Sallows
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Sallows
Sallows is a fell in the English Lake District, rising between the valleys of Kentmere and Troutbeck. It is the highest point in the upland area to the south of Garburn Pass, variously termed Kentmere Park and Applethwaite Common on Ordnance Survey maps. Topography Sallows and its sister fell Sour Howes together form a horse-shoe shaped mass, with the opening to the south east. This is the catchment of Park Beck, a tributary of the River Kent. Sallows lies to the north of the beck and connects around the head of the little valley via the ridge of Moor Head. The southern flank of Sallows, above Park Beck, is smooth and grassy, other than for the remains of a quarry. The access track to these workings is still in existence, providing the easiest access from the east. The eastern end of Sallows falls in long easy slopes for half a mile toward the Kent valley, although there are a couple of low crags, particularly on Scour Rigg. The high ground then turns southerly at the subsidi ...
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Sour Howes
Sour Howes is a small fell in the English Lake District. It is situated five kilometres east of Ambleside, between the Troutbeck and Kentmere valleys and is one of the two separate fells on Applethwaite Common (the other being Sallows). Topography Sour Howes, which reaches a height of 483 m (1,585 ft) is mostly grassy although heather grows on the eastern slopes, a high dry stone wall crosses the top and links with the neighbouring fell of Sallows, which lies just over a kilometre to the north east, and with Sour Howe’s subsidiary top of Capple Howe (445 m, 1,460 ft) which is located 600 metres to the south east. The fells western flank falls away steeply to the Troutbeck valley, this slope is traversed lower down by the Dubbs Road bridleway which goes north joining the track which crosses the Garburn Pass (Restricted Byway), on its way to Kentmere. The disused and now wooded Applethwaite quarry stands on these western slope alongside the Garburn track, ...
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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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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 ...
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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 ...
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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 ...
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Coniston Old Man
The Old Man of Coniston is a fell in the Furness Fells in the Cumbria, English Lake District and is the highest point (county top) of the historic county of Lancashire. It is at least high, and lies to the west of the village of Coniston and the lake, Coniston Water. The fell is sometimes known by the alternative name of Coniston Old Man, or simply The Old Man. The mountain is popular with tourists and fell-walkers with a number of well-marked paths to the summit. The mountain has also seen extensive copper and slate mining activity for eight hundred years, and the remains of abandoned mines and spoil tips are a significant feature of the north-east slopes. Height A detailed survey on 24 May 2018 measured the height of the highest visible natural ground to be 802.42 metres (2632'7¼"). The height of the ground on the summit plinth (man-made ground) is 803.53 metres (2636'3"). The same survey also measured the height of nearby Swirl How, and measured it to be also 802.42 metres ...
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Scafell
Scafell ( or ; also spelled Sca Fell, previously Scawfell) is a mountain in the English Lake District, part of the Southern Fells. Its height of makes it the second-highest mountain in England after its neighbour Scafell Pike, from which it is separated by Mickledore col. Topography Scafell stands between Wasdale in the west and upper Eskdale to the east. The highest part of the fell is a ridge running south from Mickledore as far as Slight Side, which is counted as a separate fell by most guidebooks.Richards, Mark: ''Mid-Western Fells'': Collins (2004): Despite regarding Slight Side as a separate entity, Wainwright included the wide upland area beyond it to the south west as a part of Scafell. More modern guides have partitioned the plateau off as a further independent top, Great How. The opposing flanks of Scafell are entirely different in character. To the south, monotonous smooth slopes, stony and lacking vegetation at higher levels, run down toward Burnmoor and ...
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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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Yoke (Lake District)
Yoke is a fell in the Lake District in Cumbria, England. It has a height of 706 m (2,316 ft) and is situated in the far eastern sector of the national park, 6½ kilometres (4 miles) ENE of the town of Ambleside. Yoke is the southern extremity of the long ridge that runs southwards from the fell of High Street. Yoke’s name is believed to be derived from the Old English language word ''geoc'' which is similar to the German word ''joch'' meaning mountain ridge. Ascents Yoke is not known to Lake District writers as one of the most attractive fells but it is climbed frequently as part of the Kentmere Horseshoe, a 19-kilometre (12-mile) walk with 1,100 metres (3,609 feet) of ascent that starts and finishes in the village of Kentmere and takes in the other fells of Kentmere Pike, Harter Fell, Mardale Ill Bell, High Street, Thornthwaite Crag, Froswick and Ill Bell. Most common direct ascents go via the summit of the Garburn Pass ( Byway open to all traffic), which c ...
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Rights Of Way In England And Wales
In England and Wales, other than in the 12 Inner London London boroughs, boroughs and the City of London, the right of way is a legally protected right of the public to pass and re-pass on specific paths. The law in England and Wales differs from Scots law in that rights of way exist only where they are so designated (or are able to be designated if not already), whereas in Scotland any route that meets certain conditions is rights of way in Scotland, defined as a right of way, and in addition, there is a general presumption of access to the countryside ("right to roam"). Private rights of way or easements also exist (see also Highways in England and Wales). Inner London Definitive maps of public rights of way have been compiled for all of England and Wales, as a result of the National Parks and Access to the Countryside Act 1949, except the 12 Inner London boroughs, which, along with the City of London, were not covered by the Act. Definitive maps exist for the Outer London bo ...
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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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Diatomite
Diatomaceous earth (), diatomite (), or kieselgur/kieselguhr is a naturally occurring, soft, siliceous sedimentary rock that can be crumbled into a fine white to off-white powder. It has a particle size ranging from more than 3  μm to less than 1  mm, but typically 10 to 200 μm. Depending on the granularity, this powder can have an abrasive feel, similar to pumice powder, and has a low density as a result of its high porosity. The typical chemical composition of oven-dried diatomaceous earth is 80–90% silica, with 2–4% alumina (attributed mostly to clay minerals), and 0.5–2% iron oxide. Diatomaceous earth consists of the fossilized remains of diatoms, a type of hard-shelled microalgae. It is used as a filtration aid, mild abrasive in products including metal polishes and toothpaste, mechanical insecticide, absorbent for liquids, matting agent for coatings, reinforcing filler in plastics and rubber, anti-block in plastic films, porous support for chemic ...
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