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Boredale From Hallin Fell
Boredale sometimes known as Boardale, is a valley within Lake District National Park, in Cumbria, England. The valley is close to the eastern shore of Ullswater and lies between the hills of Place Fell to the west and Beda Fell to the east. Boredale runs in a northerly direction for a distance of 4.5 km from its head at Boredale Hause to its convergence with the valley of Martindale. It is a thinly populated valley with the structures of Garth Heads, Howsteadbrow, Nettleslack and Boredale Head being the only inhabited buildings in the valley. The traditional stone and slate Nettleslack cottage dates from 1756, it was modernised in 1997 and is now rented out as holiday accommodation. Internet Cottages.com. Gives details of Nettleslack. There is a narrow |
Boredale From Hallin Fell
Boredale sometimes known as Boardale, is a valley within Lake District National Park, in Cumbria, England. The valley is close to the eastern shore of Ullswater and lies between the hills of Place Fell to the west and Beda Fell to the east. Boredale runs in a northerly direction for a distance of 4.5 km from its head at Boredale Hause to its convergence with the valley of Martindale. It is a thinly populated valley with the structures of Garth Heads, Howsteadbrow, Nettleslack and Boredale Head being the only inhabited buildings in the valley. The traditional stone and slate Nettleslack cottage dates from 1756, it was modernised in 1997 and is now rented out as holiday accommodation. Internet Cottages.com. Gives details of Nettleslack. There is a narrow |
Lake District
The Lake District, also known as the Lakes or Lakeland, is a mountainous region in North West England. A popular holiday destination, it is famous for its lakes, forests, and mountains (or ''fells''), and its associations with William Wordsworth and other Lake Poets and also with Beatrix Potter and John Ruskin. The Lake District National Park was established in 1951 and covers an area of . It was designated a UNESCO World Heritage Site in 2017. The Lake District is today completely within Cumbria, a county and administrative unit created in 1974 by the Local Government Act 1972. However, it was historically divided between three English counties ( Cumberland, Westmorland and Lancashire), sometimes referred to as the Lakes Counties. The three counties met at the Three Shire Stone on Wrynose Pass in the southern fells west of Ambleside. All the land in England higher than above sea level lies within the National Park, including Scafell Pike, the highest mountain in England. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cumbria
Cumbria ( ) is a ceremonial and non-metropolitan county in North West England, bordering Scotland. The county and Cumbria County Council, its local government, came into existence in 1974 after the passage of the Local Government Act 1972. Cumbria's county town is Carlisle, in the north of the county. Other major settlements include Barrow-in-Furness, Kendal, Whitehaven and Workington. The administrative county of Cumbria consists of six districts ( Allerdale, Barrow-in-Furness, Carlisle, Copeland, Eden and South Lakeland) and, in 2019, had a population of 500,012. Cumbria is one of the most sparsely populated counties in England, with 73.4 people per km2 (190/sq mi). On 1 April 2023, the administrative county of Cumbria will be abolished and replaced with two new unitary authorities: Westmorland and Furness (Barrow-in-Furness, Eden, South Lakeland) and Cumberland ( Allerdale, Carlisle, Copeland). Cumbria is the third largest ceremonial county in England by area. It i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ullswater
Ullswater is the second largest lake in the English Lake District, being about long and wide, with a maximum depth a little over . It was scooped out by a glacier in the Last Ice Age. Geography It is a typical Lake District "ribbon lake", formed after the last ice age by a glacier scooping out the valley floor, which then filled with meltwater. Ullswater was formed by three glaciers. Surrounding hills give it the shape of an extenuated "Z" with three segments or reaches winding through them. For much of its length, Ullswater formed the border between the historic counties of Cumberland and Westmorland. Etymology The origin of the name Ullswater is uncertain. Whaley suggests "Ulf's lake", from Old Norse personal name Ulfr plus Middle English water, influenced in usage by the Old Norse ''vatn'' (water or lake). ''Ulfr'' is also the Old Norse noun meaning wolf, and Hutchinson thought that the name might refer to the lake as a resort of wolves, or to its elbow-shaped bend (citi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Place Fell
Place Fell is a hill in the English Lake District. It stands at the corner of the upper and middle reaches of Ullswater, with steep western flanks overlooking the villages of Glenridding and Patterdale. Topography A ten-mile-long horseshoe of high ground surrounds the Martindale catchment, a system of valleys draining northward into Ullswater. Place Fell is at the western terminus of this ridge. To the south is Angletarn Pikes, whilst on all other sides Place Fell stands independent and is bordered by deep valleys. The fell is bounded on the north and west by Ullswater. For the most part these flanks fall steeply to the shore, with several areas of woodland on the lower slopes. The exception is Silver Point, the promontory separating the upper and middle reaches of the lake. This is formed by Silver Crag (890 ft), an outlier standing apart from the mass of the fell. The lakeshore path from Sandwick in the north to Patterdale in the south was described by Wainwright as ''t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Beda Fell
