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Shipman Knotts
Shipman Knotts is a fell in the English Lake District in Cumbria, England. It reaches a height of and is situated in one of the quieter areas of the national park, north-east of Kentmere village. Although not one of the best-known Lake District fells (and strictly speaking it is just the southern shoulder of Kentmere Pike), it earned a separate chapter in Alfred Wainwright’s Pictorial Guide to the Lakeland Fells due to ''“Its characteristic roughness . . . rocky outcrops are everywhere on its steep slopes”''. Topography The ridge from Shipman Knotts to Kentmere Pike climbs due north as far as the cairned top of Goat Scar (), before turning north-west to reach the summit of Kentmere Pike. A dry-stone wall follows the ridge, although in places it zigzags abruptly off the watershed. The eastern face above Longsleddale is steeper and includes Rough Crags and Goat Scar itself. The western face is rough but, after the initial climb out of Kentmere, has shallower gradients. The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bannisdale Horseshoe
The Bannisdale Horseshoe is an upland area in Cumbria, England, near the eastern boundary of the Lake District National Park, surrounding the valley of Bannisdale Beck, a tributary of the River Mint. It is described in the final chapter of Wainwright's book ''The Outlying Fells of Lakeland ''The Outlying Fells of Lakeland'' is a 1974 book written by Alfred Wainwright dealing with hills in and around the Lake District of England. It differs from Wainwright's '' Pictorial Guides'' in that each of its 56 chapters describes a walk, ...''. Wainwright's clockwise walk visits Whiteside Pike at , Todd Fell at , Capplebarrow at , a nameless summit at (identified in the ''Database of British and Irish Hills'' (DoBIH) as Swinklebank Crag), a further nameless summit at (identified in ''DoBIH'' as Ancrow Brow North), Long Crag at , White Howe at , a further nameless summit at (identified in ''DoBIH'' as The Forest) and Lamb Pasture at . Wainwright describes Whiteside Pike as ''"a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hollow Moor
Green Quarter Fell is an upland area in the east of the English Lake District, near Kentmere village, Cumbria. It is the subject of a chapter of Wainwright's book ''The Outlying Fells of Lakeland ''The Outlying Fells of Lakeland'' is a 1974 book written by Alfred Wainwright dealing with hills in and around the Lake District of England. It differs from Wainwright's '' Pictorial Guides'' in that each of its 56 chapters describes a walk, ...''. Wainwright's walk is an anticlockwise circuit from Kentmere, reaching the summit of Hollow Moor at and a nameless summit at and making a detour to admire the tarn of Skeggles Water. He says that the walk offers "a perfectly-balanced and lovely view of upper Kentmere... that cries aloud for a camera." References Fells of the Lake District Kentmere {{Cumbria-geo-stub ... [...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] |
Froswick
Froswick is a fell in the English Lake District, standing on the fine narrow ridge between the valleys of Kentmere and Troutbeck. Topography To the north is Thornthwaite Crag, while the adjoining fell to the south is Ill Bell. Froswick is shorter in stature than either of its neighbours and also has no obvious route of direct ascent. For these reasons it is often seen merely as a stopping point on the Ill Bell ridge, or the longer Kentmere Horseshoe walk. Froswick also apes the form of Ill Bell to a surprising degree, particularly when the ridge is viewed in profile. The western Troutbeck side is steep and smooth, except for the ravine of Blue Gill. This rends the fellside from top to bottom and is a feeder of Hagg Gill. The Kentmere flank is rougher and falls in fans of scree to the River Kent, just above Kentmere Reservoir. Topographically, Froswick has one feature which Ill Bell lacks - a subsidiary ridge. Starting out southwards from halfway down the western side, a nar ... [...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] |
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] |
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] |
Dry-stone Wall
Dry stone, sometimes called drystack or, in Scotland, drystane, is a building method by which structures are constructed from stones without any mortar to bind them together. Dry stone structures are stable because of their construction method, which is characterized by the presence of a load-bearing façade of carefully selected interlocking stones. Dry stone construction is best known in the context of stone walls, traditionally used for the boundaries of fields and churchyards, or as retaining walls for terracing, but dry stone sculptures, buildings, bridges, and other structures also exist. The term tends not to be used for the many historic styles which used precisely-shaped stone, but did not use mortar, for example the Greek temple and Inca architecture. The art of dry stone walling was inscribed in 2018 on the UNESCO representative list of the intangible cultural heritage of humanity, for dry stone walls in countries such as France, Greece, Italy, Slovenia, Cro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
A Pictorial Guide To The Lakeland Fells
''A Pictorial Guide to the Lakeland Fells'' is a series of seven books by A. Wainwright, detailing the fells (the local word for hills and mountains) of the Lake District in northwest England. Written over a period of 13 years from 1952, they consist entirely of reproductions of Wainwright's manuscript, hand-produced in pen and ink with no typeset material. The series has been in print almost continuously since it was first published between 1955 and 1966, with more than 2 million copies sold. It is still regarded by many walkers as the definitive guide to the Lakeland mountains. The 214 fells described in the seven volumes have become known as the Wainwrights. the LDWA register of those who have climbed all the fells listed 674 names. The Wainwright Society maintains a "register of current Society members who have climbed all 214 fells". First editions The first five books were originally published by Wainwright's friend, Henry Marshall, Chief Librarian of Kendal and West ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brunt Knott
Potter Fell is a fell near the villages of Burneside and Staveley, Cumbria, England, reaching a maximum height of at Brunt Knott. Alfred Wainwright in his ''The Outlying Fells of Lakeland'' identifies four summits on Potter Fell: Brunt Knott, Ulgraves and two unnamed summits, all of which are thus recognised by the Database of British and Irish Hills. There are a number of tarns on the fell, including Gurnal Dubs and Potter Tarn. Summits Potter Fell is made up of four separate peaks (as identified by Wainwright), two of which are unnamed. The first unnamed summit (395 m / 1,296 ft) lies between Potter Tarn and Brunt Knott.Lakeland Fells – Potter Fell , retrieved 30 September 2008 Further north from the first unnamed summit is Brunt Knott (427 m / 1,401 ft), [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Outlying Fells Of Lakeland
''The Outlying Fells of Lakeland'' is a 1974 book written by Alfred Wainwright dealing with hills in and around the Lake District of England. It differs from Wainwright's '' Pictorial Guides'' in that each of its 56 chapters describes a walk, sometimes taking in several summits, rather than a single fell. This has caused some confusion on the part of authors attempting to prepare a definitive list of peaks. The Outlying Fells do not form part of the 214 hills generally accepted as making up the Wainwrights, but they are included in Category 2B of the ''Hill Walkers' Register'' maintained by the Long Distance Walkers Association. The book The first edition was published in 1974 by ''The Westmorland Gazette''. It was republished by Michael Joseph in 1992 () and a second edition, revised by Chris Jesty, was published by the Wainwright Society in 2020 (). The first edition is uniform with the seven volumes of Wainwright's ''Pictorial Guides'', with a yellow band at head and fo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
