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River Burn, North Yorkshire
The River Burn is a river that flows wholly within North Yorkshire, England. The river starts as several small streams on Masham Moor and drains Colsterdale flowing eastwards before emptying into the River Ure just south of Masham. Conservation work on removing a weir, and introducing fish to the river in 2016, has meant that salmon have been recorded spawning in the river for the first time in over 100 years. Whilst the River Burn valley is not in Nidderdale, almost all of it is included in the Nidderdale Area of Outstanding Natural Beauty. History During the Ice Age, a glacier forced water to build up in what are now the valleys that hold the Pott Beck and the River Burn. This created large lakes that deposited minerals such as limestone and chert. The river flows over several types of bedrock (limestone, sandstone, mudstone and shale) which is covered by gravel and silty clay which is a result of riverine alluvia. When tested in the 1990s, this alluvia was found to be the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Masham
Masham ( ) is a market town and civil parish in the Harrogate district of North Yorkshire, England. It had a population of 1,205 at the 2011 census. Etymology In Wensleydale, on the western bank of the River Ure, the name derives from the Anglo-Saxon "Mæssa's Ham", the homestead belonging to Mæssa. History The Romans had a presence here, but the first permanent settlers were the Angles. Around 900 AD the Vikings invaded, burning and laying waste to the church. They also introduced sheep farming, for which the town is still known. Masham was historically a large parish in the North Riding of Yorkshire. As well as the town of Masham the parish included the townships of Burton-on-Yore, Ellingstring, Ellington High and Low, Fearby, Healey with Sutton, Ilton cum Pott and Swinton. In 1866 the townships became separate civil parishes. Masham Moor was an area of moorland to the west of the parish bordering the West Riding, common to the parishes of Masham and East Witton. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Bain, North Yorkshire
The River Bain is a river in North Yorkshire, England. As a tributary of the River Ure, it is one of the shortest, named rivers in England. The river is home to the small scale hydroelectricity project River Bain Hydro located at Bainbridge. Course The river leaves the second-largest natural lake in North Yorkshire, Semerwater, in a north-east direction past the hamlet of Countersett. After a couple of gentle meanders it runs through woodland before slowly turning northward. It passes under the A684 road in Bainbridge and joins the River Ure The River Ure in North Yorkshire, England is approximately long from its source to the point where it becomes the River Ouse. It is the principal river of Wensleydale, which is the only major dale now named after a village rather than its r ... to the east of Yore Bridge opposite the mouth of Grange Beck. Images File:River Bain - geograph.org.uk - 346172.jpg, River Bain leaving Semerwater Sources *Ordnance Survey Open ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Swinton Estate
The Swinton Estate is a large privately owned estate in North Yorkshire, England. It comprises some of countryside in the Nidderdale Area of Outstanding Natural Beauty, extending west from the River Ure near Masham. The estate includes Swinton Park, the seat of the Danby family and (from 1882) of the Cunliffe-Lister family (the Earls of Swinton), an English country house in Swinton near Masham. It is set in of parkland, lakes and gardens. The house is a Grade II* listed building, and now operates as the 42-bedroom Swinton Park Hotel. The Cunliffe-Lister family still own the house but the seat of the Earl of Swinton is now at Dykes Hill House, also located near Masham. Beyond the parkland surrounding the house, the estate comprises farmland and large areas of grouse moor in and around the valley of the River Burn. History The construction at Swinton Park was commenced in 1695 by Sir Abstrupus Danby (1655-1727). His successors built the stable block and gatehouse and, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Grewelthorpe
Grewelthorpe is a village and civil parish in the Harrogate district of North Yorkshire, England situated south of Masham and north of Ripon. It is located in the Nidderdale area of outstanding natural beauty. The name Grewelthorpe derives from the words Gruel and Thorpe, Gruel being a family name and thorpe meaning "outlying farmstead". Grewelthorpe was mentioned in the ''Domesday Book'' when it was known as Torp and was in the ownership of Gospatric. In 2009 Grewelthorpe has one active church, St James's and a pub, the Crown. It also has a duck pond, which is a distinctive feature of the village, it is populated by ducks which people come from surrounding villages to feed. The local primary school is known as Grewelthorpe Church of England Primary school and takes children from two years old to eleven years old. The current school building was opened in June 2003 and is located at cross hills in Grewelthorpe. However, Grewelthorpe has had a school since 1876. Unlike many ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Grade II Listed
In the United Kingdom, a listed building or listed structure is one that has been placed on one of the four statutory lists maintained by Historic England in England, Historic Environment Scotland in Scotland, in Wales, and the Northern Ireland Environment Agency in Northern Ireland. The term has also been used in the Republic of Ireland, where buildings are protected under the Planning and Development Act 2000. The statutory term in Ireland is " protected structure". A listed building may not be demolished, extended, or altered without special permission from the local planning authority, which typically consults the relevant central government agency, particularly for significant alterations to the more notable listed buildings. In England and Wales, a national amenity society must be notified of any work to a listed building which involves any element of demolition. Exemption from secular listed building control is provided for some buildings in current use for worship, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Roundhill Reservoir
