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Hedgehope Hill
Hedgehope Hill is a mountain in the Cheviot Hills of north Northumberland in northeast England, and categorised as a Hewitt. At a height of and a distance of about from the Scottish border, it is best climbed from Langleeford in the Harthope Valley, over which it looms. The Harthope valley is accessible by a minor road from near Wooler to the northeast. A slightly gentler climb, though a longer distance, is from Linhope in the Breamish valley, approaching from the south east. An alternative route to the summit could involve a long day's climb of both 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 lo ... and Hedgehope Hill, starting and finishing at Langleeford. It is a steep climb from any approach, best reserved for fitter walkers though the steepest inclines are ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hewitt (hill)
This is a list of Hewitt mountains in England, Wales and Ireland by height. Lists of mountains and hills in the British Isles#Hewitts, Hewitts are defined as "Hills in England, Wales and Ireland over two thousand" feet in height, the general requirement to be called a Lists of mountains and hills in the British Isles#Elevation, "mountain" in the British Isles, and with a prominence above ; a mix of imperial measures, imperial and metric system, metric thresholds. The Hewitt classification was suggested by Alan Dawson in his 1992 book, "The Relative Hills of Britain". Dawson originally called his Hewitts "Sweats", from "Summits - Wales and England Above Two thousand", before settling on the label Hewitt. In a series of three booklets edited by Dave Hewitt, the list of English Hewitts was published in 1997, and the list of Welsh Hewitts was also published in 1997, and the list of Irish Hewitts was published in 1998. Hewitts were designed to address one of the criticisms of ... [...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
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] |
Ordnance Survey
, nativename_a = , nativename_r = , logo = Ordnance Survey 2015 Logo.svg , logo_width = 240px , logo_caption = , seal = , seal_width = , seal_caption = , picture = , picture_width = , picture_caption = , formed = , preceding1 = , dissolved = , superseding = , jurisdiction = Great BritainThe Ordnance Survey deals only with maps of Great Britain, and, to an extent, the Isle of Man, but not Northern Ireland, which has its own, separate government agency, the Ordnance Survey of Northern Ireland. , headquarters = Southampton, England, UK , region_code = GB , coordinates = , employees = 1,244 , budget = , minister1_name = , minister1_pfo = , chief1_name = Steve Blair , chief1_position = CEO , agency_type = , parent_agency = , child1_agency = , keydocument1 = , website = , footnotes = , map = , map_width = , map_caption = Ordnance Survey (OS) is the national mapping agency for Great Britain. The agency's name indicates its original military purpose (se ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited Summit (topography), summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosys ... [...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] |
Scotland
Scotland (, ) is a country that is part of the United Kingdom. Covering the northern third of the island of Great Britain, mainland Scotland has a border with England to the southeast and is otherwise surrounded by the Atlantic Ocean to the north and west, the North Sea to the northeast and east, and the Irish Sea to the south. It also contains more than 790 islands, principally in the archipelagos of the Hebrides and the Northern Isles. Most of the population, including the capital Edinburgh, is concentrated in the Central Belt—the plain between the Scottish Highlands and the Southern Uplands—in the Scottish Lowlands. Scotland is divided into 32 administrative subdivisions or local authorities, known as council areas. Glasgow City is the largest council area in terms of population, with Highland being the largest in terms of area. Limited self-governing power, covering matters such as education, social services and roads and transportation, is devolved from the Scott ... [...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] |
Linhope
Linhope is a small village in Northumberland, England. It is located in the Cheviots on the River Breamish, and within 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 .... Linhope Spout, a waterfall that falls into a 16 ft plunge pool, is located on the Linhope Burn, a tributary of the Breamish, 1 km north of the village. References External links GENUKI(Accessed: 20 November 2008) {{authority control Villages in Northumberland Ingram, Northumberland ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Breamish
The Breamish is a river in Northumberland, England, which rises on Comb Fell in the Northumberland National Park on the southern side of The Cheviot. It is one of the eight rivers rising in the Cheviot Hills, the others being the College Valley, the Harthope Burn, the Bowmont Water, the Kale Water, the Heatherhope Burn, the Coquet and the Alwin. There are two notable villages in the upper Breamish valley: Ingram and Linhope, both of which are in the Northumberland National Park. The Breamish becomes the River Till in the locality of Bewick Bridge, 8.5 km to the southeast of Wooler; this is the only tributary of the River Tweed that flows exclusively in England. Etymology The name ''Breamish'' is of Brittonic origin and derived from the verbal root ''breμ–''. "bellow, bray, roar" (Welsh ''brefu''). This is the origin of the rivers Braan, Scotland and Brefi, Wales. History The Salters Road runs from the upper Breamish Valley across the Cheviots into Scotland. T ... [...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] |
Blyth, Northumberland
Blyth () is a town and civil parish in southeast Northumberland, England. It lies on the coast, to the south of the River Blyth and is approximately northeast of Newcastle upon Tyne. It has a population of about 37,000, as of 2011. The port of Blyth dates from the 12th century, but the development of the modern town only began in the first quarter of the 18th century. The main industries which helped the town prosper were coal mining and shipbuilding, with the salt trade, fishing and the railways also playing an important role. These industries have largely vanished, but the port still thrives, receiving paper and pulp from Scandinavia for the newspaper industries of England and Scotland. The town was seriously affected when its principal industries went into decline, and it has undergone much regeneration since the early 1990s. The Keel Row Shopping Centre, opened in 1991, brought major high street retailers to Blyth, and helped to revitalise the town centre. The market place ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
