114-667: The North York Moors is an upland area in north-eastern Yorkshire , England. It contains one of the largest expanses of heather moorland in the United Kingdom. The area was designated as a National Park in 1952, through the National Parks and Access to the Countryside Act 1949 . Covering an area of 554 sq mi (1,430 km), the National Park has a population of 23,380. It is administered by
228-599: A circular long distance bridle route created around the North York Moors which can be accessed at a number of locations. The steep escarpments that define the edges of the National Park on three sides are used by several gliding clubs. In late 2020, the National Park was named as an International Dark Sky Reserve. This honour confirms that the area has "low levels of light pollution with good conditions for astronomy". The National Park has two visitor centres which have tourist information and exhibitions, as well as
342-551: A collection of circular stone hut foundations on Percy Rigg. Other evidence of Iron Age occupation is scarce, having been obliterated by subsequent agricultural activity. By 71 AD, the Roman army had reached Yorkshire, where they established a fort at Malton. Wade's Causeway may have been one of the several Roman roads which radiated from this point. It led north-eastwards over the Vale of Pickering and across Wheeldale Moor towards
456-532: A contemporary gallery. These are at: The North York Moors have not changed much in the past 50 years, and are often used as a location for British television programmes and films . The series Heartbeat and the scenes of Hogsmeade Station in the Harry Potter movies were filmed in Goathland . Yorkshire Yorkshire ( / ˈ j ɔːr k ʃ ər , - ʃ ɪər / YORK -shər, -sheer )
570-798: A cottage industry, centred on the old market towns moved to the West Riding where entrepreneurs were building mills that took advantage of water power gained by harnessing the rivers and streams flowing from the Pennines . The developing textile industry helped Wakefield and Halifax grow. The 19th century saw Yorkshire's continued growth, with the population growing and the Industrial Revolution continuing with prominent industries in coal, textile and steel (especially in Sheffield , Rotherham and Middlesbrough ). However, despite
684-661: A low watershed, is drained by the River Leven , which flows west to join the River Tees . On their south side, the moorland is incised by a series of dales which drain into tributaries of the River Derwent . The westernmost dale is Rye Dale , to the west of which rise the Hambleton Hills . Bilsdale is a side dale of Rye Dale. East of Bilsdale Bransdale , Farndale , Rosedale and Newton Dale cut into
798-521: A new Danish kingdom based at York. The Danes settled in the area and later themselves became Christian. They introduced their language, elements of which still remain in the local dialect, and renamed a number of settlements. King William I of England and his Norman barons took control of the nation in 1066. Central to the imposition of Norman rule was the building of castles. There are well-preserved castle ruins at Helmsley, Pickering and Scarborough and others existed at Ayton, Danby, Mulgrave and Whorlton. In
912-509: A number of gods, notably Woden . However, Christianity came to Yorkshire when King Edwin of Northumbria was baptised in 627 AD at York. Christian monasteries were established at Lastingham in 654 and Whitby in 657. A nunnery was built at Hackness in 680. In the 9th century, Viking raiders began to attack the Yorkshire coast, and in 867 these Danes destroyed the religious houses at Whitby, Lastingham and Hackness and after battle set up
1026-529: A separate kingdom. The Wessex Kings of England were reputed to have respected the Norse customs in Yorkshire and left law-making in the hands of the local aristocracy. In the weeks leading up to the Battle of Hastings in 1066 AD, Harold II of England was distracted by pushing back efforts to reinstate the kingdom of Jorvik and Danelaw. His brother Tostig and Harald Hardrada , King of Norway , having won
1140-583: A third of the population. When King Richard II was overthrown in 1399, antagonism between the House of York and the House of Lancaster , both branches of the royal House of Plantagenet , began to emerge. Eventually the two houses fought for the throne of England in a series of civil wars, commonly known as the Wars of the Roses . Some of the battles took place in Yorkshire, such as those at Wakefield and Towton ,
1254-551: A trio of very prominent and popular summits (the Yorkshire Three Peaks ) which can be climbed in a challenging single day's walk. The highest point in the Yorkshire part of the Peak District is Black Hill (height 582 metres (1,909 ft)) on the border with historic Cheshire (which also forms the historic county top of that county). The hill ranges along the eastern side of Yorkshire are lower than those of
SECTION 10
#17327657944221368-608: A vast expanse of the Yorkshire lowlands with the Pennines forming a backdrop. It was called the "finest view in England" by local author and veterinary surgeon James Herriot in his 1979 guidebook James Herriot's Yorkshire . The Royal Society for the Protection of Birds runs nature reserves such as the one at Bempton Cliffs with coastal wildlife such as the northern gannet , Atlantic puffin and razorbill . Spurn Point
1482-532: A widespread scattering of flint tools and the barbed flint flakes used in arrows and spears. By 5000 BC, as global sea levels rose and the North Sea came into existence, Britain was cut off from mainland Europe. During the New Stone Age, which lasted from around 4500 to 2000 BC, the population increased and agriculture was adopted. These early farmers were the first to destroy the forest cover of
1596-820: Is a tributary of the River Tees . It rises on Warren Moor, part of Kildale Moor, in the North York Moors and flows to the north of the moors to join the River Tees at Yarm . The source of the river is on Warren Moor, part of Kildale Moor, just south of the village of Kildale . The river flows east until it reaches the Whitby to Middlesbrough railway line where it turns around to flow west to Kildale. It then flows south-south-west through woodland to its confluence with Dundale Beck where it turns north-west through Low Easby and Little Ayton, before turning west and then south-west at Great Ayton . It runs parallel to
