Yorkshire Wolds
The Yorkshire Wolds are hills in the counties of the East Riding of Yorkshire and North Yorkshire in Northern England. They are the northernmost chalk hills in the UK and within lies the northernmost chalk stream in Europe, the Gypsey Race. On the western edge, the Wolds rise to an escarpment which then drops sharply to the Vale of York. The highest point on the escarpment is Bishop Wilton Wold (also known as Garrowby Hill), which is above sea level. To the north, on the other side of the Vale of Pickering, lie the North York Moors, and to the east the hills flatten into the plain of Holderness. The hills are separated by many dry dales, formed during the last ice age and where many springs rise. The largest town in the Wolds is Driffield, with other places including Pocklington, Thixendale and Kilham, the original 'capital' of the Wolds. The highest village on the Yorkshire Wolds is Fridaythorpe at above sea level. The market town of Beverley lies on the eastern ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Yorkshire Wolds Way
The Yorkshire Wolds Way is a National Trail in Yorkshire, England. It runs 79 miles (127 km) from Hessle to Filey, around the Yorkshire Wolds. At Filey Brigg, it connects with the Cleveland Way, another National Trail. In 2007 the Yorkshire Wolds Way celebrated the 25th anniversary of its official opening which took place on 2 October 1982. Route The route of the Yorkshire Wolds Way passes close to or through the following places: * Hessle * North Ferriby * Melton * Welton * Brantingham * South Cave * North Newbald * Goodmanham * Market Weighton * Londesborough * Nunburnholme * '' Pocklington'' * Millington * Huggate * Fridaythorpe * Thixendale * Wharram Percy * Wharram le Street * Wintringham * Sherburn * Potter Brompton * Ganton * Muston * Filey Places in italics are slightly off the main route. BBC documentary ''Yorkshire Wolds Way'', a 2017 two-part BBC television documentary, features a journey along the Yorkshire Wolds Way. Presenter Paul ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Pocklington
Pocklington () is a market town and Civil parishes in England, civil parish at the foot of the Yorkshire Wolds in the East Riding of Yorkshire, England. At the 2021 United Kingdom census, its population was 10,123. It lies east of York, and north-west of Kingston upon Hull, Hull. The town's skyline is marked by the 15th-century tower of All Saints' parish church. The ecclesiastical parish includes the hamlet of Kilnwick Percy. History Pocklington gets its name via the Old English "Poclintun" from the Angles (tribe), Anglian settlement of Pocel's (or Pocela's) people and the Old English word "tun" meaning farm or settlement, but though the town's name can only be traced back to around 650 AD, the inhabitation of Pocklington as a site is thought to extend back a further 1,000 years or more to the Bronze Age. Pocklington appears on the 14th-century Gough Map, the oldest route map in Great Britain. In the Iron Age Pocklington was a major town of the Parisi (tribe), Pari ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
North Sea
The North Sea lies between Great Britain, Denmark, Norway, Germany, the Netherlands, Belgium, and France. A sea on the European continental shelf, it connects to the Atlantic Ocean through the English Channel in the south and the Norwegian Sea in the north. It is more than long and wide, covering . It hosts key north European shipping lanes and is a major fishery. The coast is a popular destination for recreation and tourism in bordering countries, and a rich source of energy resources, including wind energy, wind and wave power. The North Sea has featured prominently in geopolitical and military affairs, particularly in Northern Europe, from the Middle Ages to the modern era. It was also important globally through the power northern Europeans projected worldwide during much of the Middle Ages and into the modern era. The North Sea was the centre of the Viking Age, Vikings' rise. The Hanseatic League, the Dutch Golden Age, Dutch Republic, and Kingdom of Great Britain, Brita ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Kingston Upon Hull
Kingston upon Hull, usually shortened to Hull, is a historic maritime city and unitary authorities of England, unitary authority area in the East Riding of Yorkshire, England. It lies upon the River Hull at its confluence with the Humber Estuary, inland from the North Sea. It is a tightly bounded city which excludes the majority of its suburbs, with a population of (), it is the fourth-largest city in the Yorkshire and the Humber region. The built-up area has a population of 436,300. Hull has more than 800 years of seafaring history and is known as Yorkshire's maritime city. The town of Wyke on Hull was founded late in the 12th century by the monks of Meaux Abbey as a port from which to export their wool. Renamed ''Kings-town upon Hull'' in 1299, Hull had been a market town, military supply port, trading centre, fishing and whaling centre and industrial metropolis. Hull was an early theatre of battle in the First English Civil War, English Civil Wars. Its 18th-century ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Humber
The Humber is a large tidal estuary on the east coast of Northern England. It is formed at Trent Falls, Faxfleet, by the confluence of the tidal rivers River Ouse, Yorkshire, Ouse and River Trent, Trent. From there to the North Sea, it forms part of the boundary between the East Riding of Yorkshire on the north bank and North Lincolnshire on the south bank. Also known as the River Humber, it is tidal its entire length. Below Trent Falls, the Humber passes the junction with the Market Weighton Canal on the north shore, the confluence of the River Ancholme on the south shore; between North Ferriby and South Ferriby and under the Humber Bridge; between Barton-upon-Humber on the south bank and Kingston upon Hull on the north bank (where the River Hull joins), then meets the North Sea between Cleethorpes on the Lincolnshire side and the long and thin headland of Spurn, Spurn Head to the north. Ports on the Humber include the Port of Hull, the Port of Grimsby and the Port of Immin ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Chalk Group