Beda Fell is a fell in the English Lake District, situated to the south of Ullswater. It divides the valleys of Boredale and Bannerdale within the Martindale system. Topography The southern boundary of the Martindale catchment is formed by a long ridge running from Rampsgill Head to Place Fell. Spurs run north from here to separate the individual valleys and Beda Fell is one of these. Starting from its parent fell of Angletarn Pikes, the spur runs north for around two and a half miles before dropping to valley level close to Sandwick. Part way along, Beda Fell broadens and rises to its summit, the top being named as Beda Head. The top of the ridge is grassy, but the flanks are universally steep with considerable areas of crag. The western Boredale side is fairly straight, with Brock Crag below the summit and Low Brock Crag further north. The eastern flank bows outward around the summit area as the fell widens and then narrows again. Bannerdale runs below the southern slopes o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Boredale Hause
Boredale Hause is a mountain pass between Place Fell and Angletarn Pikes in the east of the English Lake District. It links the Patterdale and Boredale valleys. There is a large confusion of paths on the hause, which is largely grassy. See also *List of hill passes of the Lake District Hill passes of the Lake District were originally used by people in one valley travelling to another nearby without having to go many miles around a steep ridge of intervening hills. Historically, in the Lake District of northwest England, trav ... References Mountain passes of the Lake District {{Cumbria-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Martindale, Cumbria
Martindale is a valley, village and civil parish in Cumbria, England, situated within the Lake District National Park between the lakes of Ullswater and Haweswater. The valley is served by a narrow minor road which runs as far as the farm of Dale Head. This road commences at Howtown, a hamlet on the shore of Ullswater that forms part of the civil parish but is not in the valley of Martindale, and passes over a mountain pass or hause into the valley. At the time of the 2011 census the population of the civil parish was less than 100. Details are included in the parish of Bampton. Description Martindale runs for approximately nine km in a north to south direction, it is a remote and thinly populated valley which has a permanent population of only about 50 residents. English Lakes website. Gives population of valley as "about ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tarmacadam
Tarmacadam is a road surfacing material made by combining crushed stone, tar, and sand, patented by Welsh inventor Edgar Purnell Hooley in 1902. It is a more durable and dust-free enhancement of simple compacted stone macadam surfaces invented by Scottish engineer John Loudon McAdam in the early 1800s. The terms "tarmacadam" and tarmac are also used for a variety of other materials, including tar- grouted macadam, bituminous surface treatments and modern asphalt concrete. Origins Macadam roads pioneered by British engineer John Loudon McAdam in the 1820s are prone to rutting and generating dust. Methods to stabilise macadam surfaces with tar date back to at least 1834 when John Henry Cassell, operating from ''Cassell's Patent Lava Stone Works'' in Millwall, England, patented "lava stone". This method involved spreading tar on the subgrade, placing a typical macadam layer, and finally sealing the macadam with a mixture of tar and sand. Tar-grouted macadam was in use well before ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bridle Path
A bridle path, also bridleway, equestrian trail, horse riding path, ride, bridle road, or horse trail, is a trail or a thoroughfare that is used by people riding on horses. Trails originally created for use by horses often now serve a wider range of users, including equestrians, hikers, and cyclists. Such paths are either impassable for motorized vehicles, or vehicles are banned. The laws relating to allowable uses vary from country to country. In industrialized countries, bridle paths are now primarily used for recreation. However, they are still important transportation routes in other areas. For example, they are the main method of traveling to mountain villages in Lesotho. In England and Wales a bridle path now refers to a route which can be legally used by horse riders in addition to walkers, and since 1968, by cyclists. A "ride" is another term used for a bridleway: "a path or track, esp. one through a wood, usually made for riding on horseback" (''Oxford English Dicti ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fell
A fell (from Old Norse ''fell'', ''fjall'', "mountain"Falk and Torp (2006:161).) is a high and barren landscape feature, such as a mountain or Moorland, moor-covered hill. The term is most often employed in Fennoscandia, Iceland, the Isle of Man, parts of northern England, and Scotland. Etymology The English word "fell" comes from Old Norse ''fell'' and ''fjall'' (both forms existed). It is cognate with Danish language, Danish ''fjeld'', Faroese language, Faroese ''fjall'' and ''fjøll'', Icelandic language, Icelandic ''fjall'' and ''fell'', Norwegian language, Norwegian ''fjell'' with Norwegian dialects, dialects ''fjøll'', ''fjødd'', ''fjedd'', ''fjedl'', ''fjill'', ''fil(l)'', and ''fel'', and Swedish language, Swedish ''fjäll'', all referring to mountains rising above the Tree line, alpine tree line.Bjorvand and Lindeman (2007:270–271). British Isles In northern England, especially in the Lake District and in the Pennines, Pennine Dale (origin), Dales, the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Old Norse
Old Norse, Old Nordic, or Old Scandinavian, is a stage of development of North Germanic languages, North Germanic dialects before their final divergence into separate Nordic languages. Old Norse was spoken by inhabitants of Scandinavia and their Viking expansion, overseas settlements and chronologically coincides with the Viking Age, the Christianization of Scandinavia and the consolidation of Scandinavian kingdoms from about the 7th to the 15th centuries. The Proto-Norse language developed into Old Norse by the 8th century, and Old Norse began to develop into the modern North Germanic languages in the mid-to-late 14th century, ending the language phase known as Old Norse. These dates, however, are not absolute, since written Old Norse is found well into the 15th century. Old Norse was divided into three dialects: Old West Norse, ''Old West Norse'' or ''Old West Nordic'' (often referred to as ''Old Norse''), Old East Norse, ''Old East Norse'' or ''Old East Nordic'', and ''Ol ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