1710-516: Is a narrow 3-mile (4.8 km) long sand spit . It is a national nature reserve owned by the Yorkshire Wildlife Trust and is noted for its cyclical nature whereby the spit is destroyed and re-created approximately once every 250 years. There are seaside resorts in Yorkshire with sandy beaches; Scarborough is Britain's oldest seaside resort dating back to the spa town -era in the 17th century, while Whitby has been voted as
1824-598: Is abundant rain and poor drainage. Cotton grass is a distinctive plant which grows in the boggy areas. In the cold acid waters of peat bogs there is little decomposition of organic material with the result that the dead sphagnum moss gradually accumulates to form peat. This raises the levels of the bogs and they dry out. Heather then invades the area. Large areas of the moorland are now covered in heather, bilberries and grasses growing on thick layers of peat. The acid soils and peat bogs are unsuitable for earthworms so species which usually feed on earthworms such as moles and
1938-403: Is an area of Northern England which was historically a county . Despite no longer being used for administration, Yorkshire retains a strong regional identity. The county was named after its original county town , the city of York . The south-west of Yorkshire is densely populated, and includes the cities of Leeds , Sheffield , Bradford , Doncaster and Wakefield . The north and east of
2052-450: Is burned in strips by gamekeepers and farmers to encourage new heather growth to feed the grouse. Grouse shooting is part of the moorland economy. About 20 per cent of the national park is covered in bracken . Few things can grow under its dense cover and it does not support many insects and is unpalatable to most animals. The bracken is extremely invasive. Sheep are a ubiquitous part of the moorland landscape. Their grazing helps to maintain
2166-437: 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 fine weather. In winter, anticyclones bring cold dry weather. In summer, the anticyclones tend to bring dry settled conditions, which can lead to drought. For its latitude, this area
2280-544: Is milder in winter and cooler in summer due to the influence of the Gulf Stream in the North 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 the climate of the North York Moors are the shelter against the worst of the moist westerly winds provided by the Pennines and
2394-504: Is not, as is sometimes claimed, the highest waterfall in England ( Hardraw Force in Wensleydale , also in Yorkshire, has a 30 metres (98 ft) drop for example). However, High Force is unusual in being on a major river and carries a greater volume of water than any higher waterfall in England. The highest mountains in Yorkshire all lie in the Pennines on the western side of the county, with millstone grit and limestone forming
SECTION 20
#17327657944222508-574: Is now York and renamed it Jórvík , making it the capital city of a new Danish kingdom under the same name. The area which this kingdom covered included most of Southern Northumbria, roughly equivalent to the borders of Yorkshire extending further West. The Danes went on to conquer an even larger area of England that afterwards became known as the Danelaw ; but whereas most of the Danelaw was still English land, albeit in submission to Viking overlords, it
2622-487: Is sometimes referred to as "God's own country". Yorkshire is represented in sport by Yorkshire County Cricket Club and Yorkshire Rugby Football Union . There are several ways of defining Yorkshire, including the historic county and the group of four modern ceremonial counties. The county boundaries were reasonably stable between 1182, when it ceded western areas to the new county of Lancashire, and 1889 when administrative counties were created, which saw some adjustments to
2736-620: Is supported by the fact that yew trees were once abundant in the area around York, and that the city was known for its skilled bow makers who used yew wood to make their bows. This became 'Eboracum' to the Romans , 'Eorfowic' to the Angles and then, most famously, 'Jorvik' to the Vikings . Secondly, and much less reliable, is that it may come from the Old English word "Eow", which referred to
2850-723: Is variable from year to year, but the area gets much more snow on average than other parts of the country. Heavy falls are associated with northeasterly winds off the North Sea. Roads over the high moorland areas are notoriously prone to drifting snow due to the exposed nature of the terrain. Average recordings are: The geology of the North York Moors is dominated by rocks of the Jurassic period. They were mostly laid down in subtropical seas 205 to 142 million years ago. Fluctuations in sea level produced different rock types varying from shales to sandstones and limestones derived from coral. These marine and delta deposited rocks are well exposed on
2964-550: The Battle of Fulford . The King of England marched north where the two armies met at the Battle of Stamford Bridge . Tostig and Hardrada were both killed and their army was defeated decisively. Harold Godwinson was forced immediately to march his army south, where William the Conqueror was landing. The King was defeated in what is now known as the Battle of Hastings , which led to the Norman conquest of England . The people of
3078-603: The Brigantes (known to be in the north and western areas of now Yorkshire) and the Parisi (present-day East Riding ). The Brigantes controlled territory that later became all of Northern England and more territory than most Celtic tribes on the island of Great Britain . Six of the nine Brigantian poleis described by Claudius Ptolemaeus in the Geographia fall within the historic county. The Parisi, who controlled
3192-701: The Countryside and Rights of Way Act 2000 . Popular named walks include the Cleveland Way , which circles the North York Moors, including a coastal section; and the Lyke Wake Walk , which leads directly across the heart of the National Park. The route of the White Rose Way , a long distance walk from Leeds to Scarborough also passes through. The area also offers opportunities for cycling , mountain biking , and horse-riding , including
