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Scafells
Image:Annotated Scafell range.jpg, 300px, The Scafell range as seen looking west from Crinkle Crags. (Interactive labels.) rect 23 372 252 419 Slight Side (762m) rect 173 794 560 834 Scafell East Buttress rect 707 787 893 861 Esk Crag or Buttress (c. 750m) rect 245 303 409 358 Sca Fell (964m) rect 408 238 637 280 Mickledore (c.840m) rect 544 174 826 213 South Summit (c. 950m) rect 706 310 928 355 Scafell Pike (978m) rect 870 238 1108 286 Broad Crag (934m) rect 1043 308 1198 360 Ill Crag (935m) rect 1238 311 1446 351 Great End (910m) rect 0 0 1444 1085 Click hyperlink or button to expand desc none Scafells, also known as the Scafell Massif, range of fells in the western English Lake District, made up of the remains of a caldera volcano. Fells in the range include Scafell, England's tallest mountain Scafell Pike, Broad Crag and Ill Crag. Great End, Lingmell and Slight Side are also usually included within the definition. These hills form part of the Southern Fells. G ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scafell Pike
Scafell Pike () is the highest and the most prominent mountain in England, at an elevation of above sea level. It is located in the Lake District National Park, in Cumbria, and is part of the Southern Fells and the Scafell massif. Scafell Pike forms part of the inactive Scafells volcano. Etymology and name history The name ''Scafell'' is believed by some to derive from the Old Norse ''skalli fjall'', meaning either the fell with the shieling or the fell with the bald summit, and is first recorded in 1578 in the corrupted form ''Skallfield''. An alternative derivation is from the Old Norse "skagi", meaning a cape, headland, promontory or peninsula – so giving an etymology that aligns with Skaw in Shetland. It originally referred to Scafell, which neighbours Scafell Pike.Dorothy Wordsworth's ascent of Scafell Pike, 1818, http://www.pastpresented.ukart.com/eskdale/wordsworth1.htm What are now known as Scafell Pike, Ill Crag, and Broad Crag were collectively called either ''t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Southern Fells
Image:Annotated Scafell range.jpg, 300px, The Scafells rect 23 372 252 419 Slight Side, Slight Side (762 m) rect 173 794 560 834 Sca Fell, Scafell East Buttress rect 707 787 893 861 Esk Pike, Esk Pike or Crag (885 m) rect 245 303 409 358 Sca Fell, Sca Fell (964 m) rect 408 238 637 280 Mickledore, Mickledore (c. 840 m) rect 544 174 826 213 Scafell Pike, South Summit (<978 m) rect 706 310 928 355 Scafell Pike, Scafell Pike (978 m) rect 870 238 1108 286 Broad Crag, Broad Crag (934 m) rect 1043 308 1198 360 Ill Crag, Ill Crag (935 m) rect 1238 311 1446 351 Great End, Great End (910 m) rect 0 0 1444 1085 #top, Click hyperlink or button to expand desc none The Southern Fells are a group of hills in the England, English Lake District. Including Scafell Pike, the highest peak in England, they occupy a broad area to the south of Great Langdale, Borrowdale and Wasdale. High and rocky towards the centre of the Lake District, the Southern Fells progressively take on a moorland c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bowfell
Bowfell (named ''Bow Fell'' on Ordnance Survey maps) is a pyramid-shaped mountain lying at the heart of the English Lake District, in the Southern Fells area. It is the sixth-highest mountain in the Lake District and one of the most popular of the Lake District fells for walkers. It is listed in Alfred Wainwright's 'best half dozen' Lake District fells. Topography The Southern Fells include the highest ground in England, a horseshoe which begins with Scafell and Scafell Pike in the west and then curves around the north of Upper Eskdale to take in Great End, Esk Pike, Bowfell and Crinkle Crags. In addition to Eskdale, Bowfell has a footing in two other well known valleys. It stands at the head of Great Langdale — its east ridge dividing the two branches of Mickleden and Oxendale — while to the north is the Langstrath branch of Borrowdale. From all of these valleys Bowfell presents a striking profile with a conical top resting upon a wider summit plateau. To the north-w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Calderas Of England
A caldera ( ) is a large cauldron-like hollow that forms shortly after the emptying of a magma chamber in a volcano eruption. When large volumes of magma are erupted over a short time, structural support for the rock above the magma chamber is gone. The ground surface then collapses into the emptied or partially emptied magma chamber, leaving a large depression at the surface (from one to dozens of kilometers in diameter). Although sometimes described as a crater, the feature is actually a type of sinkhole, as it is formed through subsidence and collapse rather than an explosion or impact. Compared to the thousands of volcanic eruptions that occur each century, the formation of a caldera is a rare event, occurring only a few times per century. Only seven caldera-forming collapses are known to have occurred between 1911 and 2016. More recently, a caldera collapse occurred at Kīlauea, Hawaii in 2018. Etymology The term ''caldera'' comes from Spanish ', and Latin ', meaning "c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Caldera
A caldera ( ) is a large cauldron-like hollow that forms shortly after the emptying of a magma chamber in a volcano eruption. When large volumes of magma are erupted over a short time, structural support for the rock above the magma chamber is gone. The ground surface then collapses into the emptied or partially emptied magma chamber, leaving a large depression at the surface (from one to dozens of kilometers in diameter). Although sometimes described as a Volcanic crater, crater, the feature is actually a type of sinkhole, as it is formed through subsidence and collapse rather than an explosion or impact. Compared to the thousands of volcanic eruptions that occur each century, the formation of a caldera is a rare event, occurring only a few times per century. Only seven caldera-forming collapses are known to have occurred between 1911 and 2016. More recently, a caldera collapse occurred at Kīlauea, Hawaii in 2018. Etymology The term ''caldera'' comes from Spanish language, S ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Caldera
