Bakestall
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Bakestall
Bakestall is a fell in the English Lake District, it is situated seven kilometres (4½ miles) north of Keswick in the quieter, even secluded northern sector of the national park known as ‘Back o’ Skiddaw’. Topography Bakestall reaches a height of 673 m (2,208 ft) and strictly speaking it is not a separate fell being just an insignificant rise on Skiddaw’s northern slopes. Alfred Wainwright gave Bakestall a separate chapter in his ''Pictorial Guide to the Lakeland Fells'' because of the impressive Dead Crags which fall beneath the summit and the fine waterfall of Whitewater Dash at the fells foot. Indeed Bakestall was not even mentioned on the old Ordnance Survey one-inch map for many years, a situation now rectified on its metric equivalent probably because of Wainwright’s having drawn attention to the fell. Dead Crags are composed of Skiddaw Slate and drop 150 metres (500 feet) down into the corrie on the northern side of the fell. The crags do not at ...
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List Of Wainwrights
Wainwrights are the 214 English peaks (known locally as ''fells'') described in Alfred Wainwright's seven-volume ''Pictorial Guide to the Lakeland Fells'' (1955–66). They all lie within the boundary of the Lake District National Park in Cumbria, and all but one (Castle Crag) are over in height. Over two million copies of the ''Pictorial Guides'' have been sold since their publication. In 1974, Wainwright published a supplementary volume ''The Outlying Fells of Lakeland'' (1974), which includes another 116 summits (described in 56 walks); these are the Wainwright Outlying Fells. Summiting all of the Wainwrights is a popular form of peak bagging in the Lake District, along with the Birketts. Because both lists are based on historical books, unlike, for example, the Munros, their constituents remain fixed, regardless of revisions to height or other metrics. In this regard, they are similar to the Scottish lowlands, Donalds. There are 214 Wainwrights, of which 209 are also c ...
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Skiddaw
Skiddaw is a mountain in the Lake District National Park in England. Its summit is the sixth-highest in England. It lies just north of the town of Keswick, Cumbria, and dominates the skyline in this part of the northern lakes. It is the simplest of the Lake District mountains of this height to ascend (as there is a well-trodden tourist track from a car park to the north-east of Keswick, near the summit of Latrigg) and, as such, many walking guides recommend it to the occasional walker wishing to climb a mountain. This is the first summit of the fell running challenge known as the Bob Graham Round when undertaken in a clockwise direction. The mountain lends its name to the surrounding areas of Skiddaw Forest and Back o' Skidda, and to the isolated Skiddaw House, situated to the east, formerly a shooting lodge and subsequently a youth hostel. It also provides the name for the slate derived from that region: Skiddaw slate. Skiddaw slate has been used to make tuned percussi ...
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Dash Valley
The Dash Valley is a small valley in the English Lake District. It has only one dwelling, Dash Farm, the fields of which spread right across the valley. The valley is flanked on the northern side by Great Cockup, and on the southern side by Bakestall, part of the Skiddaw massif. At the head of the valley Dash Beck, the river which flows through the valley, falls dramatically forming Dash Falls The dash is a punctuation mark consisting of a long horizontal line. It is similar in appearance to the hyphen but is longer and sometimes higher from the baseline. The most common versions are the endash , generally longer than the hyphen b ... (aka Whitewater Dash), which Wainwright called the finest succession of falls in the Lake District. A private road leads up the valley to Dash Farm, and a track branches off this and goes all the way up the valley, past Dash Falls to Skiddaw House, a former shepherd's hut now used as a youth hostel. External links References Valleys ...
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Great Cockup
Great Cockup is a fell in the northern region of the English Lake District, one of the four Uldale Fells (the others being Longlands Fell, Great Sca Fell and Meal Fell). Description Great Cockup reaches a height of and merits a chapter in Alfred Wainwright's ''Pictorial Guide to the Lakeland Fells''. Wainwright describes the fell as functional rather than ornamental, writing: "Viewed from a distance Great Cockup appears as a modest but extensive eminence with no obvious summit and nothing calling for closer inspection. First impressions are confirmed by a tour of exploration, the fell underfoot proving no more attractive than the fell at a distance." Etymology The fell is known as "Great" to distinguish it from its smaller neighbour Little Cockup which lies on its north-western shoulder overlooking the hamlet of Orthwaite with a height of . The fell's name originates from the Old English language, a combination of the words ''cocc'' and ''hop'', where ''hop'' means a ...
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Skiddaw Slate
Skiddaw slate is an early Ordovician metamorphosed sedimentary rock, as first identified on the slopes of Skiddaw in the English Lake District. The base of this series is unknown. The thickness could, therefore, amount to several thousand feet of sediment. These sediments were formed about 500 mya by deposition in a shallow sea, low-energy environment. The series contains differing grain sizes and comprises grits, flags, shales and mudstones. In some places, there is evidence of intrusion In geology, an igneous intrusion (or intrusive body or simply intrusion) is a body of intrusive igneous rock that forms by crystallization of magma slowly cooling below the surface of the Earth. Intrusions have a wide variety of forms and com ... of Skiddaw Granite into the Skiddaw Slates, close to the anticlinal axis of the Lake District. Skiddaw slate has a grey hue (as opposed to Honister slate which has a green hue) and is used for building, in the Lake District. The traditional build ...