3306-520: The Devensian , ended about 11,000 years ago. The higher parts of the North York Moors were not covered by the ice sheets but glaciers flowed southwards on either side of the higher land mass. As the climate became warmer at the end of the ice age, the snowfields on the North York Moors began to melt. The meltwater was unable to escape northwards, westwards or eastwards because it was blocked by ice. Huge torrents of water were forced southwards. Water from
3420-688: The Dissolution of the Monasteries in 1536 led to a popular uprising known as Pilgrimage of Grace , started in Yorkshire as a protest. Some Catholics in Yorkshire continued to practise their religion and those caught were executed during the reign of Elizabeth I . One such person was a York woman named Margaret Clitherow who was later canonised . During the English Civil War , which started in 1642, Yorkshire had divided loyalties; Hull (full name Kingston upon Hull ) famously shut
3534-651: The North York Moors and Yorkshire Dales National Parks , and part of the Peak District National Park. Nidderdale and the Howardian Hills are designated Areas of Outstanding Natural Beauty , as is the North Pennines (a part of which lies within the county). Spurn Point, Flamborough Head and the coastal North York Moors are designated Heritage Coast areas, and are noted for their scenic views with rugged cliffs such as
North York Moors - Misplaced Pages Continue
3648-605: The River Derwent rises on the North York Moors, flows south then westwards through the Vale of Pickering then turns south again to drain the eastern part of the Vale of York. It empties into the River Ouse at Barmby on the Marsh . In the far north of the county the River Tees flows eastwards through Teesdale and empties its waters into the North Sea downstream of Middlesbrough . The smaller River Esk flows from west to east at
3762-578: The Roman Empire from Eboracum for the two years before his death. Another emperor, Constantius Chlorus , died in Eboracum during a visit in 306 AD. Thereafter his son Constantine the Great , who became renowned for his acceptance of Christianity, was proclaimed emperor in the city. In the early 5th century, Roman rule ceased with the withdrawal of the last active Roman troops. By this stage,
3876-742: The Vale of Pickering . Four roads cross the North York Moors from north to south. In the east, the A171 joins Whitby and Scarborough . Further inland, the A169 runs between Pickering and Whitby. More centrally, a minor road departs from the A170 at Keldholme and passes through Castleton before joining the A171 which connects Whitby and Guisborough . The most westerly route is the B1257 connecting Helmsley to Stokesley . The A170 from Thirsk to Scarborough marks
3990-424: The common shrew are absent on the moorland. The pygmy shrew survives by eating the insects and spiders that live in the heather. Lapwing , curlew and redshank breed on the moorland and there are sandpipers along the streams. Wheatear and golden plovers inhabit grassier patches on the moorland and ring ouzels live in stony areas. Red grouse , which feed on young heather shoots, are abundant. The heather
4104-613: The governance section below. For most administrative purposes the county had been divided since the Middle Ages; the last county-wide administrative role was the Sheriff of Yorkshire . The sheriff had been a powerful position in the Middle Ages but gradually lost most of its functions, and by the twentieth century was a largely ceremonial role. It was abolished as part of the 1974 reforms to local government, which established instead high sheriffs for each modern county. Historically,
4218-475: The jet cliffs at Whitby, the limestone cliffs at Filey and the chalk cliffs at Flamborough Head. Moor House – Upper Teesdale, most of which is part of the former North Riding of Yorkshire, is one of England's largest national nature reserves . At High Force on the border with County Durham, the River Tees plunges 22 metres (72 ft) over the Whin Sill (an intrusion of igneous rock). High Force
4332-469: The wood vetch and orchids are also to be found. Adders are widespread throughout the national park. On the moors they eat common lizards and around the hedgerows and woodland edges they feed on mice and voles. The limestone grasslands support a wide variety of wild flowers, and many rarer butterflies can be seen. Pearl-bordered fritillary , Duke of Burgundy fritillary , marbled white , dingy skipper and grayling are just some of species that inhabit
4446-435: The 11th and 12th centuries monasteries were established on the moors at Whitby Abbey , Rievaulx Abbey , Byland Abbey and Mount Grace Priory . Gifts of land and money were bestowed on these establishments and the monastic orders became notable landowners, eventually owning about a third of the land in the area. The abbeys managed their land as sheep farms and became very rich on the profits. They continued to take in land from
4560-409: The 19th century railways were built from Pickering to Whitby (1836), Middlesbrough to Whitby (1868) and Scarborough to Whitby (1884). Locally sourced iron ore has been processed on the North York Moors from medieval times. In the 19th century it became a boom industry. Dozens of ironstone mines and several short-lived blast furnaces were constructed. Between 1856 and 1926 high-grade magnetic ironstone
4674-541: The A173 to Stokesley. The river becomes increasingly meandering as it continues south-west past Skutterskelfe to Hutton Rudby and Rudby, where it turns north-west and then west again over Slape Stones waterfall. At Crathorne it turns north and then north-east as far as Middleton-on-Leven before passing under the A19 in a north-west direction. The final couple of miles are north and north-west between Ingleby Barwick and Yarm , before
North York Moors - Misplaced Pages Continue
4788-505: The Esk Valley, and East Yorkshire route 128 connects Scarborough and Helmsley. On weekends during the summer, these are complemented by Moorsbus services, which run from local urban centres into more remote parts of the national park which are difficult to access without private transport. Some of the routes across the North York Moors are noted for their beauty – the 840 was declared Britain's most scenic bus route by Bus Users UK while
