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Brae Fell
Brae Fell is a fell in the English Lake District, situated 12 kilometres north of Keswick it reaches a height of 586 m (1,923 ft) and is regarded as part of the Caldbeck Fells along with High Pike and Carrock Fell even though it has ridge links to the Uldale Fells. The fell's name has Scottish overtones and translates from the Scots language as a hillside or slope. Its northern flanks face the Scottish Borders country across the Eden Valley and Solway Firth. Topography Brae Fell is large and grassy and is really an outlying part of Great Sca Fell being situated on that fell's northern ridge separated by a col with a height of approximately 570 metres. With a height of less than 2000 feet and prominence of around 16 metres it fails to be a fell of real importance. Alfred Wainwright gives it a chapter in his Pictorial Guide to the Lakeland Fells, being less than complimentary, saying, ''“If all hills were like Brae Fell there would be far fewer fell walkers”''. It i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Knott, Caldbeck
Knott is a mountain in the northern part of the English Lake District. It is the highest point of the ''Back o'Skiddaw'' region, an area of wild and unfrequented moorland to the north of Skiddaw and Blencathra. Other tops in this region include High Pike, Carrock Fell and Great Calva. The fell's slopes are mostly smooth, gentle, and covered in grass, with a few deep ravines. It stands a long way from a road and requires a long walk across the moor top get to it; this, as well as the fact that it is hidden from the rest of the Lake District by the two aforementioned giants, make it one of the most unfrequented tops in the Lakes. When it is climbed it is most often from Mungrisdale or from the north via Great Sca Fell. The word ''Knott'' is of Cumbric origin, and means simply "hill". 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scottish Borders
The Scottish Borders ( sco, the Mairches, 'the Marches'; gd, Crìochan na h-Alba) is one of 32 council areas of Scotland. It borders the City of Edinburgh, Dumfries and Galloway, East Lothian, Midlothian, South Lanarkshire, West Lothian and, to the south-west, south and east, the English counties of Cumbria and Northumberland. The administrative centre of the area is Newtown St Boswells. The term Scottish Borders, or normally just "the Borders", is also used to designate the areas of southern Scotland and northern England that bound the Anglo-Scottish border. Geography The Scottish Borders are in the eastern part of the Southern Uplands. The region is hilly and largely rural, with the River Tweed flowing west to east through it. The highest hill in the region is Broad Law in the Manor Hills. In the east of the region, the area that borders the River Tweed is flat and is known as 'The Merse'. The Tweed and its tributaries drain the entire region with the river flowi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pennines
The Pennines (), also known as the Pennine Chain or Pennine Hills, are a range of uplands running between three regions of Northern England: North West England on the west, North East England and Yorkshire and the Humber on the east. Commonly described as the "backbone of England", the range stretches northwards from the Peak District at the southern end, through the South Pennines, Yorkshire Dales and North Pennines to the Tyne Gap, which separates the range from the Border Moors and Cheviot Hills across the Anglo-Scottish border, although some definitions include them. South of the Aire Gap is a western spur into east Lancashire, comprising the Rossendale Fells, West Pennine Moors and the Bowland Fells in North Lancashire. The Howgill Fells and Orton Fells in Cumbria are sometimes considered to be Pennine spurs to the west of the range. The Pennines are an important water catchment area with numerous reservoirs in the head streams of the river valleys. The North Pennin ... [...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] |
Lead
Lead is a chemical element with the symbol Pb (from the Latin ) and atomic number 82. It is a heavy metal that is denser than most common materials. Lead is soft and malleable, and also has a relatively low melting point. When freshly cut, lead is a shiny gray with a hint of blue. It tarnishes to a dull gray color when exposed to air. Lead has the highest atomic number of any stable element and three of its isotopes are endpoints of major nuclear decay chains of heavier elements. Lead is toxic, even in small amounts, especially to children. Lead is a relatively unreactive post-transition metal. Its weak metallic character is illustrated by its amphoteric nature; lead and lead oxides react with acids and bases, and it tends to form covalent bonds. Compounds of lead are usually found in the +2 oxidation state rather than the +4 state common with lighter members of the carbon group. Exceptions are mostly limited to organolead compounds. Like the lighter members of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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] |
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] |
Topographic Prominence
