|
Cheviot Fringe
Cheviot Fringe ( ) is a geographical region and a Natural England designated National Character Area (or NCA) located in the county Northumberland in northern England. The region consists of the undulating lowlands between the Cheviot Hills and the Northumberland Sandstone Hills NCA. Three major rivers flow through the region, it is bounded on the north by the River Tweed and on the south by the River Coquet and the River Till, Northumberland, River Till flows through the middle. Description The Cheviot Fringe make up the foothills of the Cheviot Hills, and so, the region is more populous as, unlike The Cheviots, the region does not sit in the Northumberland National Park. The A697 is the only major road going through the region, with Wooler being its largest town. Like Northumbria in general, Cheviot Fringe is relatively dispersed in settlement and has a strong tradition of farming and shepherding. The northern part of the region is more arable versus the south, where sheep rais ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wooler
Wooler ( ) is a small town in Northumberland, England. It lies on the edge of the Northumberland National Park, near the Cheviot Hills. It is a popular base for walkers and is referred to as the "Gateway to the Cheviots". As well as many shops and pubs, the town has a youth hostel, many hotels, and campsites. It lies on the St. Cuthbert's Way long-distance footpath between Melrose Abbey and Lindisfarne. The main A697 links the town with Morpeth and Coldstream on the Scottish Border. Wooler has two schools; Wooler First School (including Little Acorns Nursery) and Glendale Community Middle School. The schools and nursery share a single campus on Brewery Road (from September 2015) providing education for children in the Glendale area from 2 years old to 13 years old. Close by to the west is Yeavering Bell, crowned by a large Iron Age fort, a stronghold of the Votadini. The remnants of many stone huts can be seen on its summit, which is surrounded by a collapsed stone wall. Hi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cheviots
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 or ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Northumberland
Northumberland () is a county in Northern England, one of two counties in England which border with Scotland. Notable landmarks in the county include Alnwick Castle, Bamburgh Castle, Hadrian's Wall and Hexham Abbey. It is bordered by land on three sides; by the Scottish Borders region to the north, County Durham and Tyne and Wear to the south, and Cumbria to the west. The fourth side is the North Sea, with a stretch of coastline to the east. A predominantly rural county with a landscape of moorland and farmland, a large area is part of Northumberland National Park. The area has been the site of a number of historic battles with Scotland. Name The name of Northumberland is recorded as ''norð hẏmbra land'' in the Anglo-Saxon Chronicle, meaning "the land north of the Humber". The name of the kingdom of ''Northumbria'' derives from the Old English meaning "the people or province north of the Humber", as opposed to the people south of the Humber Estuary. History ... [...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 improved. 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, a constraint that was not placed on its predecessor NDPBs. Its powers inc ... [...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] |
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] |
Northumberland Sandstone Hills
The Northumberland Sandstone Hills are a major natural region in the English county of Northumberland. The hills form distinctive skylines with generally level tops, northwest facing scarps and craggy outcrops offering views to the Cheviots further west. The Northumberland Sandstone Hills lie not far from the coast of Northumberland and the region is listed as National Character Area no. 2 by Natural England, the UK Government's advisor on the natural environment. The region covers an area of , beginning at Kyloe in the north and running in a strip roughly wide and parallel to the coastal plain as far as Alnwick, where it changes direction to head southwest via Thrunton Wood, Rothbury Forest and Harwood Forest to the area of Throckington and the River Rede, passing over the highest peaks in the area, including Tosson Hill () in the Simonside Hills. The region has a range of semi-natural habitats: moorland with heather and rough, acid grassland mosaics on the thin, sandy soil ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Tweed
The River Tweed, or Tweed Water ( gd, Abhainn Thuaidh, sco, Watter o Tweid, cy, Tuedd), is a river long that flows east across the Border region in Scotland and northern England. Tweed cloth derives its name from its association with the River Tweed. The Tweed is one of the great salmon rivers of Britain and the only river in England where an Environment Agency rod licence is not required for angling. The river generates a large income for the local borders region, attracting anglers from all around the world. Etymology ''Tweed'' may represent an Old Brittonic name meaning "border". A doubtful proposal is that the name is derived from a non-Celtic form of the Indo-European root ''*teuha-'' meaning "swell, grow powerful". Course The River Tweed flows primarily through the scenic Borders region of Scotland. Eastwards from the settlements on opposing banks of Birgham and Carham it forms the historic boundary between Scotland and England. It rises in the Lowther Hills at ... [...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 Till, Northumberland
The River Till is a river of north-eastern Northumberland. It is a tributary of the River Tweed, of which it is the only major tributary to flow wholly in England. Upstream of the locality of Bewick Bridge, 8.5 km to the southeast of Wooler the river is known as the Breamish, River Breamish. It rises on Comb Fell in the Cheviot Hills. Its tributaries include Wooler Water, which originates in the Cheviots, and the River Glen, Northumberland, River Glen in Glendale, Northumberland, Glendale. It meets the Tweed a mile to the west of Twizell Bridge, 4 km downstream of Coldstream. According to local folklore: ::::''Tweed said to Till'' ::::"What gars ye rin sae stil?" ::::Says Till to Tweed, ::::"Though ye rin wi' speed ::::And I rin slaw ::::Whar ye droon yin man ::::I droon twa"'' Recent environmental projects have included an attempt to conserve the native brown trout. References External links A walk along the River Till bank from Etal to Tiptoe* Map sources f ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Cheviots
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 oro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