4902-483: The Esk valley area flowed southwards gouging out the deep Newtondale valley as it went. Water from the North York Moors formed a vast lake in the area of the Vale of Pickering. Eventually this lake filled its basin and then overflowed at the lowest point which was at Kirkham. Here it cut the steep sided Kirkham gorge. When the ice finally retreated it left deep deposits of boulder clay (or till ) behind. The boulder clay blocked
5016-867: The Houses of York and Lancaster respectively, were combined to form the Tudor Rose of England. This rivalry between the royal houses of York and Lancaster has passed into popular culture as a rivalry between the counties of Yorkshire and Lancashire , particularly in sport (for example the Roses Match played in County Cricket ), although the House of Lancaster was based in York and the House of York in London. The English Reformation began under Henry VIII and
5130-591: The Middle Ages the county was subdivided into smaller administrative areas; the city of York was a self-governing county corporate from 1396, and the rest of the county was divided into three ridings – North , East, and West . From 1660 onwards each riding had its own lord-lieutenant , and between 1889 and 1974 the ridings were administrative counties . There was a Sheriff of Yorkshire until 1974. Yorkshire gives its name to four modern ceremonial counties : East Riding of Yorkshire , North Yorkshire , South Yorkshire , and West Yorkshire , which together cover most of
5244-587: The Moors and finally destroyed much of the original forest. The climate was relatively warmer and drier at this time so it was possible to live on the high moors throughout the year. When a piece of land was exhausted of nutrients, these people moved on, leaving behind land that was incapable of supporting anything but a heathland vegetation. There are about 3,000 Bronze Age burial mounds on the moors. The Iron Age dates from about 600 BC. There are remains of two promontory hill forts at Boltby Scar and Roulston Scar and
5358-465: The North Sea coast. There are Roman camps at Cawthorn and Lease Rigg near Grosmont and signal stations along the coast at Filey, Scarborough, Ravenscar, Goldsborough and Hunt Cliff . The Romans left Britain in 410 AD. After the departure of the Romans, Germanic tribes arrived and settled in the area. These Angles, Saxons and Jutes gave many of the place names to villages on the moors. They worshipped
5472-797: The North York Moors National Park Authority, which is based in Helmsley . To the east, the area is clearly defined by the impressive cliffs of the North Sea coast. The northern and western boundaries are defined by the steep scarp slopes of the Cleveland Hills edging the Tees lowlands and the Hambleton Hills above the Vale of Mowbray . To the south lies the broken line of the Tabular Hills and
5586-646: The North rebelled against the Normans in September 1069 AD, enlisting Sweyn II of Denmark . They tried to take back York, but the Normans burnt it before they could. What followed was the Harrying of the North ordered by William. From York to Durham , crops, domestic animals, and farming tools were scorched . Many villages between the towns were burnt and local northerners were indiscriminately murdered. During
5700-576: The Parliamentarians ("Roundheads") fought back, re-taking Yorkshire town by town, until they won the Battle of Marston Moor and with it control of all of the North of England . In the 16th and 17th centuries Leeds and other wool-industry-centred towns continued to grow, along with Huddersfield, Hull and Sheffield, while coal mining first came into prominence in the West Riding of Yorkshire . The wool textile industry, which had previously been
5814-512: The Romans enabled her to keep control of the kingdom; however, her former husband staged rebellions against her and her Roman allies. At the second attempt, Venutius seized the kingdom, but the Romans, under general Petillius Cerialis , conquered the Brigantes in 71 AD. The fortified city of Eboracum (now York) was named as capital of Britannia Inferior and joint capital of all Roman Britain . The emperor Septimius Severus ruled
SECTION 50
#17327657944225928-435: The United Kingdom's best beach, with a "postcard-perfect harbour". There are eight officially designated cities in Yorkshire: Bradford, Doncaster, Kingston upon Hull, Leeds, Ripon , Sheffield, Wakefield, and York. City status is formally held by the administrative territory rather than the urban area. River Leven, North Yorkshire The River Leven (pronounced / ˈ l i v ən / ) in North Yorkshire , England
6042-416: The Vale of Pickering flowing westwards, turns southwards at Malton and flows through the eastern part of the Vale of York before emptying into the River Ouse at Barmby on the Marsh . As part of the United Kingdom, the North York Moors area generally has warm 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
6156-564: The Western Empire was in intermittent decline. After the Romans left, small Celtic kingdoms arose in the region, including the kingdoms of Deira to the east (domain of settlements near Malton on Derwent ), Ebrauc (domain of York) around the north and Elmet to the west. The latter two were successors of land south-west and north-east of the former Brigantia capital. Angles (hailing from southern Denmark and northern Germany, probably along with Swedish Geats ) consolidated (merging Ebrauc ) under Deira, with York as capital. This in turn
6270-471: The X93 was the tenth most scenic. The cyclists in the 2018 and 2019 Tour de Yorkshire passed through a section of the North York Moors. The North York Moors consist of a moorland plateau, dissected by a number of deep dales or valleys containing cultivated land or woodland. The largest dale is Eskdale , the valley of the River Esk which flows from west to east and empties into the North Sea at Whitby . The Cleveland Hills rise north of Eskdale. At
6384-445: The Yorkshire coast from Staithes to Filey. Subsequently, about 30 million years ago, the land was uplifted and tilted towards the south by earth movements. The upper layers of rock were eroded away and the older rocks were exposed in places. Because of the tilt the oldest rocks became exposed in the north. These are the bands of shales and ironstones on the northern scarp of the North York Moors and Cleveland Hills. The middle layers form
