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River Derwent, Yorkshire
The Derwent is a river in Yorkshire in the north of England. It flows from Fylingdales Moor in the North York Moors National Park, east then southwards as far as its confluence with the River Hertford then westwards through the Vale of Pickering, south through Kirkham Gorge and the Vale of York, joining the River Ouse at Barmby on the Marsh. The confluence is unusual in that the Derwent converges on the Ouse at a shallow angle in an upstream direction. The river used to flow further east, its old course entering the Ouse east of Howden. The River Derwent catchment area includes the Upper Derwent, River Rye, River Hertford, Bielby Beck and Pocklington Canal and their tributaries. It covers an area of 2,057 square kilometres and includes the towns of Stamford Bridge, Malton, Pickering, Helmsley, Filey and Scarborough. The area is bounded by the Cleveland Hills, North York Moors and Hambleton Hills to the north, the Yorkshire Wolds and the coast to the east, the Vale of Yo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
England
England is a country that is part of the United Kingdom. It shares land borders with Wales to its west and Scotland to its north. The Irish Sea lies northwest and the Celtic Sea to the southwest. It is separated from continental Europe by the North Sea to the east and the English Channel to the south. The country covers five-eighths of the island of Great Britain, which lies in the North Atlantic, and includes over 100 smaller islands, such as the Isles of Scilly and the Isle of Wight. The area now called England was first inhabited by modern humans during the Upper Paleolithic period, but takes its name from the Angles, a Germanic tribe deriving its name from the Anglia peninsula, who settled during the 5th and 6th centuries. England became a unified state in the 10th century and has had a significant cultural and legal impact on the wider world since the Age of Discovery, which began during the 15th century. The English language, the Anglican Church, and Engli ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pickering, North Yorkshire
Pickering is a market town and civil parishes in England, civil parish in the Ryedale district in North Yorkshire, England, on the border of the North York Moors National Park. Historic counties of England, Historically part of the North Riding of Yorkshire, it is at the foot of the moors, overlooking the Vale of Pickering to the south. Pickering Parish Church, with its medieval wall paintings, Pickering Castle, the North Yorkshire Moors Railway and Beck Isle Museum have made Pickering popular with visitors. Nearby places include Malton, North Yorkshire, Malton, Norton-on-Derwent and Scarborough, North Yorkshire, Scarborough. History Positioned on the shores of a glacial lake at the end of the Last Glacial Period, last ice age, Pickering was in an ideal place for early settlers to benefit from the multiple natural resources of the moorlands to the north, the wetlands to the south, running water in the Costa Beck, beck and the forests all around. It had wood, stone, wildfowl, g ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bubwith
Bubwith is a village and civil parish in the East Riding of Yorkshire, England. The village is situated about north-east of Selby, and south-east of York. It is situated on the east bank of the River Derwent, west of which is the Selby District of North Yorkshire. It lies between Selby and Market Weighton on the A163 road. The civil parish is formed by the villages of Bubwith and Breighton and the hamlets of Gunby and Willitoft. According to the 2011 UK census, Bubwith parish had a population of 1,225, an increase on the 2001 UK census figure of 1,104. History The ancient parish of Bubwith also covers the village of Breighton and the hamlets of Gunby and Willitoft, but its location on and crossing over the River Derwent led to its becoming the largest settlement in the area.Information notice board, car park, Bubwith Toll Bridge. The village's name means ''Bubba's wood'', Bubba being a Scandinavian male name. It is listed as "Bobewyth" in the 11th-century accounts of Se ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wheldrake
Wheldrake is a village and civil parish located south-east of York. Administratively it is in the unitary authority of the City of York in North Yorkshire, England. According to the 2001 census the parish had a population of 1,909, increasing to 2,107 at the 2011 Census. The village was historically part of the East Riding of Yorkshire until 1974. It was then a part of the Selby District in North Yorkshire from 1974 until 1996. Since 1996 it has been part of the City of York unitary authority. The parish of Wheldrake covers an area of . It was established before 1066 and after being largely in the possession of Fountains Abbey in the Middle Ages, it became part of a landed estate until the mid 20th century. It has a significant conservation area and a nature reserve of international importance. This, named Wheldrake Ings, is a mile east of the village, and is where many wild flowers flourish and rare birds prosper. Most of the employed people who live in the village commute to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Elvington, City Of York
Elvington is a village and civil parish approximately south-east of York, England, on the B1228 York-Howden road. According to the 2001 census the parish had a population of 1,212, it increased to 1,239 at the 2011 Census. The River Derwent forms part of the parish boundary and the historic Sutton Bridge connects Elvington with Sutton upon Derwent. The village has three separate large industrial estates including a site for Yara International, a Norwegian chemical company. Elvington was in the East Riding of Yorkshire until local government boundary changes in 1974, when it became part of the Selby District in North Yorkshire. In 1996 it became part of the City of York unitary authority. History The village is mentioned in the ''Domesday Book'', which states that in 1086 Ulfketill had six carucates of land taxable, where three ploughs were possible. There is a mention of the church, which is Norman in origin and exists in part today. Richard Neville, 16th Earl of Warwick ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Biochemical Oxygen Demand
