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Great Dodd
Great Dodd (meaning: ''big round hill'') is a mountain or fell in the English Lake District. It stands on the main ridge of the Helvellyn range, a line of mountains which runs in a north-south direction between the lakes of Thirlmere and Ullswater in the east of the Lake District. Great Dodd, with a height of 857 m is the highest of the fells in this range to the north of Sticks Pass. Walkers may approach Great Dodd from either High Row near Dockray to the east, or from Legburthwaite to the west – or along the main ridge track from either north or south. Scramblers with climbing skills may be attracted to three gill climbs on the western side of the mountain. The summit of Great Dodd is a smooth, grassy, rounded dome, like its two southern neighbours, Watson's Dodd and Stybarrow Dodd. Together, these three are sometimes called ‘The Three Dodds’. These three are made of volcanic rocks of the Borrowdale Volcanic Group, and the tops of all three are covered by the sa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Helvellyn
Helvellyn (; possible meaning: ''pale yellow moorland'') is a mountain in the English Lake District, the highest point of the Helvellyn range, a north–south line of mountains to the north of Ambleside, between the lakes of Thirlmere and Ullswater. Helvellyn is the third-highest point both in England and in the Lake District, and access to Helvellyn is easier than to the two higher peaks of Scafell Pike and Scafell. The scenery includes three deep glacial coves and two sharp-topped ridges on the eastern side (Striding Edge and Swirral Edge). Helvellyn was one of the earliest fells to prove popular with walkers and explorers; beginning especially in the later 18th century. Among the early visitors to Helvellyn were the poets Samuel Taylor Coleridge and William Wordsworth, both of whom lived nearby at one period. Many routes up the mountain are possible so that it may be approached from all directions. However, traversing the mountain is not without dangers; over the last two h ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mineral Vein
In geology, a vein is a distinct sheetlike body of crystallized minerals within a rock. Veins form when mineral constituents carried by an aqueous solution within the rock mass are deposited through precipitation. The hydraulic flow involved is usually due to hydrothermal circulation. Veins are classically thought of as being the ones in the body not the rock veins and arteries planar fractures in rocks, with the crystal growth occurring normal to the walls of the cavity, and the crystal protruding into open space. This certainly is the method for the formation of some veins. However, it is rare in geology for significant open space to remain open in large volumes of rock, especially several kilometers below the surface. Thus, there are two main mechanisms considered likely for the formation of veins: ''open-space filling'' and ''crack-seal growth''. Open space filling Open space filling is the hallmark of epithermal vein systems, such as a stockwork, in greisens or in cer ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Greta, Cumbria
The River Greta is a river in Cumbria, England. It is a tributary of the River Derwent and flows through the town of Keswick. "Greta" derives from the Old Norse "Griótá", meaning "stony stream".Ekwall, p. 205 The name is in records dating from the early 13th century, and also appears in Latinised form, as "Gretagila", at the time of Magna Carta. The source of the river is near Threlkeld, at the confluence of the River Glenderamackin and St. John's Beck. From there, the river runs westward, roughly aligned with the former Cockermouth, Keswick and Penrith Railway between Keswick and Penrith. The river subsequently flows through Keswick before joining the Derwent just after the latter flows out of Derwentwater.Jenkinson, pp. 131, 183 and 189 The medieval bridge over the river in Keswick was unusual in having two arches; on the great coach road from Kendal to Cockermouth all but two of the other bridges ( Troutbeck and Portinscale) crossed their rivers in a single span. The c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Trout Beck (Glenderamackin)
Trout Beck is a long stream or beck in the English Lake District, Cumbria. It rises on the northwestern slopes of Great Dodd, with tributaries including Groove Beck and Thornsgill Beck, and flows east then north to the hamlet of Troutbeck. It then flows west, parallel to and south of the A66 road, going just south of Hutton Moor End then under the old Hutton Moor Road at Wolt Bridge where it joins the River Glenderamackin. To the west of Troutbeck hamlet the beck is bridged by the former Cockermouth, Keswick and Penrith Railway The Cockermouth, Keswick and Penrith Railway (CK&PR) was an English railway company incorporated by Act of Parliament on 1 August 1861, to build a line connecting the town of Cockermouth with the London and North Western Railway (LNWR) West Coast .... References Rivers of Cumbria Derwent (Cumbria) catchment Beck watercourses {{England-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mosedale Beck (Glenderamackin)
Mosedale Beck is a river in Cumbria, England, which rises on the northern slopes of Great Dodd and flows north east, to the south of Clough Head before joining the River Glenderamackin to the east of Threlkeld village. This then flows west, alongside the A66 road south of Blencathra, to form the River Greta which flows into the River Derwent. Shortly before joining the Glendaramackin, Mosedale Beck is crossed by the Mosedale Viaduct of the former Cockermouth, Keswick and Penrith Railway The Cockermouth, Keswick and Penrith Railway (CK&PR) was an English railway company incorporated by Act of Parliament on 1 August 1861, to build a line connecting the town of Cockermouth with the London and North Western Railway (LNWR) West Coast ..., now a footpath. References Rivers of Cumbria 3Mosedale {{England-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
A Pictorial Guide To The Lakeland Fells
''A Pictorial Guide to the Lakeland Fells'' is a series of seven books by A. Wainwright, detailing the fells (the local word for hills and mountains) of the Lake District in northwest England. Written over a period of 13 years from 1952, they consist entirely of reproductions of Wainwright's manuscript, hand-produced in pen and ink with no typeset material. The series has been in print almost continuously since it was first published between 1955 and 1966, with more than 2 million copies sold. It is still regarded by many walkers as the definitive guide to the Lakeland mountains. The 214 fells described in the seven volumes have become known as the Wainwrights. the LDWA register of those who have climbed all the fells listed 674 names. The Wainwright Society maintains a "register of current Society members who have climbed all 214 fells". First editions The first five books were originally published by Wainwright's friend, Henry Marshall, Chief Librarian of Kendal and West ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alfred Wainwright
