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Caudale
Stony Cove Pike (alternatively known as Caudale Moor or John Bell's Banner) is a fell in the Far Eastern part of the English Lake District. It stands on the other side of the Kirkstone Pass from Red Screes, and is on the end of a ridge coming down from High Street. It is separated from its neighbours by the deep col of Threshthwaite Mouth, so is a Marilyn (a hill with topographic prominence of at least 150m) – the sixteenth highest in the Lake District. Name There is considerable variation over use of the alternative names for the fell. The Ordnance Survey maps name the main summit as 'Stony Cove Pike', the second top to the west as 'Caudale Moor' and 'John Bell's Banner' is reserved for the south west ridge descending to St Raven's Edge. Alfred Wainwright in his '' Pictorial Guide to the Lakeland Fells'' uses Caudale Moor for the fell as a whole, John Bell's Banner as an alternative to this and Stony Cove Pike as a name for the (main) summit. Bill Birkett p ...
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Hartsop Dodd
Hartsop Dodd is a fell in the English Lake District, standing to the south east of Brothers Water. It is a subsidiary top on the north ridge of Caudale Moor, but was given separate fell status by Wainwright in his ''Pictorial Guide to the Lakeland Fells''.Alfred Wainwright:''A Pictorial Guide to the Lakeland Fells'', Book 2: That convention is followed here. Topography A broad grassy ridge descends gently from Caudale Moor, running north from the summit plateau and topped by a stone wall. After about half a mile it narrows considerably and turns north-west for the same distance again. Finally it throws up a small grassy dome which is the summit of Hartsop Dodd. After this the ridge drops quickly to valley level between Hartsop village and Brothers Water. The western flank of the ridge stands above the high valley of Caudale, which is a feeder of Kirkstone Beck and Brothers Water. On the eastern side is Pasture Bottom, the valley of Pasture Beck. This stream joins the outflow ...
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Wansfell
Wansfell is a fell in English Lake District situated 1½ miles (2.5 kilometres) east of the town of Ambleside. The fell is part of the long southern ridge of Caudale Moor and occupies the swath of territory between Ambleside and the Troutbeck valley. Topography Wansfell has an extensive summit ridge with two tops. The highest point of the fell is called Baystones with a height of 488 m (1,601 ft), while Wansfell Pike, which lies a kilometre to the south west reaches an elevation of 482 m (1,581 ft). Of the two summits, Wansfell Pike is regarded as the “true” summit of the fell by many fell walkers because of its superior view, even though it is the lower of the pair. Despite its modest elevation, Wansfell has significant topographic prominence, being linked to the higher fell of Caudale Moor by a col near the Kirkstone Pass road (A592) with a height of around 339.2 metres. This gives the fell a prominence of 147.7 metres, which means it just fails to ac ...
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Thornthwaite Crag
Thornthwaite Crag is a fell in the English Lake District, standing to the west of Haweswater Reservoir. It is a focal point of the Far Eastern Fells, standing at the head of several valleys. Topography The summit area is broadly horseshoe-shaped, concave to the north with the head of Hayeswater Gill in the opening. The north-western horn of the shoe connects to Gray Crag and the north-eastern ridge to High Street and Mardale Ill Bell. Two other principal ridges run south to Froswick and west to Caudale Moor. The north-eastern and southern ridges enclose the head of Kentmere with scree and crag predominating. To the south-west of Thornthwaite Crag is the craggy head of the long valley of Troutbeck, emptying into Windermere. Between the western and north-western ridges is the head of Pasture Beck, which ultimately joins Hayeswater Beck en route to Ullswater. The western ridge to Caudale Moor is narrow and rough, dropping very steeply to the depression of Threshwaite Mouth at ...
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List Of Fells In The Lake District
This is a list of fells, hills, mountains, groups of mountains and subsidiary summits and tops in the Lake District, England. Alphabetical list A *Allen Crags * Angletarn Pikes *Ard Crags *Armboth Fell * Arnison Crag * Arthur's Pike B *Bakestall * Bannerdale Crags * Barf * Barrow * Base Brown * Beda Fell *Binsey * Birker Fell *Birkhouse Moor * Birks * Black Combe * Black Fell *Blake Fell *Blea Rigg *Bleaberry Fell *Blencathra *Bonscale Pike * Bowfell *Bowscale Fell *Brae Fell *Brandreth *Branstree *Brim Fell * Brock Crags * Broom Fell * Brown Pike * Buckbarrow * Buck Pike * Burnbank Fell C * Calf Crag *Carl Side * Carrock Fell * Castle Crag * Catbells * Catstycam * Caudale Moor * Causey Pike * Caw Fell *Clough Head * Cold Pike *Coniston Old Man *Crag Fell *Crinkle Crags D * Dale Head *Dent *Dodd *Dollywaggon Pike * Dove Crag *Dow Crag E * Eagle Crag * Eel Crag (Crag Hill) * Esk Pike F * Fairfield * Fellbarrow *Firbank Fell * Fleetwith Pike *Froswick G * Gavel ...
