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Mardale Ill Bell
Mardale Ill Bell is a fell in the English Lake District, rising to the south west of Haweswater Reservoir. It stands on the watershed between Mardale and Kentmere and is the highpoint of the south-eastern ridge of High Street, midway on its course to Harter Fell. Topography The head of the Kentmere valley lies to the south-west of the fell with rough slopes leading down over scree to Kentmere Reservoir. Mardale Ill Bell sends out a short grass-topped spur, Lingmell End, which splits the head of the valley into two. The north-eastern face of Mardale Ill Bell forms the craggy backdrop to Blea Water. This perfect corrie tarn is the deepest in the Lake District at 207 ft. Its outflow feeds Haweswater, joining with that of a second tarn, Small Water. Between the two, Mardale Ill Bell throws out the rocky spur of Piot Crag. Two tiers of crag drop down to the confluence at Mardale Waters. South-east of the summit a rough narrowing ridge drops to Nan Bield Pass at 2,100 ft ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
High Street (Lake District)
High Street is a fell in the English Lake District. At 828 metres (2,718 ft), its summit is the highest point in the far eastern part of the national park. The fell is named after the Roman road which ran over the summit. History Roman road A Roman road, a scheduled monument, crosses the fell between Roman forts at Brougham ('' Brocavum'') near Penrith and Ambleside ('' Galava''). Although the route takes the road higher than any other Roman road in England, the High Street range has quite gentle slopes and a flat summit plateau, characteristics that may have persuaded Roman surveyors to build the road over the fell tops rather than through the valleys which were densely forested and marshy making them susceptible to ambush. There has been speculation that the Romans made use of a prehistoric trackway. The nature of the Roman road remains problematic, as much of it is sunken in a hollow, rather than being built on top of an embankment or ''agger'' in the usual ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Harter Fell (Mardale)
Harter Fell is a fell in the far eastern part of the English Lake District. The summit at lies the meeting point of three ridges, and Harter Fell forms the head of three valleys: Mardale, Longsleddale and the valley of the River Kent. Topography In plan section the summit area forms a horseshoe, open to the south east. This ridge is narrow and grassy, with a relatively new fence in place. There are subsidiary tops on both horns of the horseshoe. The southern ridge passes over The Knowe and then Brown Howe, before connecting to Kentmere Pike. The eastern branch includes the rocky top of Little Harter Fell (2,234 ft), and Adam Seat (2,185 ft) which is marked by a prominent boundary stone. This ridge continues down to Gatescarth Pass before rising again to Branstree. Connecting to the centre of the summit horseshoe, producing a shape not unlike a tuning fork in plan, is Harter Fell's third ridge. This starts lower down the fell-side and cannot be seen from the summit. Th ... [...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] |
Furness Fells
The Furness Fells are a multitude of hills and mountains in the Furness region of Cumbria, England. Historically part of Lancashire, the Furness Fells or High Furness is the name given to the upland part of Furness, that is, that part of Furness lying north of the line between Ulverston and Ireleth. The hills lie largely within the English Lake District. The term ''Furness Fells'' is also sometimes used as a synonym with ''Coniston Fells'', perhaps partly as a result of the placing of the words "Furness Fells" on some Ordnance Survey 1:250 000 maps. The Coniston Fells properly form only part of the Furness Fells, albeit with all the highest mountains; other fells in Furness are of lower altitude. The Coniston Fells form part of the Southern Fells of the Lake District as defined by Alfred Wainwright. Coniston Fells The Coniston Fells are separated from the Scafell and Bowfell massif to their north by Wrynose Pass, and are surrounded on all other sides by lower ground. Coniston ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ill Bell
Ill Bell is a fell in the English Lake District, in the county of Cumbria, standing on the narrow ridge between the valleys of Kentmere and Troutbeck. Topography To the north is Froswick, a strikingly similar lesser copy, while the adjoining fell to the south is Yoke. Ill Bell appears from some directions to be a perfectly symmetrical bell-shaped peak, and 'Hill Bell' is one possible derivation of the name, quoted by Alfred Wainwright.Alfred Wainwright:''A Pictorial Guide to the Lakeland Fells'', Book 2: With this form aped by Froswick, the ridge assumes an unmistakable 'roller-coaster' appearance when viewed in profile. The western side is steep and relatively smooth, falling not direct to the Troutbeck valley but to its main tributary, Hagg Gill. The low top of Troutbeck Tongue stands between the two valleys. The eastern Kentmere flank is rougher and steeper, falling in a great tumble of scree to the shore of Kentmere Reservoir. There is the hint of a ridge to the north-eas ... [...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 s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 1,9 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nan Bield Pass
Hill passes of the Lake District were originally used by people in one valley travelling to another nearby without having to go many miles around a steep ridge of intervening hills. Historically, in the Lake District of northwest England, travel on foot or by pony was difficult because of the region's steep-sided valleys so tracks across the ridges were created taking the easiest route over passes – often, but not always, via a col. Since Roman times long-distance travel had tended to be along ridges. From the 19th century these passes and ridge routes were brought back into use when recreational hill walking become popular. Forty hill passes within the Lake District National Park are listed here, using criteria for selecting the major routes. Background The Lake District National Park was created in 1951 covering an area of over and, although its population is only 42,000, over 10 million visitors arrive each year, mostly attracted by the lakes and fells. Geology Abou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kentmere Reservoir
Kentmere Reservoir is a water storage facility situated in the Kentmere valley in the county of Cumbria, England. It is located north-northeast of the town of Windermere. The reservoir is fed by the streams which form the headwaters of the River Kent which rise to the north in Hall Cove on the southern slopes of a mountainous ridge called High Street, which is named after the nearby Roman road. It is also fed by Lingmell Gill, which drains the large corrie on the western side of Harter Fell beneath the Nan Bield Pass. After Kentmere Tarn was drained to provide agricultural land in the 1840s, water supply to the mills further downstream became erratic, and the mill owners met to plan a reservoir to regulate the flow. They employed the water engineer John Frederick Bateman to advise, and the Act of Parliament obtained in 1845 authorised five reservoirs. Despite Bateman's preference for the reservoir at Skeggles Water, the millers opted to build that at Kentmere Head, which was c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kentmere
Kentmere is a valley, village and civil parish in the Lake District National Park, a few miles from Kendal in the South Lakeland district of Cumbria, England. Historically in Westmorland, at the 2011 census Kentmere had a population of 159. Geography The narrow valley spans about in length and begins with a bowl of hills known as the Kentmere Round; a horseshoe of high fells which surrounds Kentmere Reservoir. The River Kent, which gives Kendal its name, begins from Hall Cove, a corrie at the head of the valley, before flowing through the reservoir. Access to this part of the valley is available via the Roman High Street, over Nan Bield Pass, from Troutbeck over Garburn Pass ( Bridleway only. No motor vehicles), or along an old bridleway up from the village. The valley is sandwiched between Troutbeck on the west side and Longsleddale on the east. It can be reached by road only by travelling through the village of Staveley, which sits at its mouth where the river meets the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