Roundhill Reservoir is situated near Leighton Reservoir in North Yorkshire, England. It was constructed by Harrogate Corporation early in the 20th century. Water from the reservoir is fed into Yorkshire Water's grid. Roundhill reservoir is overlooked by a strange stone tower. This is Carlesmoor sighting tower used to triangulate the end points of a water tunnel from the reservoir to Harrogate. It is one of several Colsterdale towers. Although not in Nidderdale, the reservoir is within the Nidderdale Area of Outstanding Natural Beauty. History Roundhill Reservoir was built for Harrogate Corporation. It was completed in 1913, at a cost of £500,000. In 1908, while Roundhill was being constructed, Leeds Corporation began building Leighton Reservoir Leighton Reservoir is a reservoir which drains via the River Burn to the River Ure in North Yorkshire, England. It neighbours Roundhill Reservoir and is about west of Masham. It takes its name from the nearby village of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Leighton Reservoir
Leighton Reservoir is a reservoir which drains via the River Burn to the River Ure in North Yorkshire, England. It neighbours Roundhill Reservoir and is about west of Masham. It takes its name from the nearby village of Leighton. Work on the reservoir was started by the Leeds Corporation in 1908, and although the major parts of the building process were over by March 1926, the final cementation was not completed until 1941. The reservoir was allowed to fill with water over the winter of 1926–1927. A newspaper report from 1910, estimated that the final cost of the construction would be £437,000 (). Although the Leeds Corporation intended to build another reservoir in Colsterdale on the River Burn, this never came to pass, and Leighton Reservoir was constructed on two tributaries of the Burn; Pott Beck and Spruce Gell. Water from the reservoir is used to compensate for abstraction from the River Ure. Although not in Nidderdale, the reservoir is within the Nidderdale Area o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Leighton, North Yorkshire
Leighton is a hamlet in the civil parish of Healey in the Harrogate district of North Yorkshire, England. It is near Leighton Reservoir that provides for Yorkshire Water. Notable residents The religious prophet In religion, a prophet or prophetess is an individual who is regarded as being in contact with a divine being and is said to speak on behalf of that being, serving as an intermediary with humanity by delivering messages or teachings from the s ... Martha Hatfield was from Leighton. References External links Villages in North Yorkshire {{harrogate-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
SSSI
A Site of Special Scientific Interest (SSSI) in Great Britain or an Area of Special Scientific Interest (ASSI) in the Isle of Man and Northern Ireland is a conservation designation denoting a protected area in the United Kingdom and Isle of Man. SSSI/ASSIs are the basic building block of site-based nature conservation legislation and most other legal nature/geological conservation designations in the United Kingdom are based upon them, including national nature reserves, Ramsar sites, Special Protection Areas, and Special Areas of Conservation. The acronym "SSSI" is often pronounced "triple-S I". Selection and conservation Sites notified for their biological interest are known as Biological SSSIs (or ASSIs), and those notified for geological or physiographic interest are Geological SSSIs (or ASSIs). Sites may be divided into management units, with some areas including units that are noted for both biological and geological interest. Biological Biological SSSI/ASSIs may b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
V-shaped Valley
A valley is an elongated low area often running between Hill, hills or Mountain, mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacier, glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glaciation, glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In karst, areas of limestone bedrock, dry valleys may also result from drainage now taking place cave, underground rather than at the surface. Rift valleys arise principally from tectonics, earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coverdale (dale)
Coverdale is a dale in the far east of the Yorkshire Dales, North Yorkshire, England. It takes its name from the River Cover, a tributary of the River Ure. The dale runs south-west from the eastern end of Wensleydale to the dale head at a pass, known as Park Rash Pass, between Great Whernside to the south and Buckden Pike to the north. It is accessible by a single track road, which runs the length of the dale and over the pass to Kettlewell in Wharfedale. The name is taken from that of the River Cover, which is of Brittonic origin. Ekwall suggested that it might mean "hollow stream", but more recently Andrew Breeze has argued that it is cognate with Welsh ''gofer'' "streamlet". History An abbey was founded at Coverham in the 14th century by Ralph, son of Robert, Lord of Middleham. The order that it belonged to was Premonstratensian (or White Canons) and was formally dissolved in 1536. Whilst some of the ruins are still extant, it is not open to the general public. In the 1 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Tutt
The River Tutt is a long tributary of the River Ure in North Yorkshire, England. The river rises near to the villages of Nidd and Scotton, Harrogate, Scotton draining mainly arable land north eastwards before emptying into the Ure at Boroughbridge. Where the river joins the Ure in Boroughbridge, has been the site of significant historic flooding. An Environment Agency project to alleviate flooding on the river has seen diversion schemes and pumps added to prevent this. Toponymy The river is known as the Tutt for only about of its length, and is variously known as Jumwell, Shaw and Occaney Beck in its early stages. It is also known as Tutt Beck, Fleet Beck and Minskip Beck. The derivation of the name ''Tutt'' for the river has many explanations; one theory is that it is from a Viking word, another states that it comes from the Roman people, Roman goddess Tutelina (mythology), Tutelina, who looked after corn when it was in storage. A H Smith, writing in ''The Place Names of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
