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Northumberland (other)
Northumberland ( ) is a ceremonial county in North East England, bordering Scotland. It is bordered by the Scottish Borders to the north, the North Sea to the east, Tyne and Wear and County Durham to the south, and Cumbria to the west. The town of Blyth is the largest settlement. The county has an area of and a population of 320,274, making it the least-densely populated county in England. The south-east contains the largest towns: Blyth (37,339), Cramlington (27,683), Ashington (27,670), and Morpeth (14,304), which is the administrative centre. The remainder of the county is rural, and the largest towns are Berwick-upon-Tweed (12,043) in the far north and Hexham (13,097) in the west. For local government purposes the county is a unitary authority area. The county historically included the parts of Tyne and Wear north of the River Tyne. The west of Northumberland contains part of the Cheviot Hills and North Pennines, while to the east the land becomes flatter befor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bamburgh Castle
Bamburgh Castle is a castle on the northeast coast of England, by the village of Bamburgh in Northumberland. It is a Grade I listed building. The site was originally the location of a Celtic Brittonic fort known as ''Din Guarie'' and may have been the capital of the kingdom of Bernicia from its foundation in 420 to 547. In that latter year, it was captured by King Ida of Bernicia. After passing between the Britons and the Anglo-Saxons three times, the fort came under Anglo-Saxon control in 590. The fort was destroyed by Vikings in 993, and the Normans later built a new castle on the site, which forms the core of the present one. After a revolt in 1095 supported by the castle's owner, it became the property of the English monarch. In the 17th century, financial difficulties led to the castle deteriorating, but it was restored by various owners during the 18th and 19th centuries. It was finally bought by the Victorian era industrialist William Armstrong, who completed its resto ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tyne And Wear
Tyne and Wear () is a metropolitan county in North East England, situated around the mouths of the rivers Tyne and Wear. It was created in 1974, by the Local Government Act 1972, along with five metropolitan boroughs of Gateshead, Newcastle upon Tyne, Sunderland, North Tyneside and South Tyneside. It is bordered by Northumberland to the north and Durham to the south; the county boundary was formerly split between these counties with the border as the River Tyne. The former county council was based at Sandyford House. There is no longer county level local governance following the county council disbanding in 1986, by the Local Government Act 1985, with the metropolitan boroughs functioning separately. The county still exists as a metropolitan county and ceremonial purposes, as a geographic frame of reference. There are two combined authorities covering parts of the county area, North of Tyne and North East. History In the late 600s and into the 700s Saint Bede lived ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Coquet
The River Coquet runs through the county of Northumberland, England, discharging into the North Sea on the east coast at Amble. It rises in the Cheviot Hills on the border between England and Scotland, and follows a winding course across the landscape ("Coquetdale"). The upper reaches are bordered by the Otterburn Ranges military training ground, and are crossed by a number of bridges built in the 20th century. It passes a number of small villages and hamlets, and feeds one of the lakes created by extraction of gravel that form the Caistron Nature Reserve, before reaching the town of Rothbury, where it is crossed by a grade II listed bridge. Below the town is Thrum Mill, the restoration of which was featured on Channel 4 television. It loops around Brinkburn Priory, founded in the 1130s for Augustinian Canons, and its associated mill. At Felton it is crossed by two bridges, one dating from the 15th century, and its replacement, built in 1927, both of which are listed structu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Blyth, Northumberland
The River Blyth flows eastwards through southern Northumberland into the North Sea at the town of Blyth. It flows through Plessey Woods Country Park. The River Pont is a tributary. The Blyth is long and the Pont is . The tidal limit of the river is at Bebside. The estuary widens from this point eastwards and with the addition of a burn that enters on the northern side (Sleek Burn), it covers an area of . Ecologists have suggested that a dam on the river at Humford Country Park in Bedlington could be removed to allow for fish migration. The local community have expressed a desire to keep the dam as it is a local beauty spot; they have suggested that a fish passage A fish ladder, also known as a fishway, fish pass, fish steps, or fish cannon is a structure on or around artificial and natural barriers (such as dams, locks and waterfalls) to facilitate diadromous fishes' natural migration as well as movemen ... be built alongside instead. References External links *Brid ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Cheviot
The Cheviot () is an extinct volcano and the highest summit in the Cheviot Hills and in the county of Northumberland. Located in the extreme north of England, it is a walk from the Scottish border and, with a height of above sea-level, is located on the northernmost few miles of the Pennine Way, before the descent into Kirk Yetholm. The Cheviot was formed when melting in the crust over 390 million years ago gave rise to volcanic activity, and it has subsequently sustained intense erosion. Several watercourses radiate from The Cheviot. How this tranquil part of the North East is far from the madding crowd . Chronicle Live. Retrieved November 28, 2021. Etymology The name ''Cheviot'', which was first documented in 1181 as ''Chiuiet'', is probably of[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North Pennines
The North Pennines is the northernmost section of the Pennine range of hills which runs north–south through northern England. It lies between Carlisle to the west and Darlington to the east. It is bounded to the north by the Tyne Valley and to the south by the Stainmore Gap. Overview The North Pennines was designated as an Area of Outstanding Natural Beauty (AONB) in 1988 for its moorland scenery, the product of centuries of farming and lead-mining, and is also a UNESCO Global Geopark. At almost , it is the second largest of the 49 AONBs in the United Kingdom. The landscape of the North Pennines AONB is one of open heather moors between deep dales, upland rivers, hay meadows and stone-built villages, some of which contain the legacies of a mining and industrial past. The area has previously been mined and quarried for minerals such as barytes, coal fluorspar, iron, lead, witherite and zinc. Natural England maps Maps for North Pennines – Area of Outstanding Natural Beauty, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cheviot Hills
