Burnmoor Tarn
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Burnmoor Tarn
Burnmoor Tarn, on Eskdale Fell in Cumbria, England, is one of the largest entirely natural tarns in the Lake District. Its waters flow into Whillan Beck at the tarn's north-eastern corner, which immediately turns south and flows into Eskdale, joining the Esk at Beckfoot. Burnmoor Lodge, a former fishing lodge, stands by the southern shore and a mediaeval corpse road runs past the eastern shore where it fords the beck. Eskdale Moor or Boat How lies to the south of the tarn. The tarn is one of the sites in DEFRA's UK Upland Waters Monitoring Network. It occupies and lies at an altitude of in a moraine hollow on the uplands between Wastwater and Eskdale. The lake has two distinct basins close to the south-eastern shore and a maximum depth of . There are four main inflow streams to the north and north-west. The outflow at the eastern end joins the Hardrigg Beck which drains the slopes of Scafell and, in times of especially high flow, is partly diverted into the lake across a brai ...
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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. ...
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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 ...
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Tarn (lake)
A tarn (or corrie loch) is a Proglacial lake, proglacial mountain lake, pond or pool, formed in a cirque excavated by a glacier. A moraine may form a natural dam below a tarn. Etymology The word is toponymy, derived from the Old Norse word ''tjörn'' ("a small mountain lake without tributaries") meaning pond. In parts of Northern England - predominantly Cumbria but also areas of North Lancashire and North Yorkshire - 'tarn' is widely used as the name for small lakes or ponds, regardless of their location and origin (e.g. Talkin Tarn, Urswick Tarn, Malham Tarn). Similarly, in Scandinavian languages, a ''tjern'' or ''tjørn'' (both Norwegian) or ''tjärn'' or ''tärn'' (both Swedish) is a small natural lake, often in a forest or with vegetation closely surrounding it or growing into the tarn. The specific technical use for a body of water in a glacial corrie comes from high number of tarns found in corries in the Lake District, an upland area in Cumbria. Nonetheless, there are ...
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Eskdale, Cumbria
Eskdale is a glacial valley and civil parish in the western Lake District National Park in Cumbria, England. It forms part of the Borough of Copeland, and in 2001 had a population of 264, increasing to 304 at the 2011 Census. One of the Lake District's most popular tourist attractions, the Ravenglass and Eskdale Railway, runs through the valley, though along with other western valleys of the Lake District, Eskdale is notably quieter during the high summer season than the more accessible eastern areas. Topography The River Esk flows through the valley to its estuary at Ravenglass. The valley is notable in being one of few major valleys in the Lake District not to have its own lake, although several tarns are perched above the valley sides. The main access to the valley is from the western end; however, there is also a steep pass with a motor road leading out of the valley to the east over Hardknott Pass, as well as a road with beautiful views leading southwards over Birker ...
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River Esk, Cumbria
The River Esk, sometimes called the Cumbrian Esk, is a river in Cumbria, England. It flows for approximately 25 km (15.5 miles) from its source in the Scafells range of mountains to its estuary at Ravenglass. It is one of two Rivers Esk in Cumbria, and not to be confused with the Border Esk which flows into Cumbria from Scotland. Course The Esk rises in the Sca Fell range of mountains at a height of 800 metres, just below Esk Hause, the mountain pass between the fells of Great End and Esk Pike. The infant river then flows southerly through wild and picturesque countryside receiving many streams flowing off the Scafell range, the most significant of which are Calfcove Gill and Little Narrowcove Beck. The river makes several leaps over waterfalls including the Esk Falls before being joined by its first major tributary Lingcove Beck at Lingcove Bridge. Within a few miles the Esk passes Brotherilkeld Farm, which formerly belonged to the monks of Furness Abbey, at this po ...
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Corpse Road
Corpse roads provided a practical means for transporting corpses, often from remote communities, to cemetery, cemeteries that had burial rights, such as parish churches and chapel of ease, chapels of ease. In Britain, such routes can also be known by a number of other names, e.g.: bier road, burial road, coffin line, coffin road, corpse way, funeral road, lych way, lyke way, or procession way. etc. Such "church-ways" have developed a great deal of associated folklore regarding ghosts, spirits, ghost#Terminology, wraiths, etc. Origins In late medieval times a population increase and an expansion of church building took place in Great Britain inevitably encroaching on the territories of existing mother churches or minster (cathedral), minsters. Demands for autonomy from outlying settlements made minster officials feel that their authority was waning, as were their revenues, so they instituted corpse roads connecting outlying locations and their mother churches (at the heart of pari ...
