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Sail (Lake District)
Sail is a hill in the English Lake District, lying between Derwentwater and Crummock Water. Topography The North Western Fells occupy the area between the rivers Derwent and Cocker, a broadly oval swathe of hilly country, elongated on a north-south axis. Two roads cross from east to west, dividing the fells into three convenient groups. The central sector, rising between Whinlatter Pass and Newlands Pass, includes Sail. The highest ground in the North Western Fells is an east-west ridge in this central sector, beginning with Grasmoor above Crummock Water and then gradually descending eastwards over Crag Hill, Sail, Scar Crags and Causey Pike. Sail is in every sense a satellite of Crag Fell, although having sufficient prominence to be listed as a Hewitt. From the summit of Crag Hill the eastward ridge narrows between opposing walls of crag. This rocky crest is The Scar, the depression being at around 2,425 ft. The roughness decreases as the rounded top of Sail is reach ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Crag Hill
Crag Hill is a mountain in the North Western part of the English Lake District. It was formerly known as Eel Crag; however, the Ordnance Survey now marks Eel Crag as referring to the northern crags of the fell. It is not to be confused with another Crag Hill lying on the border of North Yorkshire. It overlooks the valleys of Rannerdale on the west, and Coledale on the east. It is the second highest fell in the area of high ground between the passes of Whinlatter and Newlands, second to Grasmoor. It is 839 m (2,753 feet) high, and has a relative height of 117 m. Topography The North Western Fells occupy the area between the rivers Derwent and Cocker, a broadly oval swathe of hilly country, elongated on a north-south axis. Two roads cross from east to west, dividing the fells into three convenient groups. The central sector, rising between Whinlatter and Newlands passes, includes Crag Hill. The highest ground in the North Western Fells is an east-west ridge ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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'', or ''linking col'', or ''link'') is defined as the highest of these points, along all connecting paths; the prom ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mudstone
Mudstone, a type of mudrock, is a fine-grained sedimentary rock whose original constituents were clays or muds. Mudstone is distinguished from '' shale'' by its lack of fissility (parallel layering).Blatt, H., and R.J. Tracy, 1996, ''Petrology.'' New York, New York, W. H. Freeman, 2nd ed, 529 pp. The term ''mudstone'' is also used to describe carbonate rocks (limestone or dolomite) that are composed predominantly of carbonate mud. However, in most contexts, the term refers to siliciclastic mudstone, composed mostly of silicate minerals. The NASA Curiosity rover has found deposits of mudstone on Mars that contain organic substances such as propane, benzene and toluene. Definition There is not a single definition of mudstone that has gained general acceptance,Boggs 2006, p.143 though there is wide agreement that mudstones are fine-grained sedimentary rocks, composed mostly of silicate grains with a grain size less than . Individual grains this size are too small to be disting ... [...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] |
Ordovician
The Ordovician ( ) is a geologic period and System (geology), system, the second of six periods of the Paleozoic Era (geology), Era. The Ordovician spans 41.6 million years from the end of the Cambrian Period million years ago (Mya) to the start of the Silurian Period Mya. The Ordovician, named after the Celtic Britons, Welsh tribe of the Ordovices, was defined by Charles Lapworth in 1879 to resolve a dispute between followers of Adam Sedgwick and Roderick Murchison, who were placing the same Rock (geology), rock beds in North Wales in the Cambrian and Silurian systems, respectively. Lapworth recognized that the fossil fauna in the disputed Stratum, strata were different from those of either the Cambrian or the Silurian systems, and placed them in a system of their own. The Ordovician received international approval in 1960 (forty years after Lapworth's death), when it was adopted as an official period of the Paleozoic Era by the International Union of Geological Sciences, Intern ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Buttermere
Buttermere is a lake in the Lake District in North West England. The adjacent village of Buttermere takes its name from the lake. Historically in Cumberland, the lake is now within the county of Cumbria. Owned by the National Trust, it forms part of its Buttermere and Ennerdale property. Geography The lake is long by wide, and is deep. It has an elevation above sea level of . It is situated towards the head of the valley of the River Cocker and is surrounded by fells, notably the High Stile range to the south west, Robinson to the north-east, Fleetwith Pike and Haystacks to the south-east and Grasmoor to the north-west. The village of Buttermere stands at the north-western end of the lake, and beyond this is Crummock Water. There is a path around the lake which is about long, and at one point runs through a rock tunnel beneath the locality of Hassness. Access is by road, from Cockermouth in the north-west; from Borrowdale via the Honister Pass; or from Braithwaite and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wandope