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Solway Firth
The Solway Firth ( gd, Tràchd Romhra) is a firth that forms part of the border between England and Scotland, between Cumbria (including the Solway Plain) and Dumfries and Galloway. It stretches from St Bees Head, just south of Whitehaven in Cumbria, to the Mull of Galloway, on the western end of Dumfries and Galloway. The Isle of Man is also very near to the firth. The firth comprises part of the Irish Sea. The firth’s coastline is characterised by lowland hills and small mountains. It is a mainly rural area, with mostly small villages and settlements (such as Powfoot). Fishing, hill farming, and some arable farming play a large part in the local economy, although tourism is increasing. The northern part of the English coast of the Solway Firth was designated as an Area of Outstanding Natural Beauty, known as the Solway Coast, in 1964. Construction of the Robin Rigg Wind Farm in the firth began in 2007. Within the firth, there are some salt flats and mud flats that can b ...
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Cairn
A cairn is a man-made pile (or stack) of stones raised for a purpose, usually as a marker or as a burial mound. The word ''cairn'' comes from the gd, càrn (plural ). Cairns have been and are used for a broad variety of purposes. In prehistoric times, they were raised as markers, as memorials and as burial monuments (some of which contained chambers). In modern times, cairns are often raised as landmarks, especially to mark the summits of mountains. Cairns are also used as trail markers. They vary in size from small stone markers to entire artificial hills, and in complexity from loose conical rock piles to elaborate megalithic structures. Cairns may be painted or otherwise decorated, whether for increased visibility or for religious reasons. A variant is the inuksuk (plural inuksuit), used by the Inuit and other peoples of the Arctic region of North America. History Europe The building of cairns for various purposes goes back into prehistory in Eurasia, ranging in s ...
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Cumbria Way
The Cumbria Way is a linear long-distance footpath in Cumbria, England. The majority of the route is inside the boundaries of the Lake District National Park. Linking the two historic Cumbrian towns of Ulverston and Carlisle, it passes through the towns of Coniston and Keswick. The route cuts through Lakeland country via Coniston Water, Langdale, Borrowdale, Derwent Water, Skiddaw Forest and Caldbeck. It is a primarily low-level route with some high-level exposed sections. History The Cumbria Way was originally devised in the 1970s by local Ramblers Association members. The waymarking of the entire route was completed by volunteers and national park staff in May 2007. Route The route can be walked in either direction but is described here as south to north beginning at the trailhead of Ulverston and ending in Carlisle. Stage 1: Ulverston to Coniston The route leaves the urban area of Ulverston, birthplace of Stan Laurel, and heads north towards the village of Gawthwaite a ...
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Bassenthwaite Lake
Bassenthwaite Lake is one of the largest water bodies in the English Lake District. It is long and narrow, approximately long and wide, but is also extremely shallow, with a maximum depth of about . It is the only body of water in the Lake District to use the word ''"lake"'' in its name, all the others being ''"waters"'' (for example, Derwentwater), ''"meres"'' (for example, Windermere) or ''"tarns"'' (for example, Dock Tarn). It is fed by, and drains into, the River Derwent. The lake lies at the foot of Skiddaw, near the town of Keswick. Some maps dating from the 18th century do in fact mark this lake with the name ''Bassenwater'', and the use of the name ''Broadwater'' for this lake is also attested. The A66 dual carriageway runs roughly north–south along the western side of the lake. The lay-bys are popular spots for photographers and bird watchers looking for osprey. The section running south towards Keswick was built along the course of the former Cockermouth, K ...
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Lead
Lead is a chemical element with the symbol Pb (from the Latin ) and atomic number 82. It is a heavy metal that is denser than most common materials. Lead is soft and malleable, and also has a relatively low melting point. When freshly cut, lead is a shiny gray with a hint of blue. It tarnishes to a dull gray color when exposed to air. Lead has the highest atomic number of any stable element and three of its isotopes are endpoints of major nuclear decay chains of heavier elements. Lead is toxic, even in small amounts, especially to children. Lead is a relatively unreactive post-transition metal. Its weak metallic character is illustrated by its amphoteric nature; lead and lead oxides react with acids and bases, and it tends to form covalent bonds. Compounds of lead are usually found in the +2 oxidation state rather than the +4 state common with lighter members of the carbon group. Exceptions are mostly limited to organolead compounds. Like the lighter members of the ...
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Climbing
Climbing is the activity of using one's hands, feet, or any other part of the body to ascend a steep topographical object that can range from the world's tallest mountains (e.g. the eight thousanders), to small boulders. Climbing is done for locomotion, sporting recreation, and for competition, and is also done in trades that rely on ascension; such as emergency rescue and military operations. Climbing is done indoors and outdoors and on natural (e.g. rock and ice) and artificial surfaces. Professional mountain guides or rock climbing guides (e.g. the UIAGM), were a significant element in developing the popularity of the sport in the natural environment, and remain so today. Since the 1980s, the development of competition climbing and the availability of artificial climbing walls have dramatically increased the popularity of rock climbing as a sport and led to the emergence of professional rock climbers, such as Wolfgang Güllich, Chris Sharma, Lynn Hill and Catherine ...
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Cirque
A (; from the Latin word ') is an amphitheatre-like valley formed by glacial erosion. Alternative names for this landform are corrie (from Scottish Gaelic , meaning a pot or cauldron) and (; ). A cirque may also be a similarly shaped landform arising from fluvial erosion. The concave shape of a glacial cirque is open on the downhill side, while the cupped section is generally steep. Cliff-like slopes, down which ice and glaciated debris combine and converge, form the three or more higher sides. The floor of the cirque ends up bowl-shaped, as it is the complex convergence zone of combining ice flows from multiple directions and their accompanying rock burdens. Hence, it experiences somewhat greater erosion forces and is most often overdeepened below the level of the cirque's low-side outlet (stage) and its down-slope (backstage) valley. If the cirque is subject to seasonal melting, the floor of the cirque most often forms a tarn (small lake) behind a dam, which marks the down ...
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