Biochemical oxygen demand (BOD) is the amount of dissolved oxygen (DO) needed (i.e. demanded) by aerobic biological organisms to break down organic material present in a given water sample at a certain temperature over a specific time period. The BOD value is most commonly expressed in milligrams of oxygen consumed per litre of sample during 5 days of incubation at 20 °C and is often used as a surrogate of the degree of organic pollution of water. BOD reduction is used as a gauge of the effectiveness of wastewater treatment plants. BOD of wastewater effluents is used to indicate the short-term impact on the oxygen levels of the receiving water. BOD analysis is similar in function to chemical oxygen demand (COD) analysis, in that both measure the amount of organic compounds in water. However, COD analysis is less specific, since it measures everything that can be chemically oxidized, rather than just levels of biologically oxidized organic matter. Background Most natur ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Baron Derwent
Baron Derwent, of Hackness in the North Riding of the County of York, is a title in the Peerage of the United Kingdom. It was created on 10 October 1881 for the former Liberal Member of Parliament for Scarborough, Sir Harcourt Vanden-Bempde-Johnstone, 3rd Baronet. His grandson, the third Baron (who succeeded his uncle the second Baron), was an author, poet and minor diplomat. On his death in 1949 the titles passed to his younger brother, the fourth Baron. He served in the Conservative administrations of Harold Macmillan and Sir Alec Douglas-Home as Minister of State for Trade and Minister of State for Home Affairs. the titles are held by his son, the fifth Baron, who succeeded in 1986. The Baronetcy, of Hackness Hall in the North Riding of the County of York, was created in the Baronetage of Great Britain on 6 July 1795 for Richard Vanden-Bempde-Johnstone, with remainder in default of male issue of his own to the male issue of his brother Charles John. He notably represent ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Viscount FitzAlan Of Derwent
Viscount FitzAlan of Derwent, of Derwent in the County of Derby, was a title in the Peerage of the United Kingdom. It was created in 1921 for Lord Edmund Talbot on his appointment as Lord Lieutenant of Ireland. Born Lord Edmund FitzAlan-Howard, he was the third born, but second surviving son of Henry Fitzalan-Howard, 14th Duke of Norfolk. In 1876 he assumed by Royal licence the surname of Talbot in lieu of his patronymic in an unsuccessful attempt to succeed to the estates of Bertram, 17th Earl of Shrewsbury and Waterford, having been named by will as his successor and chief beneficiary. Shortly after being raised to the peerage he resumed his first surname. The title became extinct on the death of his son, the second Viscount, in 1962. Viscounts FitzAlan of Derwent (1921) * Edmund Bernard FitzAlan-Howard, 1st Viscount FitzAlan of Derwent (1855–1947) * Henry Edmund FitzAlan-Howard, 2nd Viscount FitzAlan of Derwent (1883–1962) See also *Duke of Norfolk *Baron Howard of Gl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Humber Estuary
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 Ouse and 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. Although the Humber is an estuary from the point at which it is formed, many maps show it as the River Humber. 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 Head to the north. Ports on the Humber include the Port of Hull, the Port of Grimsby and the Port ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yorkshire Wolds
The Yorkshire Wolds are low hills in the counties of the East Riding of Yorkshire and North Yorkshire in north-eastern England. The name also applies to the district in which the hills lie. 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 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 slopes, along with the civil parish of Molescroft. Geology The hills are formed from a series of pure marine limestones formed during the Cretaceous period, kno ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hambleton Hills
The Hambleton Hills are a range of hills in North Yorkshire, England. They form the western edge of the North York Moors but are separated from the moors by the valley of the River Rye. They are the eastern boundary of the low-lying Vale of Mowbray which they abut with a precipitous escarpment. They run in a north–south direction for about and merge with the Cleveland Hills in the north and Howardian Hills in the south. The hills are made up of rocks of middle and late Jurassic age with the hard Corallian Limestone forming the cap at the highest points. The highest point is Black Hambleton which rises to 1,308 feet (400 m) at the northern end of the range. Roulston Scar reaches 919 feet (280 m) and Whitestone cliff is 1,063 feet (324 m). The Corallian Limestone also outcrops along the southern edge of the North York Moors forming the Tabular Hills which run from Black Hambleton eastwards to Scarborough, although much broken through by river valleys. In the 12th and 13th& ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cleveland Hills
The Cleveland Hills are a range of hills on the north-west edge of the North York Moors in North Yorkshire, England, overlooking Cleveland and Teesside. They lie entirely within the boundaries of the North York Moors National Park. Part of the long Cleveland Way National Trail runs along the hills, and they are also crossed by a section of Wainwright's Coast to Coast Walk. The hills, which rise abruptly from the flat Tees Valley to the north, include distinctive landmarks such as the cone-shaped peak of Roseberry Topping, near the village of Great Ayton – childhood home of Captain James Cook. Geology The hills are formed by multiple stacked layers of Jurassic age sedimentary rocks. The scarp rises above the low ground to the north and west formed by the mudstones of the Redcar Mudstone Formation, though largely buried beneath glacial till from the last ice age. The same formation also provides the lowermost slopes of the scarp. The full sequence, presented in stratigraph ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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