In topography, prominence (also referred to as autonomous height, relative height, and shoulder drop in US English, and drop or relative height in British English) measures the height of a mountain or hill's summit relative to the lowest contour line encircling it but containing no higher summit within it. It is a measure of the independence of a summit. A peak's ''key col'' (the highest col surrounding the peak) is a unique point on this contour line and the ''parent peak'' is some higher mountain, selected according to various criteria. Definitions The prominence of a peak may be defined as the least drop in height necessary in order to get from the summit to any higher terrain. This can be calculated for a given peak in the following way: for every path connecting the peak to higher terrain, find the lowest point on the path; the ''key col'' (or ''key Saddle point, saddle'', or ''linking col'', or ''link'') is defined as the highest of these points, along all connecting pat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Great Sca Fell
Great Sca Fell is a fell in the English Lake District, seven kilometres (4½ miles) southwest of the village of Caldbeck. It is the highest of the four Uldale Fells, the other three being Longlands Fell, Meal Fell and Great Cockup. It is a Wainwright, and the lowest of the lakeland ‘Sca fells’, the other two being Scafell and Scafell Pike. Topography The Uldale fells are a smooth and grassy sheep pasture which rise in three ridges from the low land to the north and culminate at the summit of Great Sca Fell at a height of 651 m (2,136 ft). Although the hill is a ‘Wainwright’ fell and comfortably crests the 2000-foot mark, it does not meet the criteria for any of the other major hill lists; with a prominence of 13 metres to the higher fell of Knott it narrowly fails to qualify as a Nuttall. The fell has twin summits, Great and Little Sca Fell, with Little Sca Fell, which reaches an elevation of 635 metres (2,083 feet), lying 400 metres north of the main summi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Solway Firth
The Solway Firth ( gd, Tràchd Romhra) is a firth that forms part of the border between England and Scotland, between Cumbria (including the Solway Plain) and Dumfries and Galloway. It stretches from St Bees Head, just south of Whitehaven in Cumbria, to the Mull of Galloway, on the western end of Dumfries and Galloway. The Isle of Man is also very near to the firth. The firth comprises part of the Irish Sea. The firth’s coastline is characterised by lowland hills and small mountains. It is a mainly rural area, with mostly small villages and settlements (such as Powfoot). Fishing, hill farming, and some arable farming play a large part in the local economy, although tourism is increasing. The northern part of the English coast of the Solway Firth was designated as an Area of Outstanding Natural Beauty, known as the Solway Coast, in 1964. Construction of the Robin Rigg Wind Farm in the firth began in 2007. Within the firth, there are some salt flats and mud flats that can b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Eden, Cumbria
The River Eden is a river that flows through the Eden District of Cumbria, England, on its way to the Solway Firth. Etymology The river was known to the Romans as the ''Itouna'', as recorded by the Greek geographer Claudius Ptolemaeus (Ptolemy) in the 2nd century AD. This name derives from the Celtic word ''ituna'', meaning ''water'', or ''rushing''. Thus there is no relation to the biblical Garden of Eden. Course of river The Eden rises in Black Fell Moss, Mallerstang, on the high ground between High Seat, Yorkshire Dales and Hugh Seat. Here it forms the boundary between the counties of Cumbria and North Yorkshire. Two other rivers arise in the same peat bogs here, within a kilometre of each other: the River Swale and River Ure. It starts life as Red Gill Beck, then becomes Hell Gill Beck, before turning north and joining with Ais Gill Beck to become the River Eden. (Hell Gill Force, just before it meets Ais Gill Beck, is the highest waterfall along its journey to the sea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scots Language
Scots ( endonym: ''Scots''; gd, Albais, ) is an Anglic language variety in the West Germanic language family, spoken in Scotland and parts of Ulster in the north of Ireland (where the local dialect is known as Ulster Scots). Most commonly spoken in the Scottish Lowlands, Northern Isles and northern Ulster, it is sometimes called Lowland Scots or Broad Scots to distinguish it from Scottish Gaelic, the Goidelic Celtic language that was historically restricted to most of the Scottish Highlands, the Hebrides and Galloway after the 16th century. Modern Scots is a sister language of Modern English, as the two diverged independently from the same source: Early Middle English (1150–1300). Scots is recognised as an indigenous language of Scotland, a regional or minority language of Europe, as well as a vulnerable language by UNESCO. In the 2011 United Kingdom census, 2011 Scottish Census, over 1.5 million people in Scotland reported being able to speak Scots. As there are ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
