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Red Beck Top
Glaramara is a fell in the English Lake District in Cumbria. It is a substantial fell that is part of a long ridge that stretches for over six kilometres from Stonethwaite in Borrowdale up to the important mountain pass of Esk Hause. The summit of Glaramara at 783 m (2,569 ft) is the central point of this ridge, which separates the valleys of Langstrath and Grains Gill. However, the ridge has two additional fells, numerous subsidiary tops and several small tarns making its traverse an appealing and challenging walk. Name The fell’s unusual and pleasant-sounding name, previously only applied to the summit rocks, has now been accepted as the name for the whole fell. Like many fells of the district the name comes from a series of Old Norse words which in this case is translated as ''“Hill with the mountain hut by a chasm”''. Topography Glaramara’s most striking feature is Combe Gill on its northern slopes, a classic example of a hanging valley that w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Grange Fell
Grange Fell is a small fell in the English Lake District in the county of Cumbria, situated in the Borrowdale valley overlooking the villages of Grange in Borrowdale and Rosthwaite. Topography The fell has a summit plateau which consist of many heather-covered hummocks, drystone walls and clumps of trees. Well-known Lake District writer Alfred Wainwright credits Grange Fell as a single fell with three main summits, namely Brund Fell, King's How and Ether Knott. The lesser known Ether Knott is now identified as the highest point at a height of 419 metres (1,375 feet) and is less frequently visited by walkers. Brund Fell is at 415 metres (1,363 feet) while King's How is the best viewpoint and has an altitude of 392 metres (1,286 feet). On the other hand, another Lakes walking expert Bill Birkett lists Brund Fell and King's How as separate fells in his “Complete Lakeland Fells” volume,Bill Birkett:''Complete Lakeland Fells'': Collins Wil ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Esk Hause
Esk Hause is a mountain pass in the English Lake District, England. It is where the paths from Eskdale, Borrowdale, Langdale and Wasdale all meet. Esk Hause is a first step to reaching higher summits, such as Scafell Pike, Great End, Esk Pike and Allen Crags, which are all nearby. This can be a confusing place for walkers, especially in mist. This is because two paths cross at right angles on a tilted grass plateau, but not at the summit of the plateau. The popular Great Langdale-Wasdale path crosses at an elevation of at the wall shelter; this is the lower of the two passes known as Esk Hause, but is, in fact, not the true pass, which is higher and distant, a less-used pass between Eskdale and Borrowdale that occupies the depression between Great End () and Esk Pike (). The 'true' Esk Hause is the highest pass in the Lake District ( higher than Sticks Pass which crosses the Helvellyn range near Stybarrow Dodd), but Sticks Pass is commonly named as Lakeland's highest pass, most ... [...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, gen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Allen Crags
Allen Crags is a fell in the English Lake District, it lies in a group of very popular hills and is regarded as part of the Scafell group of fells. It is a hill that is frequently traversed by walkers along its ridge but is seldom climbed as the sole objective. Name The name originates from “Alein” or “Aleyn” which was a popular personal name after the Norman conquest of England, it is of Breton origin and the fell was named after an unknown French conqueror. Topography Allen Crags is situated at the southern end of a long north-south ridge that starts at Stonethwaite in Borrowdale and concludes at the strategically important mountain pass of Esk Hause. The fell is craggy and rocky and falls away steeply to the head of the Langstrath valley on its eastern side while its western flanks are characterised by grey slabs of rock and are less precipitous as they fall away to Grains Gill. To the north Allen Crags is connected to the fell of Glaramara by a three kilometre undu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Skiddaw
Skiddaw is a mountain in the Lake District National Park in England. Its summit is the sixth-highest in England. It lies just north of the town of Keswick, Cumbria, and dominates the skyline in this part of the northern lakes. It is the simplest of the Lake District mountains of this height to ascend (as there is a well-trodden tourist track from a car park to the north-east of Keswick, near the summit of Latrigg) and, as such, many walking guides recommend it to the occasional walker wishing to climb a mountain. This is the first summit of the fell running challenge known as the Bob Graham Round when undertaken in a clockwise direction. The mountain lends its name to the surrounding areas of Skiddaw Forest and Back o' Skidda, and to the isolated Skiddaw House, situated to the east, formerly a shooting lodge and subsequently a youth hostel. It also provides the name for the slate derived from that region: Skiddaw slate. Skiddaw slate has been used to make tuned percussi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rosthwaite Fell
Rosthwaite Fell is a fell in the English Lake District. It is situated some due south of Keswick and south of the village of Rosthwaite in Borrowdale. Rosthwaite Fell also has loose connections to the Scafell group of fells. The fells name derives from the Old Norse language and means “The peak above the clearing with a heap of stones” with ''“hreysi”'' meaning a heap of stones and ''“thveit”'' meaning a clearing. Topography Rosthwaite Fell reaches a height of 612 m (2,008 ft) at its highest point, which is commonly known as Rosthwaite Cam. It also has a subsidiary top, Bessyboot (550 m, 1,804 ft ), which lies 800 metres north of the main summit. Alfred Wainwright took Bessyboot as the summit of the fell for his Pictorial Guide to the Lakeland Fells. Dovenest Crag, which lies 500 metres south west of the summit, is generally considered to be a part of Glaramara and is covered in that article. The fell's boundaries are clearly defined to the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Nuttalls In England
This is a list of Nuttall mountains in England and Wales by height. Nuttalls are defined as peaks above in height, the general requirement to be called a "mountain" in the British Isles, and with a prominence above ; a mix of imperial and metric thresholds. The Nuttall classification was suggested by Anne and John Nuttall in their 1990 two–volume book, "The Mountains of England and Wales". The list was updated with subsequent revised editions by the Nuttalls. Because of the prominence threshold of only , the list is subject to ongoing revisions. In response, Alan Dawson introduced the Hewitts, with a higher prominence threshold of . This was the prominence threshold that the UIAA set down in 1994 for an "independent" peak. In 2010, Dawson replaced his Hewitts with the fully "metric" Simms, consisting of a height threshold of , and a prominence threshold of . However, both the Nuttall and Hewitt classifications have become popular with peak baggers, and both remain in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Hewitts In England
This is a list of Nuttall mountains in England and Wales by height. Nuttalls are defined as peaks above in height, the general requirement to be called a "mountain" in the British Isles, and with a prominence above ; a mix of imperial and metric thresholds. The Nuttall classification was suggested by Anne and John Nuttall in their 1990 two–volume book, "The Mountains of England and Wales". The list was updated with subsequent revised editions by the Nuttalls. Because of the prominence threshold of only , the list is subject to ongoing revisions. In response, Alan Dawson introduced the Hewitts, with a higher prominence threshold of . This was the prominence threshold that the UIAA set down in 1994 for an "independent" peak. In 2010, Dawson replaced his Hewitts with the fully "metric" Simms, consisting of a height threshold of , and a prominence threshold of . However, both the Nuttall and Hewitt classifications have become popular with peak baggers, and both remain in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scree
Scree is a collection of broken rock fragments at the base of a cliff or other steep rocky mass that has accumulated through periodic rockfall. Landforms associated with these materials are often called talus deposits. Talus deposits typically have a concave upwards form, where the maximum inclination corresponds to the angle of repose of the mean debris particle size. The exact definition of scree in the primary literature is somewhat relaxed, and it often overlaps with both ''talus'' and ''colluvium''. The term ''scree'' comes from the Old Norse term for landslide, ''skriða'', while the term ''talus'' is a French word meaning a slope or embankment. In high-altitude arctic and subarctic regions, scree slopes and talus deposits are typically adjacent to hills and river valleys. These steep slopes usually originate from late-Pleistocene periglacial processes. Notable scree sites in Eastern North America include the Ice Caves at White Rocks National Recreation Area in southern Ve ... [...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] |
Ice Age
An ice age is a long period of reduction in the temperature of Earth's surface and atmosphere, resulting in the presence or expansion of continental and polar ice sheets and alpine glaciers. Earth's climate alternates between ice ages and greenhouse periods, during which there are no glaciers on the planet. Earth is currently in the Quaternary glaciation. Individual pulses of cold climate within an ice age are termed ''glacial periods'' (or, alternatively, ''glacials, glaciations, glacial stages, stadials, stades'', or colloquially, ''ice ages''), and intermittent warm periods within an ice age are called '' interglacials'' or ''interstadials''. In glaciology, ''ice age'' implies the presence of extensive ice sheets in both northern and southern hemispheres. By this definition, Earth is currently in an interglacial period—the Holocene. The amount of anthropogenic greenhouse gases emitted into Earth's oceans and atmosphere is predicted to prevent the next glacial period for th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
