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List Of Hills In The Lake District
This is a list of hills in the Lake District. To avoid the list becoming infinitely long and arbitrary, only hills with more than 30 m relative height (rising over ) are included. This includes most, but not all, Wainwrights as well as many other hills. Topographically, the boundaries of the Lake District trace the flow of streams from the lowest point between it and the Pennines. This occurs just north of the Howgill Fells and gives the boundaries as, primarily, the River Eden and River Lune. This list therefore includes all hills to the west of those rivers including the so-called 'Westmorland Plateau' to the north of the Howgills. Hills are grouped as topographically as possible, according to their 'parent Marilyn'. The parent Marilyn of hill A can be found by dividing the nearby area into territories, by tracing the runoff from the key col of each Marilyn. The parent is the Marilyn whose territory hill A resides in. Marilyns are given in bold-faced font. In the table ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hill
A hill is a landform that extends above the surrounding terrain. It often has a distinct Summit (topography), summit. Terminology The distinction between a hill and a mountain is unclear and largely subjective, but a hill is universally considered to be not as tall, or as Grade (slope), steep as a mountain. Geographers historically regarded mountains as hills greater than above sea level, which formed the basis of the plot of the 1995 film ''The Englishman who Went up a Hill but Came down a Mountain''. In contrast, hillwalkers have tended to regard mountains as peaks above sea level. The ''Oxford English Dictionary'' also suggests a limit of and Whittow states "Some authorities regard eminences above as mountains, those below being referred to as hills." Today, a mountain is usually defined in the UK and Ireland as any summit at least high, while the official UK government's definition of a mountain is a summit of or higher. Some definitions include a topographical pro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dodd (Skiddaw)
Dodd is a small fell in the Lake District, Cumbria, England, four kilometres north-west of Keswick. It forms part of the Skiddaw range in the northern part of the national park and the slopes are heavily wooded. Forestry Dodd lies on Forestry England land known as Dodd Wood; for many years it was extensively planted with conifers right up to the summit which obstructed the view. However, Forestry England started a programme of tree clearance from the top of the fell in 2001 and the summit of the fell is now clear; it is hoped that it will revert to heather moorland in years to come. Influential guidebook author Alfred Wainwright voiced strong opposition to the afforestation of Dodd in his Pictorial Guides to the Lakeland Fells in 1962; it took 40 years for his wishes to come true. Height The fell has a height of 502 metres, though the Ordnance Survey's 1:50,000 ''Landranger'' series marks a spot height of 491 metres. This height in fact refers to a point ... [...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] |
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] |
Clints Crags
Clints Crags is a small fell in the north of the English Lake District near Blindcrake, Cumbria. It has its own chapter in Alfred Wainwright's ''The Outlying Fells of Lakeland''. He describes a circular walk from Blindcrake, and laments that at the time of writing (1974): "This is a walk on public footpaths, but until somebody removes the barbed wire and other obstacles to legitimate progress it can be recommended only to gymnasts." It reaches . Since the time of writing the barbed wire has been removed and the path to the summit is clear of obstructions. Clints Crags offers a pleasant and easy stroll to the summit from the village of Blindcrake. The gradient of the crags is much steeper rising north out of the Isel valley, however there are no footpaths to the crags from the valley bottom. There is an old limestone quarry near the summit of the hill, this is now an SSSI, being home to a rare species of newt that breeds in the old quarry lakes. The summit is a large expanse o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bassenthwaite Hill
Bassenthwaite is a village and civil parish in the borough of Allerdale in Cumbria, historically part of Cumberland, within the Lake District National Park, England. According to the 2001 census it had a population of 412, increasing to 481 at the 2011 Census. There is a Church of England Church, St John's Bassenthwaite and a tiny Methodist chapel. The village contains many elements of the archetypal English village including a green, primary school and a stream that runs through it. Bassenthwaite is at the foot of Skiddaw, one of the highest mountains in England at . Robin Hood, Skiddaw, Ullock Pike, Longside Edge and Barf can be seen from the village. Location Bassenthwaite is approximately from Bassenthwaite Lake, east of Cockermouth, north of Keswick, south of Carlisle and west of Penrith. Toponymy The name 'Bassenthwaite' is derived from an Old Norse name meaning ''Bastun's clearing''. The 1st element is usually taken to be the Anglo-French nickname or s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Caer Mote