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Boat How
Boat How or Eskdale Moor is a hill in the English Lake District, near Boot, in the Borough of Copeland, Cumbria. It lies south of Burnmoor Tarn, between the River Mite to the west and the Whillan Beck tributary of Eskdale to the east. It is the subject of a chapter of Wainwright's book ''The Outlying Fells of Lakeland''. It reaches and Wainwright describes an anticlockwise circuit from Boot. He says: "Its proliferation of ancient remains makes it a happy hunting ground for walkers with an eye for relics of days long past", mentioning the presence of four stone circles. Richards in his ''Fellranger'' books names the hill as Eskdale Moor and refers to the summit outcrop as Boat How, but the Database of British and Irish Hills identifies it as Boat How, while classifying it as a Tump, Outlying Fell, Birkett, Synge and Fellranger. Richards describes ascent routes from Dalegarth railway station, Miterdale Forest or the village of Eskdale Green, and describes the fell ...
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Department For Environment, Food And Rural Affairs
The Department for Environment, Food and Rural Affairs (Defra) is a department of His Majesty's Government responsible for environmental protection, food production and standards, agriculture, fisheries and rural communities in the United Kingdom. Concordats set out agreed frameworks for co operation, between it and the Scottish Government, Welsh Government and Northern Ireland Executive, which have devolved responsibilities for these matters in their respective nations. Defra also leads for the United Kingdom on agricultural, fisheries and environmental matters in international negotiations on sustainable development and climate change, although a new Department of Energy and Climate Change was created on 3 October 2008 to take over the last responsibility; later transferred to the Department for Business, Energy and Industrial Strategy following Theresa May's appointment as Prime Minister in July 2016. Creation The department was formed in June 2001, under the leadersh ...
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Moraine
A moraine is any accumulation of unconsolidated debris (regolith and rock), sometimes referred to as glacial till, that occurs in both currently and formerly glaciated regions, and that has been previously carried along by a glacier or ice sheet. It may consist of partly rounded particles ranging in size from boulders (in which case it is often referred to as boulder clay) down to gravel and sand, in a groundmass of finely-divided clayey material sometimes called glacial flour. Lateral moraines are those formed at the side of the ice flow, and terminal moraines were formed at the foot, marking the maximum advance of the glacier. Other types of moraine include ground moraines (till-covered areas forming sheets on flat or irregular topography) and medial moraines (moraines formed where two glaciers meet). Etymology The word ''moraine'' is borrowed from French , which in turn is derived from the Savoyard Italian ("mound of earth"). ''Morena'' in this case was derived from Provenà ...
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Wastwater
Wast Water or Wastwater () is a lake located in Wasdale, a valley in the western part of the Lake District National Park, England. The lake is almost long and more than wide. It is a glacial lake, formed in a glacially 'over-deepened' valley. It is the deepest lake in England at . The surface of the lake is about above sea level, while its bottom is over below sea level. It is owned by the National Trust. Surroundings The head of the Wasdale Valley is surrounded by some of the highest mountains in England, including Scafell Pike, Great Gable and Lingmell. The steep slopes on the southeastern side of the lake, leading up to the summits of Whin Rigg and Illgill Head, are known as the "Wastwater Screes" or on some maps as "The Screes". These screes formed as a result of ice and weathering erosion on the rocks of the Borrowdale Volcanic Group, that form the fells to the east of the lake, towards Eskdale. They are approximately , from top to base, the base being about below th ...
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Scafell
Scafell ( or ; also spelled Sca Fell, previously Scawfell) is a mountain in the English Lake District, part of the Southern Fells. Its height of makes it the second-highest mountain in England after its neighbour Scafell Pike, from which it is separated by Mickledore col. Topography Scafell stands between Wasdale in the west and upper Eskdale to the east. The highest part of the fell is a ridge running south from Mickledore as far as Slight Side, which is counted as a separate fell by most guidebooks.Richards, Mark: ''Mid-Western Fells'': Collins (2004): Despite regarding Slight Side as a separate entity, Wainwright included the wide upland area beyond it to the south west as a part of Scafell. More modern guides have partitioned the plateau off as a further independent top, Great How. The opposing flanks of Scafell are entirely different in character. To the south, monotonous smooth slopes, stony and lacking vegetation at higher levels, run down toward Burnmoor and ...
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River Delta
A river delta is a landform shaped like a triangle, created by deposition (geology), deposition of sediment that is carried by a river and enters slower-moving or stagnant water. This occurs where a river enters an ocean, sea, estuary, lake, reservoir, or (more rarely) another river that cannot carry away the supplied sediment. It is so named because its triangle shape resembles the Greek letter Delta. The size and shape of a delta is controlled by the balance between watershed processes that supply sediment, and receiving basin processes that redistribute, sequester, and export that sediment. The size, geometry, and location of the receiving basin also plays an important role in delta evolution. River deltas are important in human civilization, as they are major agricultural production centers and population centers. They can provide Coast, coastline defense and can impact drinking water supply. They are also Ecology, ecologically important, with different species' assemblages ...
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