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Great Calva
Great Calva is a fell in the Lake District, England. It is in the Northern Fells, lying roughly at the centre of this region of high ground. As a result, it is distant from roads and quite remote by Lakeland standards. Great Calva stands at the head of a major geological fault running through the centre of the Lake District, and so from the summit it is possible to see all the way south over Thirlmere. The subsidiary summit of Little Calva lies to the west. Topography Skiddaw and Blencathra are the best known of the Northern Fells, fronting the range as they loom above Keswick and the road to Penrith. Behind this wall is a further group of fells, commonly referred to as Back o' Skiddaw. Wainwright, Alfred: ''A Pictorial Guide to the Lakeland Fells,Book 5 The Northern Fells'': Birkett, Bill: ''Complete Lakeland Fells'': Collins Willow (1994): This group is centred upon Knott and Great Calva is its southernmost top. To the south of Great Calva, at the centre of the Northe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 a ... [...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 Departme ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fells Of The Lake District
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 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 ''fjeld'', Faroese ''fjall'' and ''fjøll'', Icelandic ''fjall'' and ''fell'', Norwegian ''fjell'' with dialects ''fjøll'', ''fjødd'', ''fjedd'', ''fjedl'', ''fjill'', ''fil(l)'', and ''fel'', and Swedish ''fjäll'', all referring to mountains rising above the alpine tree line.Bjorvand and Lindeman (2007:270–271). British Isles In northern England, especially in the Lake District and in the Pennine Dales, the word "fell" originally referred to an area of uncultivated high ground used as common grazing usually on common land and above the timberline. Today, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Threlkeld
Threlkeld is a village and civil parish in the north of the Lake District in Cumbria, England, to the east of Keswick. It lies at the southern foot of Blencathra, one of the more prominent fells in the northern Lake District, and to the north of the River Glenderamackin. The parish had a population of 454 in the 2001 census, decreasing to 423 at the Census 2011. Overview The name is of Norse origin and is a combination of , meaning slave or serf, and , meaning a spring or well. There was extensive Norse settlement in the area during the era of Viking expansion (790s-1066). Thraell was probably a reference to native Cumbrians subjugated by the incoming Norse. Historically a part of Cumberland, Threlkeld formerly had its own railway station on the Cockermouth, Keswick and Penrith Railway, on the opposite side of the valley, next to the (closed) Threlkeld Quarry, at the foot of Clough Head. Today the railway line is a footpath and cycle track. Three rows of terraced houses, wh ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scafells
Image:Annotated Scafell range.jpg, 300px, The Scafell range as seen looking west from Crinkle Crags. (Interactive labels.) rect 23 372 252 419 Slight Side (762m) rect 173 794 560 834 Scafell East Buttress rect 707 787 893 861 Esk Crag or Buttress (c. 750m) rect 245 303 409 358 Sca Fell (964m) rect 408 238 637 280 Mickledore (c.840m) rect 544 174 826 213 South Summit (c. 950m) rect 706 310 928 355 Scafell Pike (978m) rect 870 238 1108 286 Broad Crag (934m) rect 1043 308 1198 360 Ill Crag (935m) rect 1238 311 1446 351 Great End (910m) rect 0 0 1444 1085 Click hyperlink or button to expand desc none Scafells, also known as the Scafell Massif, range of fells in the western English Lake District, made up of the remains of a caldera volcano. Fells in the range include Scafell, England's tallest mountain Scafell Pike, Broad Crag and Ill Crag. Great End, Lingmell and Slight Side are also usually included within the definition. These hills form part of the Southern Fel ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Great Gable
Great Gable is a mountain in the Lake District, United Kingdom. It is named after its appearance as a pyramid from Wasdale, though it is dome-shaped from most other directions. It is one of the most popular of the Lakeland fells, and there are many different routes to the summit. Great Gable is linked by the high pass of Windy Gap to its smaller sister hill, Green Gable, and by the lower pass of Beck Head to its western neighbour, Kirk Fell. Topography The Western Fells occupy a triangular sector of the Lake District, bordered by the River Cocker to the north east and Wasdale to the south east. Westwards, the hills diminish toward the coastal plain of Cumbria. At the central hub of the high country are Great Gable and its satellites, while two principal ridges fan out on either flank of Ennerdale, the western fells forming a horseshoe around this valley.Alfred Wainwright: ''A Pictorial Guide to the Lakeland Fells, Volume 7 The Western Fells'': Westmorland Gazette (1966): G ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lonscale Fell
Lonscale Fell is a hill in the English Lake District. Its pointed second top is instantly recognisable, standing at the eastern end of the Skiddaw massif. The fell is easily climbed from Keswick or from Skiddaw House to the north. Although now primarily a sheep pasture, it once saw considerable mining activity beneath the long eastern wall of crag. Topography The long south east ridge of Skiddaw descends over Little Man and Jenkin Hill to the depression of Flag Pots. Beyond this is the final upthrust of Lonscale Fell before the craggy descent to the Glenderaterra Beck, The southern flanks fall gently over acres of sheep pasture in the manner of the Skiddaw range. At the base of the slope is the wooded valley of Whit Beck, separating Lonscale Fell from the east ridge of Latrigg. Here also is Lonscale, the farm which has given its name to the fell. Whit Beck is a tributary of the Glenderaterra, a stream which forms the eastern boundary of Lonscale Fell. This flows due south fro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Steel Fell
Steel Fell is a fell in the English Lake District, lying between Thirlmere and Grasmere. It is triangular in plan, the ridges running north, west and south east. Steel Fell rises to the west of the Dunmail Pass road and can be climbed from the summit, or from Grasmere and Wythburn. Topography Steel Fell stands away from the main spine of the Central Fells, forming the end of one of the many east ridges of High Raise. Intermediate between the two are Codale Head and Calf Crag. Steel Fell is bordered by Wythburndale to the north and the valley of Green Burn to the south-west. The eastern face looks down on Dunmail Raise. Being triangular in plan, Steel Fell has three principal ridges. The northern ridge drops quickly to the head of Thirlmere at Steel End, while that to the south-east falls gradually toward Grasmere village, beginning down Cotra Breast. The eastern ridge connects to Calf Crag, the next fell in the popular circuit of the Greenburn valley, crossing a narrow depress ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Loughrigg Fell
Loughrigg Fell is a hill in the central part of the English Lake District. It stands on the end of the long ridge coming down from High Raise over Silver How towards Ambleside, and is separated from its neighbours by the depression of Red Bank. Topography The fell is surrounded by an unusual amount of open water. To the north the River Rothay flows through Grasmere and Rydal Water before bending around the eastern side of Loughrigg. On the southern flank the River Brathay runs from Elter Water and is also fed by the outfall from Loughrigg Tarn. The two rivers merge at Clappersgate on the south eastern corner of the fell, just before flowing into Windermere. The western boundary is formed by Red Bank (535 ft) on the ridge to Silver How. Unnamed becks fall north and south into Grasmere and Elter Water. Loughrigg has two subsidiary ridges on its eastern flank. Lanty Scar provides the obvious line of ascent from Rydal, while the spur rising over Todd Crag leads up f ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tarn (lake)
A tarn (or corrie loch) is a 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 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 many more bodies of wat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