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Far Eastern Fells
The Far Eastern Fells are a group of hills in the English Lake District. Reaching their highest point at High Street (828 metres or 2.718 ft.), they occupy a broad area to the east of Ullswater and Kirkstone Pass. Much quieter than the central areas of Lakeland they offer in general easier walking as the fells merge mainly into the surrounding moorlands. Partition of the Lakeland Fells The Lake District is a National Park in the north-west of the country which – in addition to its lakes – features a complex range of hills. These are locally known as fells and range from low hills to the highest ground in England. Hundreds of tops exist and many writers have attempted to draw up definitive lists. In doing so the compilers frequently divide the range into smaller areas to aid their description. The most influential of all such authors was Alfred Wainwright, whose ''Pictorial Guide to the Lakeland Fells'' series has sold in excess of 2 million copies, being in print c ...
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Gray Crag
Gray Crag is a fell in the Lake District in Cumbria, England. Topography The fell reaches a height of 699 metres (2,293 feet) at the northern end of its summit ridge and this is the accepted highest point which gives the best views, although there is a spot height of 710 metres (2,329 feet) less than a kilometre to the south. Both tops have small cairns set on grass. Gray Crag is located in the far eastern sector of the national park, five kilometres south east of the village of Patterdale, and is basically the narrow grassy northern ridge of the adjoining fell of Thornthwaite Crag. It is characterised by very steep flanks with crags and gullies which fall away towards Hayeswater on the eastern side and Pasture Beck to the west. This fell should not be confused with Grey Crag another Lakeland Fell also in the far eastern sector above Longsleddale. Ascents Gray Crag is almost invariably ascended from the hamlet of Hartsop where there is a car park, Hay ...
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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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Red Screes
Red Screes is a fell in the English Lake District, situated between the villages of Patterdale and Ambleside. It may be considered an outlier of the Fairfield group in the Eastern Fells, but is separated from its neighbours by low cols. This gives Red Screes an independence which is reflected in its prominence. Topography Red Screes is a ridge of high ground which runs for nearly 7 km in a north north-easterly direction from the town of Ambleside, and reaches a maximum height of 776 m. This ridge narrows at either end, giving it the shape of a long upturned boat. It is separated from neighbouring fells by Scandale Pass to the west (c.516 m) and Kirkstone Pass to the east (455 m). These two low cols mean that Red Screes is seen as an independent fell when viewed from the south of the Lake District. They also give the fell sufficient prominence to be classified as a Marilyn. There are two minor subsidiary tops: Snarker Pike (644 m) on the south ridge ...
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Kirkstone Pass
Kirkstone Pass is a mountain pass in the English Lake District, in the county of Cumbria. It is at an altitude of . It is the District's highest pass traversed by road, the A592 road between Ambleside in Rothay Valley and Patterdale in Ullswater Valley. The road gradient approaches 1 in 4. The picturesque view down into Patterdale has Brothers Water as its focal point. The Kirkstone Pass Inn stands close to the summit. Once a vital coaching inn, it now caters primarily for tourists. It is the third-highest public house in England. Slate quarrying Lead and copper ore mining and slate mining has spanned centuries. Petts Quarry worked by Kirkstone Green Slate Company is just to the Ambleside side of the summit. Nearby is Hartsop Hall lead mine. Caudale slate mine is a few miles further down, on the Ullswater side, and was last worked at the beginning of the 20th century; all its adits are now blocked. Name The name of the pass comes from a prominent stone, the Ki ...
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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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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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Ridge
A ridge or a mountain ridge is a geographical feature consisting of a chain of mountains or hills that form a continuous elevated crest for an extended distance. The sides of the ridge slope away from the narrow top on either side. The lines along the crest formed by the highest points, with the terrain dropping down on either side, are called the ridgelines. Ridges are usually termed hills or mountains as well, depending on size. Smaller ridges, especially those leaving a larger ridge, are often referred to as spurs. Types There are several main types of ridges: ;Dendritic ridge: In typical dissected plateau terrain, the stream drainage valleys will leave intervening ridges. These are by far the most common ridges. These ridges usually represent slightly more erosion resistant rock, but not always – they often remain because there were more joints where the valleys formed or other chance occurrences. This type of ridge is generally somewhat random in orientation, often ...
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