6498-434: The air and salt or clear water. Rock pools contain sea anemones , blennies , crabs and molluscs . Sandy shores harbour a variety of plants and animals which are buried in the sand. Birds such as curlews and oyster catchers are to be seen prodding the sand to find these creatures for food. A few cormorants and fulmars breed along the coast where stonechats and rock pipits can also be spotted. Herring gulls are
6612-476: The area that would become the East Riding, might have been related to the Parisii of Lutetia Parisiorum , Gaul (known today as Paris, France). Their capital was at Petuaria , close to the Humber Estuary. Although the Roman conquest of Britain began in 43 AD, the Brigantes remained in control of their kingdom as a client state of Rome for an extended period, reigned over by the Brigantian monarchs Cartimandua and her husband Venutius . The capital
6726-414: The area was invaded and conquered for short periods by England between 927 and 954 before eventually being annexed into England in 954. It was closely associated with the much longer-lived Kingdom of Dublin throughout this period. An army of Danish Vikings , the Great Heathen Army as its enemies often referred to it, invaded Northumbrian territory in 866 AD. The Danes conquered and assumed what
6840-731: The area was split between North Yorkshire, South Yorkshire and West Yorkshire, which all kept the Yorkshire name. A large part of the east of the county went to the new county of Humberside , and an area in the north-east went to the new county of Cleveland . Some more rural areas at the edges of the historic county were transferred to County Durham, Cumbria , Lancashire and Greater Manchester , whilst South Yorkshire also included areas which had been in Nottinghamshire. Cleveland and Humberside were both abolished in 1996, since when there have been four ceremonial counties with Yorkshire in their names: East Riding of Yorkshire, North Yorkshire, South Yorkshire and West Yorkshire, which together cover most of
6954-426: The booming industry, living conditions declined in the industrial towns due to overcrowding. This saw bouts of cholera in both 1832 and 1848. However, advances were made by the end of the century with the introduction of modern sewers and water supplies . Several Yorkshire railway networks were introduced as railways spread across the country to reach remote areas. Canals and turnpike roads were introduced in
SECTION 60
#17327657944227068-431: The boundaries with County Durham, Lancashire and Lincolnshire. After 1889 there were occasional adjustments to accommodate urban areas which were developing across county boundaries, such as in 1934 when Dore and Totley were transferred from Derbyshire to Yorkshire on being absorbed into the borough of Sheffield. More significant changes in 1974 saw the historic county divided between several counties. The majority of
7182-454: The cold climate of the ice age ameliorated and temperatures rose above growing point of 5.5 °C (41.9 °F). Plant life was gradually re-established and animals and humans also returned. Around 8,000 BC, Britain was still part of the European landmass, and communities of Middle Stone Age people migrated to England and began to inhabit the North York Moors. Relics of this early hunting, gathering and fishing community have been found as
7296-432: The commonest breeding birds and are an interesting sight nesting in the chimneys of coastal towns. There are records of 12,000 archaeological sites and features in the North York Moors National Park of which 700 are scheduled monuments . Radio carbon dating of pollen grains preserved in the moorland peat provides a record of the actual species of plants that existed at various periods in the past. About 10,000 years ago,
7410-408: The conquest, only Bridlington , Pocklington , and York continued at a prominent level. In the early 12th century, people of Yorkshire had to contend with the Battle of the Standard at Northallerton with the Scots . Representing the Kingdom of England led by Archbishop Thurstan of York , soldiers from Yorkshire defeated the more numerous Scots. The population of Yorkshire boomed until it
7524-408: The county are more sparsely populated, however the north-east includes the southern part of the Teesside conurbation, and the port city of Kingston upon Hull is located in the south-east. York is located near the centre of the county. Yorkshire has a coastline to the North Sea to the east. The North York Moors occupy the north-east of the county, and the centre contains the Vale of Mowbray in
7638-480: The county councils. During the Second World War , Yorkshire became an important base for RAF Bomber Command and brought the county and its productive industries into the cutting edge of the war, and thus in the targets of Luftwaffe bombers during the Battle of Britain . From the late 20th century onwards there have been a number of significant reforms of the local government structures covering Yorkshire, notably in 1968, 1974, 1986, 1996 and 2023, discussed in
7752-415: The deposits on top of the bedrock are boulder clay . There is mixed agriculture, with some moorland and forestry near the source. Since a weir on the lower river was built during the Industrial Revolution , migratory and territorial fish and mammals had been missing from the river. In 2007, the Environment Agency built a fish bypass at the weir. In 2011, they announced the return of spawning salmon for
7866-405: The eastern end of the Vale of Pickering causing a permanent deviation in the course of the River Derwent. Alluvium from the glacial meltwater covers many areas to the north of the moors and in the Esk valley. The North York Moors National Park encompasses three main types of landscape, whose differences are clearly visible, and the coastal belt. There are predominantly green areas of pasture land,
7980-436: The edge of the Yorkshire Dales National Park and flows along Nidderdale before reaching the Vale of York and the Ouse. The River Wharfe , which drains Wharfedale , joins the Ouse upstream of Cawood . The Rivers Aire and Calder are more southerly contributors to the River Ouse and the most southerly Yorkshire tributary is the River Don , which flows northwards to join the main river at Goole . Further north and east
8094-399: The existence of many Celtic placenames in Yorkshire today, such as Kingston upon Hull and Pen-y-ghent . As well as the Angles and Geats, other settlers included Frisians (thought to have founded Fryston and Frizinghall ), Danes , Franks and Huns . At its greatest extent, Northumbria stretched from the Irish Sea to the North Sea and from Edinburgh down to Hallamshire in
