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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] |
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] |
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] |
Windy Gyle
Windy Gyle is a mountain in the Cheviot Hills range, on Anglo-Scottish border, the border between England and Scotland. Like the other hills in the area, it is rounded and grass-covered. It is the highest summit on the border, although not the highest point as the border is higher where it runs along the western shoulder of The Cheviot, at a point called Cairn Hill West Top, or Hangingstone Hill. The cairn at the summit of this hill is named Russell's Cairn and has a small depression suitable for shielding about 15 people from the wind; the border runs directly through the cairn although this can only be seen on the map, the fence which follows it in many places is absent here. The Pennine Way crosses the summit, thus providing one possible route of ascent. Windy Gyle may also be climbed from the River Coquet, Coquet valley to the south (England), or from Cocklawfoot to the north (Scotland). There are good views from the summit north towards the Scottish Borders, Eildon Hills and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kielder Forest
Kielder Forest is a large forestry plantation in Northumberland, England, surrounding Kielder village and the Kielder Water reservoir. It is the largest man-made woodland in England with three-quarters of its covered by forest. The majority of the forest lies within Kielder Water and Forest Park, with the southern tip known as Wark Forest lying within Northumberland National Park. The forest is next to the England - Scotland border. History The forest is owned and managed by Forestry England, which initiated the first plantings in the 1920s. During the 1930s, the Ministry of Labour supplied men from among the ranks of the unemployed. Many came from the mining communities and shipyards of North East England. They were housed in one of a number of instructional centres created by the Ministry, most of them on Forestry England property; by 1938, the Ministry had 38 Instructional Centres across Britain. The hutted camp in Kielder is now under Kielder Water. Numerous purpose-b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shillhope Law
Shillhope Law is a hill in the southern Cheviots, a range of hills in Northumberland, England. Shillhope Law is a relatively unremarkable member of this group; in common with its neighbours it has a small summit and steep, grassy sides falling to deeply incised valleys on either side. However, unlike its neighbours, the ridge connecting Shillhope Law to the higher dome of The Cheviot to the north is bisected by a low col at m, giving it enough relative height to be a Marilyn. The narrow road that climbs up Coquetdale from Alwinton to the foot of Shillhope Law eases any access problems. On the other side of the valley lies the Otterburn Training Area and training (without live ammunition) can take place on the northern side of Shillhope Law. Shillhope Law can be easily climbed from the farms on its western side, Barrowburn and Shillmoor, although the ascent is steep. These two climbs can be combined to give a circular walk of about . The view is not far-reaching in any directi ... [...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] |
Breamish Valley Cheviot Hills - Geograph
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] |
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] |
Pennines
The Pennines (), also known as the Pennine Chain or Pennine Hills, are a range of uplands running between three regions of Northern England: North West England on the west, North East England and Yorkshire and the Humber on the east. Commonly described as the "backbone of England", the range stretches northwards from the Peak District at the southern end, through the South Pennines, Yorkshire Dales and North Pennines to the Tyne Gap, which separates the range from the Border Moors and Cheviot Hills across the Anglo-Scottish border, although some definitions include them. South of the Aire Gap is a western spur into east Lancashire, comprising the Rossendale Fells, West Pennine Moors and the Bowland Fells in North Lancashire. The Howgill Fells and Orton Fells in Cumbria are sometimes considered to be Pennine spurs to the west of the range. The Pennines are an important water catchment area with numerous reservoirs in the head streams of the river valleys. The North Pennin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Topographic Prominence
In topography, prominence (also referred to as autonomous height, relative height, and shoulder drop in US English, and drop or relative height in British English) measures the height of a mountain or hill's summit relative to the lowest contour line encircling it but containing no higher summit within it. It is a measure of the independence of a summit. A peak's ''key col'' (the highest col surrounding the peak) is a unique point on this contour line and the ''parent peak'' is some higher mountain, selected according to various criteria. Definitions The prominence of a peak may be defined as the least drop in height necessary in order to get from the summit to any higher terrain. This can be calculated for a given peak in the following way: for every path connecting the peak to higher terrain, find the lowest point on the path; the ''key col'' (or ''key Saddle point, saddle'', or ''linking col'', or ''link'') is defined as the highest of these points, along all connecting pat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Housedon Hill
Housedon Hill is a hill on the northwestern edge of the Cheviot Hills in Northumberland, England. It is the northernmost Marilyn in England, the summit lying only about 4 miles (7 km) from the Scottish border, which runs to the north and west. The hill lies just outside the boundary of the Northumberland National Park. Until recently there was no legal right of access to the hill. This has now changed, as the western side of the hill up to the summit is designated ‘access land’ under the terms of the Countryside and Rights of Way Act 2000. The simplest route of ascent starts from Housedonhaugh on the southwest flank of the hill, utilising the new access rights. The northwestern side of the Housedon Hill is cloaked in forestry Forestry is the science and craft of creating, managing, planting, using, conserving and repairing forests, woodlands, and associated resources for human and environmental benefits. Forestry is practiced in plantations and natural stands ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Los Angeles
Los Angeles ( ; es, Los Ángeles, link=no , ), often referred to by its initials L.A., is the largest city in the state of California and the second most populous city in the United States after New York City, as well as one of the world's most populous megacities. Los Angeles is the commercial, financial, and cultural center of Southern California. With a population of roughly 3.9 million residents within the city limits , Los Angeles is known for its Mediterranean climate, ethnic and cultural diversity, being the home of the Hollywood film industry, and its sprawling metropolitan area. The city of Los Angeles lies in a basin in Southern California adjacent to the Pacific Ocean in the west and extending through the Santa Monica Mountains and north into the San Fernando Valley, with the city bordering the San Gabriel Valley to it's east. It covers about , and is the county seat of Los Angeles County, which is the most populous county in the United States with an estim ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