A caldera ( ) is a large cauldron-like hollow that forms shortly after the emptying of a magma chamber in a volcano eruption. When large volumes of magma are erupted over a short time, structural support for the rock above the magma chamber is gone. The ground surface then collapses into the emptied or partially emptied magma chamber, leaving a large depression at the surface (from one to dozens of kilometers in diameter). Although sometimes described as a Volcanic crater, crater, the feature is actually a type of sinkhole, as it is formed through subsidence and collapse rather than an explosion or impact. Compared to the thousands of volcanic eruptions that occur each century, the formation of a caldera is a rare event, occurring only a few times per century. Only seven caldera-forming collapses are known to have occurred between 1911 and 2016. More recently, a caldera collapse occurred at Kīlauea, Hawaii in 2018. Etymology The term ''caldera'' comes from Spanish language, S ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Slight Side
Slight Side is a fell in the English Lake District it stands 25 kilometres east southeast of the town of Whitehaven and reaches a height of 762 m (2,499 ft). Slight Side lies at the south western edge of the Scafells, Scafell Massif, a four-kilometre-long crescent of high ground which includes the highest ground in England. The fells names derives from the Old Norse language and means ''"The mountain shieling with the level pastures"'', it is a combination of the Norse words "sletta" and "saetr". With a shieling meaning a shepherds hut or a mountain pasture used in the summer. Topography When viewed from the valley of Eskdale, Cumbria, Eskdale the fell is seen as a distinct peak but in reality it is just the terminal point on Scafell’s southern ridge before it descends steeply to Eskdale. It only has 14 metres of topographic prominence between itself and Scafell (the col is at 748 metres) and therefore narrowly fails to qualify as a List of Nuttalls in England, Nuttal ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sca Fell
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mickledore
Mickledore (the name means ''great door'' or ''pass'') is a narrow ridge, 840 metres (2755 ft) high, connecting the mountains of Scafell and Scafell Pike in the English Lake District. It is also a pass between the valleys of Wasdale and Eskdale. Ridge The ridge is easily reached and traversed from Scafell Pike to the north, or from the valleys to the east and west. However, access to the summit of Scafell is barred by the rockface of Broad Stand, which looks much easier to climb than it is (the climb is "Difficult" in the British grading system). In descent, the cliff is even more dangerous. The poet Samuel Taylor Coleridge probably made a descent on 5 August 1802; he wrote: :I began to suspect that I ought not to go on, but then unfortunately tho' I could with ease drop down a smooth Rock high, I could not climb it, so go on I must and on I went. The next 3 drops were not half a Foot, at least not a foot more than my own height, but every Drop increased the Palsy ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lingmell
Lingmell is a fell in the English Lake District, standing above the village of Wasdale Head. It is an outlier on the north-west flank of Scafell Pike, England’s highest mountain. Topography Although standing in the shadow of its taller parent, Lingmell is very much a separate entity. In the manner of many fells it displays two contrasting aspects. The southern and western slopes– although steep– are smooth and rounded, while the northern and eastern faces fall as crags directly from the summit. The northern crag drops for a thousand feet toward the valley floor, with a further thousand feet of scree below. The connection to Scafell Pike is via Lingmell Col, a grassy depression at 734 metres (2,410 ft.) Flowing west from the col is Lingmell Gill, descending through Hollow Stones to Brackenclose at the head of Wast Water. To the east of Lingmell Col runs Piers Gill, a stream descending from high on the Scafells. This flows right around the northern perimeter of Ling ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Great End
Great End is the most northerly mountain in the Scafell chain, in the English Lake District. From the south it is simply a lump continuing this chain. From the north, however, it appears as an immense mountain, with an imposing north face rising above Sprinkling Tarn (lake). This is a popular location for wild camping, and the north face attracts many climbers. Alfred Wainwright wrote of Great End in his Pictorial Guide to the Lakeland Fells: "This is the true Lakeland of the fellwalker, the sort of terrain that calls him back time after time, the sort of memory that haunts his long winter exile. It is not the pretty places - the flowery lanes of Grasmere or Derwentwater's wooded bays - that keep him restless in his bed; it is the magnificent ones. Places like Great End..." Topography The imposing north-eastern cliffs, riven by gullies, rise some 600 ft from the Esk Hause path. Their orientation ensures that the sun rarely reaches them, the gullies often retaining sn ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dacite
Dacite () is a volcanic rock formed by rapid solidification of lava that is high in silica and low in alkali metal oxides. It has a fine-grained (aphanitic) to porphyritic texture and is intermediate in composition between andesite and rhyolite. It is composed predominantly of plagioclase feldspar and quartz. Dacite is relatively common, occurring in many tectonic settings. It is associated with andesite and rhyolite as part of the subalkaline volcanic rock, subalkaline tholeiite, tholeiitic and calc-alkaline magma series. Composition Dacite consists mostly of plagioclase feldspar and quartz with biotite, hornblende, and pyroxene (augite or enstatite). The quartz appears as rounded, corroded phenocrysts, or as an element of the ground-mass. The plagioclase in dacite ranges from oligoclase to andesine and labradorite. Sanidine occurs, although in small proportions, in some dacites, and when abundant gives rise to rocks that form rhyodacite, transitions to the rhyolites. The rel ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