Wandope (also known as ''Wanlope''Alfred Wainwright: ''A Pictorial Guide to the Lakeland Fells, Book 6, The North Western Fells'': Westmorland Gazette (1964): or ''Wandhope'') is a fell in the north-western area of the English Lake District. It lies to the east of Crummock Water and south of Crag Hill. From the summit there are excellent panoramas of the Sca Fell and High Stile ranges. Topography The North Western Fells occupy the area between the rivers Derwent and Cocker, a broadly oval swathe of hilly country, elongated on a north–south axis. Two roads cross from east to west, dividing the fells into three convenient groups. The central sector, rising between Whinlatter Pass and Newlands Pass, includes Wandope. The highest ground in the North Western Fells is an east–west ridge in this central sector, beginning with Grasmoor above Crummock Water and then gradually descending eastwards over Crag Hill, Sail (Lake District), Sail, Scar Crags and Causey Pike. Grasmoor has ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Braithwaite
Braithwaite is a village in the northern Lake District, in Cumbria, England. Historically in Cumberland, it lies just to the west of Keswick and to the east of the Grisedale Pike ridge, in the Borough of Allerdale. It forms part of the civil parish of Above Derwent. The eastern end of the Whinlatter Pass road is in the village. The A66 road bypasses Braithwaite, but does not enter the village. Braithwaite is situated around Coledale Beck, a brook which joins Newlands Beck shortly after passing through the village. Newlands Beck (coming from the Newlands Valley) then flows north towards Bassenthwaite Lake. Braithwaite has a Village Shop by the Low Bridge, several pubs, including the Coledale Inn, the Royal Oak and the Middle Ruddings Hotel. Braithwaite is easily accessible due to its close proximity to the A66. It has a campsite with a caravan park, B + Bs, pubs and guest houses. It has a wide range of sports including sailing, climbing, abseiling, canoeing, hang-gliding, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coledale (Cumbria)
Coledale is a valley in the northwestern region of the Lake District in Cumbria, England. Geography Coledale is a narrow U-shaped valley running approximately north-east towards the Derwent Valley floodplain and the village of Braithwaite at the northeastern end. The valley river Coledale Beck feeds into Newlands Beck and is fed by small streams from the valley sides and head, including Birkthwaite Beck, and Pudding Force. At the head of the valley a large rock formation is found named Force Crag, which forms a waterfall 'Low Force' as Pudding Beck passes over it. The valley is ringed by peaks popular with tourists (''Grisedale Pike'', ''Hopegill Head'', ''Coledale Hause'', ''Crag Hill'' (formerly ''Eel Crag''), ''Sail'', ''Sail Pass'', and ''Outerside'') forming a horseshoe ridge walk known as Coledale horseshoe or 'Coledale round'. Force Crag Mine Coledale's most notable feature is Force Crag Mine; the buildings, spoil heap and associated structures of which are practical ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Knott Rigg
Knott Rigg is a fell at the head of the Newlands Valley in the English Lake District. It is situated some 8.5 kilometres south west of Keswick and has a modest height of 556 metres (1825 feet). Its name is derived from the Old English language and means ''“hill on a knobbly ridge”''. Because of its moderate height, the fell fails to be listed on any significant hill lists but it does merit a separate chapter in Alfred Wainwright’s Pictorial Guide to the Lakeland Fells. Topography Knott Rigg is located on a four kilometre long ridge, which springs from Rigg Beck in the Newlands valley midway along its length and runs south westerly to conclude at Newlands Hause. The ridge also contains the adjoining fell of Ard Crags which stands 1.5 kilometres north east of Knott Rigg; both fells are usually climbed in combination with each other. Knott Rigg is steep sided, with the western flank falling away to the valley of Sail Beck, while the eastern side descends to the min ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ard Crags
Ard Crags is a fell in the Lake District in Cumbria, England, it is situated in the Newlands Valley just off the minor road between Keswick and Buttermere. The Ordnance Survey officially records the fell's altitude at , considerably more than the approximate that Alfred Wainwright attributed to it in his ''Pictorial Guide to the North Western Fells'', published in 1964 well before the advent of satellite mapping. Ard Crags is situated close to other higher fells such as Causey Pike and Eel Crag and can be easily overlooked. However, viewed from certain points in the Rigg Beck or Newlands valley area it presents a clearly defined and pyramidal shape which catches the eye. Topography A long high ridge sweeps east from Whiteless Pike, via Wandope, Crag Hill, Sail (Lake District) and Causey Pike, crossing from Buttermere to Stair. Running parallel to the south is a lower ridge, a tenuous connection made centrally at Sail. This lower ridge consists of Knott Rigg and Ard Crags, and h ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
