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Usway Burn
The Usway Burn is an upland river on the southern flanks of the Cheviot Hills, in the Northumberland National Park, England. It is a tributary of the River Coquet and is about 15 km in length. It is located close to the northernmost end of the Pennine Way. Course The Usway Burn has several tributaries and inlets, including some in the hills far to the north. Cairn Hill, a 777m subsidiary of The Cheviot, is drained by both Coldwell Strand and Shedding Sike, the Usway Burn's northernmost tributaries. Further south, the longer Davidson's Burn and Tod Sike join the Usway Burn from the western side, with sources very close to Scotland. Davidson's Linn waterfall was praised by the 20th-century travel writers F.R. Banks and Dippie Dixon. The Clay Burn is an eastern tributary, which drains from streams on the edge of Bloodybush Edge hill (610m). Uswayford is the northernmost settlement on the Usway Burn, by the hill Hazely Law (499m). Uswayford contains a farm and former quar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
United Kingdom
The United Kingdom of Great Britain and Northern Ireland, commonly known as the United Kingdom (UK) or Britain, is a country in Europe, off the north-western coast of the continental mainland. It comprises England, Scotland, Wales and Northern Ireland. The United Kingdom includes the island of Great Britain, the north-eastern part of the island of Ireland, and many smaller islands within the British Isles. Northern Ireland shares a land border with the Republic of Ireland; otherwise, the United Kingdom is surrounded by the Atlantic Ocean, the North Sea, the English Channel, the Celtic Sea and the Irish Sea. The total area of the United Kingdom is , with an estimated 2020 population of more than 67 million people. The United Kingdom has evolved from a series of annexations, unions and separations of constituent countries over several hundred years. The Treaty of Union between the Kingdom of England (which included Wales, annexed in 1542) and the Kingdom of Scotland in 170 ... [...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] |
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 National Park
Northumberland National Park is the northernmost national park in England. It covers an area of more than between the Scottish border in the north to just south of Hadrian's Wall, and it is one of least visited of the National Parks. The park lies entirely within Northumberland, covering about a quarter of the county. The park covers several distinct areas. In the north are the Cheviot Hills, a range of hills that mark the border between England and Scotland. Further south, the hills give way to areas of rolling moorland, some of which have been covered by forestry plantations to form Kielder Forest. The southernmost part of the park covers the dramatic central section of Hadrian's Wall, dating from the Roman occupation. The 10,000-year history of human habitation of the region is explored through the many archaeological sites, ranging from prehistoric monuments and Roman remains to Pele towers, constructed as a defence against invading Scots and Border Reivers. The Park's ... [...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] |
Pennine Way
The Pennine Way is a National Trail in England, with a small section in Scotland. The trail stretches for from Edale, in the northern Derbyshire Peak District, north through the Yorkshire Dales and Northumberland National Park and ends at Kirk Yetholm, just inside the Anglo-Scottish border, Scottish border. The path runs along the Pennines, Pennine hills, sometimes described as the "backbone of England". Although not the United Kingdom's longest National Trail (this distinction belongs to the South West Coast Path), it is according to The Ramblers "one of Britain's best known and toughest". History The path was the idea of the journalist and rambler Tom Stephenson (activist), Tom Stephenson, inspired by similar trails in the United States of America, particularly the Appalachian Trail. Stephenson proposed the concept in an article for the ''Daily Herald (UK newspaper), Daily Herald'' in 1935, and lobbied Parliament for the creation of an official trail. The walk was planned ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cairn Hill, Northumberland
A cairn is a man-made pile (or stack) of stones raised for a purpose, usually as a marker or as a burial mound. The word ''cairn'' comes from the gd, càrn (plural ). Cairns have been and are used for a broad variety of purposes. In prehistoric times, they were raised as markers, as memorials and as burial monuments (some of which contained chambers). In modern times, cairns are often raised as landmarks, especially to mark the summits of mountains. Cairns are also used as trail markers. They vary in size from small stone markers to entire artificial hills, and in complexity from loose conical rock piles to elaborate megalithic structures. Cairns may be painted or otherwise decorated, whether for increased visibility or for religious reasons. A variant is the inuksuk (plural inuksuit), used by the Inuit and other peoples of the Arctic region of North America. History Europe The building of cairns for various purposes goes back into prehistory in Eurasia, ranging in s ... [...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] |
Anglo-Scottish Border
The Anglo-Scottish border () is a border separating Scotland and England which runs for 96 miles (154 km) between Marshall Meadows Bay on the east coast and the Solway Firth in the west. The surrounding area is sometimes referred to as "the Borderlands". The Firth of Forth was the border between the Picts, Picto-Gaels, Gaelic Kingdom of Alba and the Angles, Anglian Kingdom of Northumbria in the early 10th century. It became the first Anglo-Scottish border with the History of Anglo-Saxon England#English unification (10th century), annexation of Northumbria by Anglo-Saxon England in the mid-10th century. In 973, Kenneth II of Scotland, Kenneth, King of Scots attended the English king, Edgar the Peaceful, at King Edgar's council at Chester, his council in Chester. After Kenneth had reportedly done homage, Edgar rewarded Kenneth by granting him Lothian. Despite this transaction, the control of Lothian#Lothian under the control of the Angles, Lothian was not finally settle ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bed And Breakfast
Bed and breakfast (typically shortened to B&B or BnB) is a small lodging establishment that offers overnight accommodation and breakfast. Bed and breakfasts are often private family homes and typically have between four and eleven rooms, with six being the average. In addition, a B&B usually has the hosts living in the house. ''Bed and breakfast'' is also used to describe the level of catering included in a hotel's room prices, as opposed to room only, half-board or full-board. International differences China In China, expatriates have remodelled traditional structures in quiet picturesque rural areas and opened a few rustic boutique hotels with minimum amenities. Most patrons are foreign tourists but they are growing in popularity among Chinese domestic tourists. India In India, the government is promoting the concept of bed & breakfast. The government is doing this to increase tourism, especially keeping in view of the demand for hotels during the 2010 Commonwealth Games ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Alwin
The River Alwin is a short, steep upland river that drains the Kidland Forest on the southern flanks of the Cheviot Hills, in the Northumberland National Park, England. It is a tributary of the River Coquet and in length. Course Rising as the Outer Sike at the edge of the Kidland Forest between the peaks of Yarnspath Law and Bloodybush edge. It flows south through the forest gaining various burns and cloughs, to become the White Burn, until it reaches the confluence of the Yoke Burn, where it forms the River Alwin to the north of Kidlandlee. From this point the river flows south to collect the Allerhope Burn at the edge of the forest, continuing through a steep sided valley before reaching Clennell Hall. It then passes to the south of Alwinton, finally reaching the hamlet of Low Alwinton where it joins the Coquet. Hydrology Between 1969 and 1983 the flow of the Alwin, was measured in its lower reaches at a weir near Clennel. The fourteen year record shows that the catchment o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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