8208-475: The families and subsequent descendants of Danish Vikings, the leadership of the kingdom nonetheless passed into Norwegian hands during its twilight years. Eric Bloodaxe , an ex-king of Norway who was the last independent Viking king of Jórvík, is a particularly noted figure in history, and his bloodthirsty approach towards leadership may have been at least partly responsible for convincing the Danish inhabitants of
8322-404: The first time in 150 years. In 2020, it was confirmed that crayfish plague had infected the river after 40 dead white-clawed crayfish were found along a 700-metre (2,300 ft) stretch of river. In Stokesley, the river is crossed by Taylorson's Bridge, a 17th-century packhorse bridge , which was once the only crossing in the town. The Domesday Book records a water mill on the banks of
8436-550: The gates of the city on the king when he came to enter a few months before fighting began, while the North Riding of Yorkshire in particular was strongly royalist . York was the base for Royalists, and from there they captured Leeds and Wakefield only to have them recaptured a few months later. The royalists won the Battle of Adwalton Moor meaning they controlled Yorkshire (with the exception of Hull). From their base in Hull
8550-415: The high ground. These woodland areas are the home of pied flycatchers, sparrow hawks and wood warblers . Roe and fallow deer can also be found here. The woodlands and south facing grasslands on the limestone belt provide a good habitat for many butterflies. The fertile alkaline soils support an abundance of wild flowers. Bluebells and primroses grow in the hedgerows in spring and rarer plants such as
8664-633: The historic county. Yorkshire Day is observed annually on 1 August and is a celebration of the general culture of Yorkshire , including its history and dialect . Its name is used by several institutions, for example the Royal Yorkshire Regiment of the British Army, in sport, and in the media. The emblem of Yorkshire is a white rose , which was originally the heraldic badge of the British royal House of York . The county
8778-575: The historic county. There is a region called Yorkshire and the Humber which covers a similar area to the combined area of the four Yorkshire ceremonial counties, the exceptions being that the region excludes the parts of North Yorkshire which had been in Cleveland, but includes North East Lincolnshire and North Lincolnshire (which had been in Humberside). Until 2009 some government powers in
8892-449: The industry grew in the middle of the 19th century in response to a fashion for the jewellery produced from it. In the 1880s cheap imports produced a decline in the industry which was focused on Whitby. The remains of alum quarries are to be found to the north of the area and along the coast. Alum was important to the textile industry because it was used as a mordant or fixative for dyes that were used to colour cloth. The industry thrived in
9006-541: The late 18th century. In the following century the spa towns of Harrogate and Scarborough flourished, due to people believing mineral water had curative properties. When elected county councils were established in 1889, rather than have a single Yorkshire County Council, each of the three ridings was made an administrative county with its own county council, and the eight larger towns and cities of Bradford, Halifax, Huddersfield, Hull, Leeds, Middlesbrough, Sheffield and York were made county boroughs , independent from
9120-401: The latter of which is known as the bloodiest battle ever fought on English soil. Richard III was the last Yorkist king. Henry Tudor , sympathiser to the House of Lancaster, defeated and killed Richard at the Battle of Bosworth Field . He then became King Henry VII and married Elizabeth of York , daughter of Yorkist Edward IV , ending the wars. The two roses of white and red, emblems of
9234-425: The livestock farms. The main arable crops are barley, wheat, oilseed rape, potatoes, and sugar beets. There is also some intensive production of pigs and poultry. Many visitors to the North York Moors are engaged in outdoor pursuits, particularly walking ; the National Park has a network of public rights of way almost 1,400 miles (2,300 km) in length, and most of the areas of open moorland are open access under
9348-483: The moorland. In the south east, the landscape is marked by the narrow valleys of the upper reaches of the Derwent and its upper tributaries. About 23 per cent of the North York Moors is under woodland cover (mostly located to the south-west and south-east), equivalent to more than 300 square kilometres of trees. It is home to the largest concentration of ancient and veteran trees in northern England. The Derwent crosses
9462-455: The moors. Their settlements were concentrated in the fertile parts of the limestone belt and these areas have been continuously farmed ever since. The Neolithic farmers grew crops, kept animals, made pottery and were highly skilled at making stone implements. They buried their dead in long low burial mounds. Around 2000 BC, the early Bronze Age Beaker People inhabited the Moors. During a 1,400 year period, these people inhabited all areas of
9576-798: The national park. The cliffs and sandy bays of the northern end of the Yorkshire Coast offer an assortment of seashore habitats. An area where the Cleveland Hills meets the sea has been designated as a Heritage Coast . The cliff at Boulby, at 690 feet (210 m), the highest point on the east coast of England is formed by Jurassic shales, clays and ironstones. There are also fine exposures of Jurassic rocks with their characteristic fossils around Robin Hoods Bay and Ravenscar. Rocky shores offer an abundance of seaweeds in zones of different types which are more and less tolerant of exposure to
9690-548: The north and the Vale of York in the south. The west contains part of the Pennines , which form the Yorkshire Dales in the north-west. The county was historically bordered by County Durham to the north, the North Sea to the east, Lincolnshire, Nottinghamshire , Derbyshire , and Cheshire to the south, and Lancashire and Westmorland to the west. It was the largest by area in the United Kingdom . From