The Cheviot Hills (), or sometimes The Cheviots, are a range of uplands straddling the Anglo-Scottish border between Northumberland and the Scottish Borders. The English section is within the Northumberland National Park. The range includes The Cheviot (the highest hill), plus Hedgehope Hill to the east, Windy Gyle to the west, and Cushat Law and Bloodybush Edge to the south. The hills are sometimes considered a part of the Southern Uplands of Scotland as they adjoin the uplands to the north. Since the Pennine Way runs through the region, the hills are also considered a part of the northern Pennines although they are separated from the Cheviot Hills by the Tyne Gap, part of which lies within the southern extent of the Northumberland National Park. The Cheviot Hills are primarily associated with geological activity from approximately 480 to 360 million years ago, when the continents of Avalonia and Laurentia collided, resulting in extensive volcanic activity (the Caledonian o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Tyne
The River Tyne is a river in North East England. Its length (excluding tributaries) is . It is formed by the North Tyne and the South Tyne, which converge at Warden Rock near Hexham in Northumberland at a place dubbed 'The Meeting of the Waters'. The Tyne Rivers Trust measure the whole Tyne catchment as , containing of waterways. Course North Tyne The North Tyne rises on the Scottish border, north of Kielder Water. It flows through Kielder Forest, and in and out of the border. It then passes through the village of Bellingham before reaching Hexham. South Tyne The South Tyne rises on Alston Moor, Cumbria and flows through the towns of Haltwhistle and Haydon Bridge, in a valley often called the Tyne Gap. Hadrian's Wall lies to the north of the Tyne Gap. Coincidentally, the source of the South Tyne is very close to those of the Tees and the Wear. The South Tyne Valley falls within the North Pennines Area of Outstanding Natural Beauty (AONB) – the second largest of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Unitary Authorities Of England
The unitary authorities of England are those local authorities which are responsible for the provision of all local government services within a district. They are constituted under the Local Government Act 1992, which amended the Local Government Act 1972 to allow the existence of counties that do not have multiple districts. They typically allow large towns to have separate local authorities from the less urbanised parts of their counties and originally provided a single authority for small counties where division into districts would be impractical. However, the UK government has more recently proposed the formation of much larger unitary authorities, including a single authority for North Yorkshire, the largest non-metropolitan county in England, at present divided into seven districts. Unitary authorities do not cover all of England. Most were established during the 1990s, though further tranches were created in 2009 and 2019–21. Unitary authorities have the powers and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hexham
Hexham ( ) is a market town and civil parishes in England, civil parish in Northumberland, England, on the south bank of the River Tyne, formed by the confluence of the North Tyne and the South Tyne at Warden, Northumberland, Warden nearby, and close to Hadrian's Wall. Hexham was the administrative centre for the Tynedale district from 1974 to 2009. In 2011, it had a population of 13,097. Smaller towns and villages around Hexham include Corbridge, Riding Mill, Stocksfield and Wylam to the east, Acomb, Northumberland, Acomb and Bellingham, Northumberland, Bellingham to the north, Allendale, Northumberland, Allendale to the south and Haydon Bridge, Bardon Mill and Haltwhistle to the west. Newcastle upon Tyne is to the east and Carlisle to the west. History Hexham Abbey originated as a monastery founded by Wilfrid in 674. The crypt of the original monastery survives, and incorporates many stones taken from nearby Roman ruins, probably Coria (Corbridge), Corbridge or Hadrian's ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Berwick-upon-Tweed
Berwick-upon-Tweed (), sometimes known as Berwick-on-Tweed or simply Berwick, is a town and civil parish in Northumberland, England, south of the Anglo-Scottish border, and the northernmost town in England. The 2011 United Kingdom census recorded Berwick's population as 12,043. The town is at the mouth of the River Tweed on the east coast, south east of Edinburgh, north of Newcastle upon Tyne, and north of London. Uniquely for England, the town is slightly further north than Denmark's capital Copenhagen and the southern tip of Sweden further east of the North Sea, which Berwick borders. Berwick was founded as an Anglo-Saxon settlement in the Kingdom of Northumbria, which was annexed by England in the 10th century. A civil parish and town council were formed in 2008 comprising the communities of Berwick, Spittal and Tweedmouth. It is the northernmost civil parish in England. The area was for more than 400 years central to historic border wars between the Kingdoms of Engla ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ashington
Ashington is a town and civil parish in Northumberland, England, with a population of 27,864 at the 2011 Census. It was once a centre of the coal mining industry. The town is north of Newcastle upon Tyne, west of the A189 and bordered to the south by the River Wansbeck. The North Sea coast at Newbiggin-by-the-Sea is away. Many inhabitants have a distinctive accent and dialect known as Pitmatic. This varies from the regional dialect known as Geordie. History Toponymy The name Ashington comes from the earlier form Essendene, which has been referenced since 1170. This may have originated from a given name ''Æsc'', not unknown among Saxon invaders who sailed from Northern Germany. If so he came to the Wansbeck and would have settled in this deep wooded valley near Sheepwash. The "de" in the early orthographies more strongly suggests dene, so ash dene - these trees would have lined it. In the 1700s all that existed of Ashington was a small farm with a few dwellings ar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