Alfred Wainwright MBE (17 January 1907 – 20 January 1991), who preferred to be known as A. Wainwright or A.W., was a British fellwalker, guidebook author and illustrator. His seven-volume ''Pictorial Guide to the Lakeland Fells'', published between 1955 and 1966 and consisting entirely of reproductions of his manuscript, has become the standard reference work to 214 of the fells of the English Lake District. Among his 40-odd other books is the first guide to the Coast to Coast Walk, a 182-mile long-distance footpath devised by Wainwright which remains popular today. Life Alfred Wainwright was born in Blackburn, Lancashire, into a family which was relatively poor, mostly because of his stonemason father's alcoholism. He did very well at school (first in nearly every subject) although he left at the age of 13. While most of his classmates were obliged to find employment in the local mills, Wainwright started work as an office boy in Blackburn Borough Engineer's Department. He ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Leat
A leat (; also lete or leet, or millstream) is the name, common in the south and west of England and in Wales, for an artificial watercourse or aqueduct dug into the ground, especially one supplying water to a watermill or its mill pond. Other common uses for leats include delivery of water for hydraulic mining and mineral concentration, for irrigation, to serve a dye works or other industrial plant, and provision of drinking water to a farm or household or as a catchment cut-off to improve the yield of a reservoir. According to the ''Oxford English Dictionary'', ''leat'' is cognate with ''let'' in the sense of "allow to pass through". Other names for the same thing include ''fleam'' (probably a leat supplying water to a mill that did not have a millpool). In parts of northern England, for example around Sheffield, the equivalent word is ''goit''. In southern England, a leat used to supply water for water-meadow irrigation is often called a ''carrier'', ''top carrier'', or ' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Drainage Divide
A drainage divide, water divide, ridgeline, watershed, water parting or height of land is elevated terrain that separates neighboring drainage basins. On rugged land, the divide lies along topographical ridges, and may be in the form of a single range of hills or mountains, known as a dividing range. On flat terrain, especially where the ground is marshy, the divide may be difficult to discern. A triple divide is a point, often a summit, where three drainage basins meet. A ''valley floor divide'' is a low drainage divide that runs across a valley, sometimes created by deposition or stream capture. Major divides separating rivers that drain to different seas or oceans are continental divides. The term ''height of land'' is used in Canada and the United States to refer to a drainage divide. It is frequently used in border descriptions, which are set according to the "doctrine of natural boundaries". In glaciated areas it often refers to a low point on a divide where it is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Keswick, Cumbria
Keswick ( ) is a market town and civil parishes in England, civil parish in the Allerdale Borough in Cumbria, England. Historic counties of England, Historically, until 1974, it was part of Cumberland. It lies within the Lake District National Park, Keswick is just north of Derwentwater and is from Bassenthwaite Lake. It had a population of 5,243 at the United Kingdom census, 2011, 2011 census. There is evidence of Prehistoric Cumbria, prehistoric occupation of the area, but the first recorded mention of the town dates from the 13th century, when Edward I of England granted a Royal charter, charter for Keswick's market, which has maintained a continuous 700-year existence. The town was an important Coal mining in the United Kingdom, mining area, and from the 18th century has been known as a holiday centre; tourism has been its principal industry for more than 150 years. Its features include the Moot Hall, Keswick, Moot Hall; a modern theatre, the Theatre by the Lake; one of Br ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Penrith, Cumbria
Penrith (, , ) is a market town and civil parish in the county of Cumbria, England, about south of Carlisle. It is less than outside the Lake District, Lake District National Park, in between the Rivers River Petteril, Petteril and River Eamont, Eamont and just north of the River Lowther. It had a population of 15,181 at the 2011 Census. Historic counties of England, Historically in Cumberland, Penrith's current local authority, local authorities are the Eden, Cumbria, Eden District Council, which is based in the town, and Cumbria County Council. In 2023, Penrith will become part of the Westmorland and Furness unitary authority area. From 1974 to 2015, it was an unparished area with no local council. A civil parish was reintroduced as Penrith Town Council and first elected on 7 May 2015. Toponymy The etymology of "Penrith" has been debated. Several writers argue for the Cumbric or Welsh language, Welsh "head, chief, end" (both noun and adjective) with the Cumbric , Wels ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
A66 Road
The A66 is a major road in Northern England, which in part follows the course of the Roman road from Scotch Corner to Penrith. It runs from east of Middlesbrough in North Yorkshire to Workington in Cumbria. Route From its eastern terminus between Redcar and Middlesbrough it runs past Stockton-on-Tees and Darlington mainly as two-lane dual-carriageway and single carriageway past Darlington, becoming motorway standard as the A66(M) shortly before meeting junction 57 of the A1(M). It shares the A1(M) route south to Scotch Corner, from where it continues west across the Pennines, past Brough, Appleby, Kirkby Thore, Temple Sowerby and Penrith until it reaches Junction 40 of the M6 motorway at Skirsgill Interchange, where traffic going towards Western Scotland turns onto the northbound M6. The A66 continues past Blencathra to Keswick and Cockermouth and on through the northern reaches of the Lake District before arriving at the coastal town of Workington. There is a short ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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