9804-593: The northern boundary of Yorkshire was the River Tees , the eastern boundary was the North Sea coast and the southern boundary was the Humber Estuary and Rivers Don and Sheaf . The western boundary meandered along the western slopes of the Pennine Hills to again meet the River Tees. In Yorkshire there is a very close relationship between the major topographical areas and the geological period in which they were formed. The Pennine chain of hills in
9918-752: The northern foot of the North York Moors to reach the sea at Whitby . To the east of the Yorkshire Wolds the River Hull flows southwards to join the Humber Estuary at Kingston upon Hull . The western Pennines are drained by the River Ribble which flows westwards, eventually reaching the Irish Sea close to Lytham St Annes . The countryside of Yorkshire has been called " God's Own County " by its inhabitants. Yorkshire includes
10032-492: The open wild landscape that is needed for many other plants and animals to thrive. Limestone weathers quickly to produce nutrient rich alkaline soils on well drained rocks. Gouging by glacial meltwaters has left spectacular valleys along whose floors run streams. The limestone streams with their nutrient rich waters support an abundance of aquatic invertebrates such as insect larvae and crustaceans . These in turn support such fish as trout and grayling . Insects which emerge from
10146-510: The park each year, has been formed and maintained by generations of farmers. The 1996 Agricultural Census recorded a total workforce of 2,913 employed on 1,342 working farms. Sheep and cattle provide the prime source of farm income. The dale farms have rights to graze sheep on the open moor. The rights to moorland grazing are often essential to the economic viability of a farm. In recent years agriculture in Britain has suffered economic setbacks and
10260-405: The proximity of the North Sea . Late, chilly springs and warm summers are a feature of the area, but there are often spells of fine autumn weather. Onshore winds in spring and early summer bring mists or low stratus clouds (known locally as sea frets) to the coasts and moorland. Within the area, variations in climate are brought about by local differences in altitude, aspect and shelter. Snowfall
10374-406: The purple and brown heather moorland, and woodland. The three kinds of scenery are the result of differences in the underlying geology and each supports different wildlife communities. Sandstones erode slowly and form poor acid soils which are deficient in nutrients. They are less permeable to water, impeding drainage and encouraging the formation of bogs. Sphagnum moss bogs are common where there
10488-441: The region from the early 17th century until 1871. Its decline came when chemical dyes were discovered. The scars of industrial activity on the moors make it an interesting area in which to pursue industrial archaeology. The area's economy is mainly founded on tourism and agriculture . For over a thousand years the basis of the economy in the North York Moors was agriculture. The rural scene, which attracts millions of visitors to
10602-535: The region to accept English sovereignty so readily in the years that followed. After around 100 years of its volatile existence, the Kingdom of Jorvik finally came to an end. The Kingdom of Wessex was now in its ascendancy and established its dominance over the North in general, placing Yorkshire again within Northumbria , which retained a certain amount of autonomy as an almost-independent earldom rather than
10716-535: The region were devolved to the Yorkshire and Humber Assembly ; since 2009 the region has been used primarily for presentation of statistics. Yorkshire is so named as it is the shire (administrative area or county) of the city of York , or York's Shire. The word "York" has an interesting etymology, first it is believed to have originated from the Celtic word "Eburakon", which means "Place of yew trees ". This theory
10830-528: The river joins the River Tees. In October 2022, a new flood defence project was opened on the river above Stokesley. When river levels are high, a new flood channel diverts the excess water around the town, meeting the Leven again further downstream. The Environment Agency funded the project at a cost of £3.7 million. The river drains from the Cleveland Hills across a mixed geology of mostly Permian and Jurassic age bedrock of low permeability. Most of
10944-671: The rivers in the Ouse system is the River Swale , which drains Swaledale before passing through Richmond and meandering across the Vale of Mowbray . Next, draining Wensleydale , is the River Ure , which the Swale joins east of Boroughbridge . Near Great Ouseburn the Ure is joined by the small Ouse Gill Beck, and below the confluence the river is known as the Ouse. The River Nidd rises on
11058-525: The sandstones of the high moorland and the youngest layers of limestone form the Tabular Hills. In the dales, where the rivers have cut through the younger rocks, there are also exposures of older shales, ironstone and sandstone. Rosedale is an example of this. During the Quaternary period , the last 2 million years, the area has experienced a sequence of glaciations . The most recent glaciation,
11172-419: The settlements took the form of isolated farms and hamlets rather than villages. Very few had an open field system of agriculture so Enclosure Acts were rarer than in other parts of England. The 17th century saw a major acceleration in the reclaiming of marginal waste land and in the eighteenth century forward looking landlords attempted to improve their lands using drainage schemes and fertilisation measures. In
11286-442: The south. Scandinavian York (also referred to as Jórvík ) or Danish/Norwegian York is a term used by historians for the south of Northumbria (modern-day Yorkshire) during the late 9th century and first half of the 10th century, when it was dominated by Norse warrior-kings; in particular, used to refer to York , the city controlled by these kings. Norse monarchy controlled varying amounts of Northumbria from 875 to 954, however
11400-684: The southern boundary of the North York Moors area. The Esk Valley Line is an east-west branch line rail link from Whitby to Middlesbrough in the north, and the North Yorkshire Moors steam railway runs from Pickering to Grosmont with a link to Whitby. Other public transport within the North York Moors includes a number of bus services. Yorkshire Coastliner route 840 runs from Whitby to Pickering (and continues to York and Leeds), Arriva North East routes X93 and X94 run from Scarborough to Middlesbrough via Whitby and Guisborough, Arriva North East route 95 runs from Whitby to Lealholm along