The Chalk Group (often just called the Chalk) is the lithostratigraphic unit (a certain number of rock strata) which contains the Upper Cretaceous limestone succession in southern and eastern England. The same or similar rock sequences occur across the wider northwest European chalk 'province'. It is characterised by thick deposits of chalk, a soft porous white limestone, deposited in a marine environment. Chalk is a limestone that consists of coccolith biomicrite. A biomicrite is a limestone composed of fossil debris ("bio") and calcium carbonate mud (" micrite"). Most of the fossil debris in chalk consists of the microscopic plates, which are called coccoliths, of microscopic green algae known as coccolithophores. In addition to the coccoliths, the fossil debris includes a variable, but minor, percentage of the fragments of foraminifera, ostracods and mollusks. The coccolithophores lived in the upper part of the water column. When they died, the microscopic calcium carbonat ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Cretaceous
The Cretaceous ( ) is a geological period that lasted from about 143.1 to 66 mya (unit), million years ago (Mya). It is the third and final period of the Mesozoic Era (geology), Era, as well as the longest. At around 77.1 million years, it is the ninth and longest geological period of the entire Phanerozoic. The name is derived from the Latin , 'chalk', which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation . The Cretaceous was a period with a relatively warm climate, resulting in high Sea level#Local and eustatic, eustatic sea levels that created numerous shallow Inland sea (geology), inland seas. These oceans and seas were populated with now-extinct marine reptiles, ammonites, and rudists, while dinosaurs continued to dominate on land. The world was largely ice-free, although there is some evidence of brief periods of glaciation during the cooler first half, and forests extended to the poles. Many of the dominant taxonomic gr ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Limestone
Limestone is a type of carbonate rock, carbonate sedimentary rock which is the main source of the material Lime (material), lime. It is composed mostly of the minerals calcite and aragonite, which are different Polymorphism (materials science), crystal forms of calcium carbonate . Limestone forms when these minerals Precipitation (chemistry), precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly Dolomite (rock), dolomite, a closely related rock, which contains a high percentage of the mineral Dolomite (mine ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Area Of Outstanding Natural Beauty
An Area of Outstanding Natural Beauty (AONB; , AHNE) is one of 46 areas of countryside in England, Wales, or Northern Ireland that has been designated for conservation due to its significant landscape value. Since 2023, the areas in England and Wales have also adopted the name National Landscape (). Areas are designated in recognition of their national importance by the relevant public body: Natural England, Natural Resources Wales, and the Northern Ireland Environment Agency respectively. On 22 November 2023, following a review, the AONBs in England and Wales adopted the National Landscapes name, and are in the process of rebranding. AONBs in Northern Ireland did not rename. The name "area of outstanding natural beauty" is still the designated legal term. In place of the term AONB, Scotland uses the similar national scenic area (NSA) designation. Areas of Outstanding Natural Beauty enjoy levels of protection from development similar to those of UK national parks, but unli ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Natural England
Natural England is a non-departmental public body in the United Kingdom sponsored by the Department for Environment, Food and Rural Affairs. It is responsible for ensuring that England's natural environment, including its land, flora and fauna, freshwater and marine environments, geology and soils, are protected and enhanced. It also has a responsibility to help people enjoy, understand and access the natural environment. Natural England focuses its activities and resources on four strategic outcomes: * a healthy natural environment * enjoyment of the natural environment * sustainable use of the natural environment * a secure environmental future Roles and responsibilities As a non-departmental public body (NDPB), Natural England is independent of government. However, the Secretary of State for Environment, Food & Rural Affairs has the legal power to issue guidance to Natural England on various matters. Its powers include defining ancient woodlands, awarding grants, designatin ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Molescroft
Molescroft is a village and civil parish in the East Riding of Yorkshire, England. It is situated approximately north-west of Beverley town centre adjoining its northern border. It lies to the north of the A1174 road and is on the eastern slopes of the Yorkshire Wolds. The Yorkshire Coast railway line from Hull to Scarborough passes through the parish but the nearest station is Beverley. According to the 2011 UK census, Molescroft had a population of 6,820, an increase on the 2001 UK census figure of 6,810. This is due to major housing developments in the north and east of the village due to unused greenfield land, firstly in the late 1990s and secondly, on a smaller scale, in the 2010s. Over 65s make up over 25% of the population, higher than Under 18s. Until the early 1990s, Molescroft was very small, with the majority of the modern village being used as allotments and small farming ventures. However, housing developers saw a large, cheap area of land to place housing fo ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Beverley
Beverley is a market town and civil parish in the East Riding of Yorkshire, England. It is located north-west of Hull city centre. At the 2021 census the built-up area of the town had a population of 30,930, and the smaller civil parish had a population of 18,014. It is the county town of the East Riding of Yorkshire. The town was founded in the seventh century by John of Beverley, who established a church in the area. It was originally named ''Inderawuda'', and was part of the Anglian kingdom of Northumbria. The town came under Viking control in the 850s, then became part of the Kingdom of England. John of Beverley was made a saint in 1037, and the town was a place of pilgrimage for the remainder of the Middle Ages. It continued to grow under the Normans, when its trading industry was first established, and eventually became a significant wool-trading town and the tenth-largest settlement in England. After the Reformation, the stature of Beverley was much reduced. The ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |