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Bowscale Fell
Bowscale Fell is a hill in the English Lake District. It rises above the village of Mungrisdale in the Northern Fells. Bowscale Fell stands at the extreme north east the Blencathra group, connected to this higher fell by the intervening Bannerdale Crags. In common with many fells the western slopes are smooth and convex while the eastern side exhibits crags. Topography A curving ridge surrounds the head of Bannerdale, with Bowscale Fell at the northern end and Bannerdale Crags to the south. The ridgeline is broad and grassy with occasional patches of bog and a couple of small tarns in the north. Bannerdale flows due east from the depression between the two fells to its junction with the River Glenderamackin. A second tributary of the Glenderamackin, Bullfell Beck, runs parallel a little to the north, its source being directly beneath the summit of Bowscale Fell. The heads of the two valleys are divided by a truncated east ridge, The Tongue, which sports a top (1,814 ft ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Blencathra
Blencathra, also known as Saddleback, is one of the most northerly hills in the English Lake District. It has six separate fell tops, of which the highest is the Hallsfell Top at 2,848 feet (868 metres). Name For many years, Ordnance Survey listed Blencathra under the alternative name of Saddleback, which was coined in reference to the shape of the mountain when seen from the east. The guidebook author Alfred Wainwright popularised the use of the older Cumbric name, which is now used almost exclusively. Ordnance Survey currently marks the summit as ‘Saddleback or Blencathra’. It is likely that the name Blencathra is derived from the Cumbric elements *''blain'' ‘top, summit’ and ''cadeir'' ‘seat, chair’, meaning ‘the summit of the seat-like mountain’. Andrew Breeze has proposed an alternative interpretation of the second element of the name, arguing that it represents a Cumbric cognate of Middle Welsh ''carthwr'' ‘working horse’. Richard Coates has sug ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Victorian Era
In the history of the United Kingdom and the British Empire, the Victorian era was the period of Queen Victoria's reign, from 20 June 1837 until her death on 22 January 1901. The era followed the Georgian period and preceded the Edwardian period, and its later half overlaps with the first part of the '' Belle Époque'' era of Continental Europe. There was a strong religious drive for higher moral standards led by the nonconformist churches, such as the Methodists and the evangelical wing of the established Church of England. Ideologically, the Victorian era witnessed resistance to the rationalism that defined the Georgian period, and an increasing turn towards romanticism and even mysticism in religion, social values, and arts. This era saw a staggering amount of technological innovations that proved key to Britain's power and prosperity. Doctors started moving away from tradition and mysticism towards a science-based approach; medicine advanced thanks to the adoption ... [...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, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North Western Fells
The North Western Fells are a group of hills in the English Lake District. Including such favourites as Catbells and Grisedale Pike, they occupy an oval area beneath the Buttermere and Borrowdale valley systems. The North Western Fells are characterised by soaring east-west ridges and an absence of mountain tarns. Partition of the Lakeland Fells The Lake District is a National Park in the north west of the country which, in addition to its lakes, contains a complex range of hills. These are known locally as fells and range from low hills to the highest ground in England. Hundreds of tops exist and many writers have attempted to draw up definitive lists. In doing so the compilers frequently divide the range into smaller areas to aid their description. The most influential of all such authors was Alfred Wainwright whose ''Pictorial Guide to the Lakeland Fells'' series has sold in excess of 2 million copies, [...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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Helvellyn Range
The Helvellyn range is the name given to a part of the Eastern Fells in the English Lake District, "fell" being the local word for "hill". The name comes from Helvellyn, the highest summit of the group. The Helvellyn range forms a ridge extending for about 10 km, at no point dropping below 600 m. The ridge runs in a north–south direction, with Patterdale on the eastern side and the Thirlmere valley to the west. The village of Threlkeld lies directly to the north, below the northernmost point on the ridge, Clough Head. Generally, the slopes above Thirlmere are steep and grassy, whilst the Patterdale side exhibits rockier features, due to cirque glaciation on the north east side of the ridge. List of peaks The majority of the peaks in the range lie directly on the north–south axis, although there are some outliers on the eastern side of the ridge. *Clough Head (726 m) *Great Dodd (856 m) *Watson's Dodd (789 m) *Stybarrow Dodd (843 m) ** Gree ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Great Dodd
Great Dodd (meaning: ''big round hill'') is a mountain or fell in the English Lake District. It stands on the main ridge of the Helvellyn range, a line of mountains which runs in a north-south direction between the lakes of Thirlmere and Ullswater in the east of the Lake District. Great Dodd, with a height of 857 m is the highest of the fells in this range to the north of Sticks Pass. Walkers may approach Great Dodd from either High Row near Dockray to the east, or from Legburthwaite to the west – or along the main ridge track from either north or south. Scramblers with climbing skills may be attracted to three gill climbs on the western side of the mountain. The summit of Great Dodd is a smooth, grassy, rounded dome, like its two southern neighbours, Watson's Dodd and Stybarrow Dodd. Together, these three are sometimes called ‘The Three Dodds’. These three are made of volcanic rocks of the Borrowdale Volcanic Group, and the tops of all three are covered by the sa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Great Mell Fell
Great Mell Fell (''Bare hill'', with the later additions of both "Fell" and "Great") is an isolated hill or fell in the English Lake District, north of Ullswater and adjacent to the Eastern Fells. It rises from a level plain to a height of 537 m. Its top is an excellent viewpoint for many of the surrounding higher fells. The fell is now owned and managed by the National Trust and offers a place of quiet refuge. The fell was once well wooded, and retains a good covering of trees on the lower slopes, as well as scattered larches and pines higher up. Its rock is unusual for the Lake District, a reddish conglomerate of Devonian age, which has been eroded to form a rounded hill with smooth outlines and no rocky crags. Topography Great Mell Fell is an isolated hill which rises abruptly from a wide expanse of marshy lowland to a height of 537 m. The fell has smooth, rounded outlines with no crags. Rock is represented only by a number of large erratic boulders, mainly on the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Keswick, Cumbria
Keswick ( ) is a market town and civil parish in the Allerdale Borough in Cumbria, England. Historically, until 1974, it was part of Cumberland. It lies within the Lake District National Park, Keswick is just north of Derwentwater and is from Bassenthwaite Lake. It had a population of 5,243 at the 2011 census. There is evidence of prehistoric occupation of the area, but the first recorded mention of the town dates from the 13th century, when Edward I of England granted a charter for Keswick's market, which has maintained a continuous 700-year existence. The town was an important mining area, and from the 18th century has been known as a holiday centre; tourism has been its principal industry for more than 150 years. Its features include the Moot Hall; a modern theatre, the Theatre by the Lake; one of Britain's oldest surviving cinemas, the Alhambra; and the Keswick Museum and Art Gallery in the town's largest open space, Fitz Park. Among the town's annual events is t ... [...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] |
Great Calva
Great Calva is a fell in the Lake District, England. It is in the Northern Fells, lying roughly at the centre of this region of high ground. As a result, it is distant from roads and quite remote by Lakeland standards. Great Calva stands at the head of a major geological fault running through the centre of the Lake District, and so from the summit it is possible to see all the way south over Thirlmere. The subsidiary summit of Little Calva lies to the west. 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, commonly referred to as Back o' Skiddaw. Wainwright, Alfred: ''A Pictorial Guide to the Lakeland Fells,Book 5 The Northern Fells'': Birkett, Bill: ''Complete Lakeland Fells'': Collins Willow (1994): This group is centred upon Knott and Great Calva is its southernmost top. To the south of Great Calva, at the centre of the Northe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carrock Fell
Carrock Fell is a fell in the English Lake District, situated in the northern region of the national park, 8 miles (13 kilometres) north-east of Keswick. Etymology The name ''Carrock'' is a Brittonic formation. Sometimes stated as deriving from ''carreg'' meaning "rock, stony place", early attestations of the name suggest that is more likely to represent ''*carr'', "rock, hard-surface", with the adjectival and nominal suffix ''-ǭg'', sometimes meaning "abounding in". Height The fell's elevation seems to have decreased by two metres in recent years. The Ordnance Survey now give it a height of 661 m (2,168 ft) in the most recent map updates after having recorded it at for many years. Many guidebooks and mountain tables still record 663 metres as the “official” height. Topography Well known Lake District scribe Alfred Wainwright rated Carrock Fell as the second most exciting and interesting fell in the northern area of Lakeland (after Blencathra and before Ski ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