11514-781: The underlying geology and producing distinctive layered hills. The county top is the remote Mickle Fell (height 788 metres (2,585 ft) above sea level) in the North Pennines southwest of Teesdale, which is also the highest point in the North Riding. The highest point in the West Riding is Whernside (height 736 metres (2,415 ft)) near to Ingleton in the Yorkshire Dales. Together with nearby Ingleborough (height 723 metres (2,372 ft)) and Pen-y-Ghent (height 694 metres (2,277 ft)), Whernside forms
11628-419: The viability of hill farming has become questionable. A number of environmental schemes to improve farm incomes have been devised but the industry continues to decline. Agricultural use of the moors is shared with grouse shooting as a means of gaining financial return from the vast expanse of heather. There is richer farmland across the southern limestone belt, where there are arable and mixed farms as well as
11742-435: The waste and what remained of the forest and in the process gave the moors the distinctive landscape that still remains. Between 1536 and 1541, Henry VIII of England dissolved the monasteries, and confiscated and sold off their property. This was bought by individual people, some rich, but also some who had been tenants of the monasteries, and became privately owned land. In many areas of the moors and their associated dales
11856-404: The water in summer are also a rich source of food for birds. Grey wagtails , swallows and spotted flycatchers are commonly seen. Dippers and kingfishers are also typical. The otter , after a period of decline, is starting to recolonise the rivers and streams. Farndale is famous for its wild daffodils in spring. Sheltered woodlands dominated by sessile oaks can be found to the south of
11970-549: The west is of Carboniferous origin. The central vale is Permo-Triassic . The North York Moors in the north-east of the county are Jurassic in age while the Yorkshire Wolds to the south east are Cretaceous chalk uplands. Yorkshire is drained by several rivers. In western and central Yorkshire the many rivers flow into the River Ouse which reaches the North Sea via the Humber Estuary . The most northerly of
12084-466: The west. The highest point of the North York Moors is Urra Moor (height 454 metres (1,490 ft)). The highest point of the Yorkshire Wolds , a range of low chalk downlands east of York, is Bishop Wilton Wold (height 246 metres (807 ft)), which is also the highest point of the East Riding. The view from Sutton Bank at the southeastern edge of the North York Moors near Thirsk encompasses
12198-457: The western end of Eskdale, the valley divides into three smaller dales, Westerdale (the upper valley of the River Esk), Baysdale and Commondale . A series of side dales drain into Eskdale from the moorland on its southern side, from west to east Danby Dale, Little Fryup Dale , Great Fryup Dale , Glaisdale and the Goathland valley. Kildale , west of Commondale and separated only by
12312-468: The winter that followed, families starved to death and thousands of peasants died of cold and hunger. Orderic Vitalis estimated that "more than 100,000" people from the North died from hunger. In the centuries following, many abbeys and priories were built in Yorkshire. Norman landowners increased their revenues and established new towns such as Barnsley , Doncaster , Hull , Leeds , Scarborough and Sheffield , among others. Of towns founded before
12426-465: The yew tree ( Taxus Baccata ). Yew trees were highly valued in ancient times for their durable wood, which was used for making bows, spears, and other tools. Over time, the word evolved into "York", and it eventually came to refer to the city of York in England. Either way, it is an evolved word for the magical 'Yew' tree. Early inhabitants of what became Yorkshire were Hen Ogledd Brythonic Celts (old north British Celts), who formed separate tribes,
12540-409: Was between the north and west ridings Isurium Brigantum (near Aldborough ) civitas under Roman rule. Initially, this situation suited both the Romans and the Brigantes, who were known as the most militant tribe in Britain. Queen Cartimandua left Venutius for his armour bearer, Vellocatus , setting off a chain of events that changed control of the region. Cartimandua's good relationship with
12654-509: Was grouped with Bernicia , another former Celtic - Brigantes kingdom that was north of the River Tees and had come to be headed by Bamburgh , to form Northumbria . Elmet had remained independent from the Germanic Angles until some time in the early 7th century, when King Edwin of Northumbria expelled its last king, Certic, and annexed the region to his Deira region. The Celts never went away, but were assimilated. This explains
12768-689: Was hit by the Great Famine of 1315. It did not help that after the English defeat in the Battle of Bannockburn in 1314, the Scottish army rampaged throughout northern England, and Yorkshire was no exception. During The Great Raid of 1322 , they raided and pillaged from the suburbs of York, even as far as East Riding and the Humber. Some like Richmond had to bribe the Scots to spare the town. The Black Death then reached Yorkshire by 1349, killing around
12882-799: Was in the Kingdom of Jórvík that the only truly Viking territory on mainland Britain was ever established. The Kingdom prospered, taking advantage of the vast trading network of the Viking nations , and established commercial ties with the British Isles , North-West Europe, the Mediterranean and the Middle East. Founded by the Dane Halfdan Ragnarsson in 875, ruled for the great part by Danish kings, and populated by
12996-485: Was mined in Rosedale. A railway was built around the top of the dale to serve the mines, and kilns were built to process the ore. In two decades the population of the valley rose from 558 to nearly 3000. Poor-quality coal was mined in many places on the moors from the 18th century to the early 20th century. The North York Moors is the only source for British jet . It has been mined in the area from prehistoric times but
#421578