Bronze Age, crosses the area near Rudston. There is also evidence of Iron Age and Romano British occupation as revealed by aerial photographs showing traces of fields, trackways and farms. A Roman villa has been excavated to the south-west of Rudston. The present day field pattern
760-532: 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
836-526: 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
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#1733085729455912-547: 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
988-568: 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
1064-425: 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
1140-546: 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
1216-459: 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
1292-475: 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
1368-436: Is the best known of these watercourses. It is a chalk stream which supports large stands of bur-reed . West of Boynton , Boynton Willow Garth SSSI is an example of fen carr with a mosaic of habitats consisting of fen, scrub, woodland and running water. In the more open areas of the lower valley vegetation includes meadowsweet and great willowherb. Under the woodland canopies wood avens and enchanters nightshade are present. In
1444-688: 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
1520-443: Is the result of parliamentary enclosure in the 18th and 19th centuries when large areas of common land were enclosed and a new system of land management was introduced. Farmers moved out of the villages onto scattered farmsteads linked to units of land. Nucleated farmsteads usually built of brick with slate or pan tiled roofs were constructed often located on high ground in the rolling farmland. These exposed locations were protected by
1596-625: 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
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#17330857294551672-564: The A614 . Great Wold Valley The Great Wold Valley is the largest and broadest of the valleys cutting into the Yorkshire Wolds in northern England . It carries the Gypsey Race , an intermittent stream, which runs from its source near Wharram-le-Street eastwards along and through the northern Yorkshire Wolds to reach the sea at Bridlington . It is known that the Great Wold Valley
1748-699: 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
1824-522: 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
1900-539: 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
1976-525: 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 ;
2052-720: 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
2128-479: 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
2204-641: 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
2280-516: 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
2356-450: The Vale of York blocked and then permanently altered the course of the Ure. The historic landscape of the Great Wold Valley provides an important insight into the activities of prehistoric peoples in the Wolds. The valley was an important place of worship in prehistoric times and the valley houses a number of important scheduled monuments dating back to Neolithic times. Rudston is the centre of
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2432-519: 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
2508-554: 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
2584-491: 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,
2660-473: 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),
2736-496: 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
2812-625: 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
2888-406: 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
2964-473: 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
3040-504: 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
3116-498: 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
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3192-453: 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
3268-534: 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
3344-501: 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
3420-727: The coast at Bridlington to York . Its line can be traced west from the western end of Woldgate along a series of bridleways and minor roads, and then a stretch of the A166 , to Stamford Bridge , where it crossed the River Derwent by a ford. Woldgate was the subject of a series of landscapes created in 2006 by the artist David Hockney . National Cycle Route 1 follows the eastern part of Woldgate. [REDACTED] Media related to Woldgate at Wikimedia Commons 54°04′54″N 0°17′37″W / 54.0816°N 0.2937°W / 54.0816; -0.2937 East Riding of Yorkshire The East Riding of Yorkshire , often abbreviated to
3496-523: 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
3572-410: 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
3648-550: 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
3724-413: 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
3800-412: 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
3876-495: 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
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#17330857294553952-519: 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
4028-690: 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
4104-696: 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
4180-558: The local vicinity. This seemingly 'magical' property is thought to be responsible for the number of significant Neolithic sites along its course, including the Rudston Monolith and the ancient burial mounds at Willy Howe , Duggleby Howe and Wold Newton . Howe, in this case a topographic name from Middle English , originated with the Old Norse word haugr meaning a small hill or a man-made mound or barrow. The underlying bedrock of
4256-752: 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
4332-596: 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
4408-422: 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
4484-541: 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
4560-435: 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
4636-456: 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
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#17330857294554712-401: The planting of shelterbelts of trees. Recreation and tourism enterprises including camping and caravan sites, hotels and fishing lakes, are to be found in the area of the valley close to Bridlington. Watercourses that are intermittent and irregular are locally referred to as 'gypsey springs'. They are found all over the Yorkshire Wolds. The Gypsey Race which passes through the Great Wold Valley
4788-520: 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
4864-510: 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
4940-418: 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
5016-409: 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
5092-707: 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
5168-442: 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
5244-410: The valley is chalk which was laid down in the Cretaceous period. On the sides of the valley wind blown sand and loess overlie the chalk and in the valley bottom alluvium covers undifferentiated deposits of fragmented chalk which were eroded from the hillsides in the Ice Age . In pre-glacial times the Great Wold Valley was the seaward outlet of the River Ure from Wensleydale but the ice sheets in
5320-436: 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
5396-417: 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
5472-593: 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,
5548-604: 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
5624-532: Was an important place of worship during Neolithic times and there are a number of scheduled monuments in the valley. There are two dramatic right angle bends in the course of the Gypsey Race, one turning to the south at Burton Fleming then another turning eastwards again at Rudston . This intermittent and irregular watercourse is believed to be affected by a siphoning action in underground reservoirs and can come into flood apparently regardless of recent rainfall in
5700-631: 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
5776-467: 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
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