Caer Mote is a hill of in the north of the English Lake District near Bothel, Cumbria. Its summit lies just outside the boundary of the Lake District National Park and offers a view of Bassenthwaite Lake. Under the name Caermote Hill it is the subject of a chapter of Wainwright's book ''The Outlying Fells of Lakeland''. Wainwright's route is an ascent from Bothel to the northern summit St. John's Hill at , ''Source for height of St. John's Hill'' continuing south to the main summit and south east to meet a minor road beside the Roman fort and follow that road north for an anticlockwise circuit. In his original book Wainwright lists the height as 920 feet (280 m), but in the 2011 2nd edition Chris Jesty corrects this to 948 feet. There is an ancient earthwork enclosure of undetermined age, known as "The Battery" on the northern summit, St. John's Hill. There are traces of a 1st-century AD Roman fort below the hill, to the south east. Caermote Hill is listed by the Datab ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Latrigg (Over Water)
Latrigg is one of the lowest fells in the Lake District in North West England, but is a popular climb due to its convenient location overlooking the town of Keswick and the beautiful views down the valley of Borrowdale from the summit. It is the least mountainous of the Skiddaw fells, the summit being almost entirely devoid of rock. The slopes of Latrigg are partially wooded, and logging work is currently being undertaken. One lone tree just south of the summit is prominently viewed in silhouette when approaching Keswick from the west along the A66. It also has petrified trees on top. Topography Latrigg is the most southerly top of the Skiddaw massif and of the Northern Fells as a whole. It takes the form of a rounded hump at the terminus of a long descending ridge, and would be unremarkable if not for its location. To the north of Latrigg summit is an unnamed depression at about and rising beyond is a grassy rigg, climbing up to Jenkin Hill and the top of Skiddaw Little M ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Binsey
Binsey is a hill on the northern edge of the Lake District in Cumbria, England. It is detached from the rest of the Lakeland hills, and thus provides a good spot to look out at the Northern and North Western Fells of the Lake District, as well as the coastal plain and, across the Solway Firth, Scotland. Snaefell on the Isle of Man is also visible on a clear day. It is the northernmost of the Wainwrights. Topography Binsey stands on the otherwise low-level watershed separating the catchments of the Ellen to the north and the Derwent to the south. A slight ridge connects it to Great Cockup in the main massif of the Northern Fells, two miles to the south east. Binsey itself has a rounded form, but somehow manages to impress the eye more than the similar Great Mell Fell and Little Mell Fell. The ‘pudding basin’ shape holds all around Binsey except to the north west where a ridge descends over Whitas Park to a depression containing the remains of a Roman fort. Beyond is St John ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Souther Fell
Souther Fell is a fell in the English Lake District. It stands to the south of Mungrisdale village in the Northern Fells. It is most famous for the appearance of a "spectral army", said to have been seen marching along its crest on Midsummer's Day, 1745. No such force was in the District at the time. Topography Souther Fell is the eastern extremity of Blencathra, a continuation of the arm that runs down from the summit over Doddick Fell and Scales Fell. A smooth slope falls eastward from Scales Fell to the col of Mousthwaite Comb at . The ridge then turns northeast for two miles along the summit of Souther Fell. Mousthwaite Comb is a geographical oddity. To the north of the depression, running eastward, is the River Glenderamackin. To the south of the col, flowing westward, is the same river. In the intervening time the Glenderamackin has run for six miles, surrounding Souther Fell on three sides like a moat. The Comb provides its only dryshod connection to other ground and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bannerdale Crags
Bannerdale Crags is a fell in the English Lake District. It stands between Blencathra and Bowscale Fell in the Northern Fells. Topography Bannerdale Crags is a ridge running north west to south east. The name was originally applied purely to the steep north eastern flank, but is now generally given to the fell as a whole. Wainwright, Alfred: ''A Pictorial Guide to the Lakeland Fells,Book 5 The Northern Fells'': A broad convex slope descends northward from Blencathra's Atkinson Pike top, gradually resolving into two ridges. The western arm continues to Mungrisdale Common while the north eastern limb, flecked with outcropping rock, falls to a steep sided col at . From the depression Blackhazel Beck descends north west to join the River Caldew while the source of the Glenderamackin lies on the opposite slope. Across the col smooth slopes rise once more up the south western flank of the Bannerdale Crags ridge. There is little clue here to the wall of crags on the other side. The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
