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Borrowdale At Dusk
Borrowdale is a valley and civil parishes in England, civil parish in the Lake District, English Lake District in the Allerdale, Borough of Allerdale in Cumbria, England. It lies within the Historic counties of England, historic county boundaries of Cumberland, England, Cumberland. It is sometimes referred to as ''Cumberland Borrowdale'' to distinguish it from Borrowdale, Westmorland, another Borrowdale in the historic county of Westmorland. Geography The valley rises in the central Lake District, and runs north carrying the River Derwent, Cumbria, River Derwent into the lake of Derwentwater. The waters of the river have their origins over a wide area of the central massif of the Lake District north of Esk Hause and Stake Pass. These origins include drains from the northern end of Scafell, Great End, the eastern side of the Dale Head massif, the western part of the Central Fells and all the Glaramara ridge. Near Rosthwaite, Borrowdale, Cumbria, Rosthwaite the side valley of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Allerdale
Allerdale is a non-metropolitan district of Cumbria, England, with borough status. Its council is based in Workington and the borough has a population of 93,492 according to the 2001 census, increasing to 96,422 at the 2011 Census. The Borough of Allerdale was formed under the Local Government Act 1972, on 1 April 1974 by the merger of the municipal borough of Workington, the urban districts of Maryport, Cockermouth and Keswick; and the rural districts of Cockermouth and Wigton, all of which were within the administrative county of Cumberland. In 1995 Allerdale was granted borough status. The name derives from the ancient region of Allerdale, represented latterly by the two wards of Cumberland, called Allerdale-above-Derwent and Allerdale-below-Derwent, the present borough corresponding largely to the latter with parts of the former. Much of the area during the medieval period was a royal forest subject to forest law. In July 2021 the Ministry of Housing, Communities an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dale Head
Dale Head is a fell in the north-western sector of the Lake District, in northern England. It is 753 metres or 2,470 feet above sea level and stands immediately north of Honister Pass, the road between Borrowdale and Buttermere. 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. Dale Head is the highest fell in the southern sector. Dale Head is the apex of two hill ridges. The principal ridge descends from Dale Head to the north-east and forms several other fells, each given a chapter by Alfred Wainwright in his Pictorial Guides to the Lakeland Fells. These are High Spy, Maiden Moor and Catbells (alternative spelling, Cat Bells). This ridge forms the western side of Borrowdale and overlooks Derwent Water. The other ridge descends to the north-west and includes the fells o ... [...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] |
Honister Pass
Honister Pass is a mountain pass in the English Lake District. It is located on the B5289 road, linking Seatoller, in the valley of Borrowdale, to Gatesgarth at the southern end of Buttermere. The pass reaches an altitude of , making it one of the highest in the region, and also one of the steepest, with gradients of up to 1-in-4 (25%). The saddle at the watershed is known as Honister Hause, using the Cumbrian word ''hause'' for such a feature. Honister Pass is one of three passes that link the tourist area around Keswick, including Derwent Water and Borrowdale, with the valley of the River Cocker, including the lakes of Buttermere, Crummock Water and Loweswater. From north to south these passes are Whinlatter Pass, Newlands Pass and Honister Pass. Honister Slate Mine and Honister Hause Youth Hostel are located at the summit of the pass. Footpaths lead from the summit of the pass to Fleetwith Pike to the west, Grey Knotts to the south, and Dale Head to the north. Honis ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
B5289 Road
The B5289 is a road in the Lake District, England. It lies in the county of Cumbria, and is an important traffic artery in the Lake District. Route The road starts in Keswick and passes alongside Derwent Water. At the southern end of the lake it enters Borrowdale, passing the settlements of Grange, Rosthwaite and Seatoller. This stretch of road is notable for its views of the surrounding fells, including Catbells and Glaramara. At Seatoller, the road starts its climb up to Honister Pass. This part of the route has many zig-zags, with gradients of 1 in 4 (25%) as it struggles up the 200 metres (600 feet) to the top. The top of the pass is an upland wilderness, with barren slopes and many erratic boulders, that is often covered in snow in the winter. Coming down the other side the road passes the settlement of Gatesgarth and runs alongside the lake of Buttermere before reaching the village of Buttermere. It then runs alongside Crummock Water and through the valley of ... [...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] |
Borrowdale Volcanic Group
The Borrowdale Volcanic Group is a group of igneous rock formations named after the Borrowdale area of the Lake District, in England. They are Caradocian (late Ordovician) in age (roughly 450 million years old). It is thought that they represent the remains of a volcanic island arc, approximately similar to the island arcs of the west Pacific today. This developed as oceanic crust to the (present) north-west and was forced by crustal movement under a continental land-mass to the present south-east. Such forcing under, as two plates meet, is termed subduction. This land-mass has been named Avalonia by geologists. It is now incorporated into England and Wales and a sliver of North America. Geology At that time the rocks that now comprise most of Scotland (and part of the northern Irish landmass) were not attached to Avalonia. They were separated by an ocean, called the Iapetus Ocean by geologists. The line of joining, or suture, is approximately under the Solway Firth and Cheviot ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Great Gable
Great Gable is a mountain in the Lake District, United Kingdom. It is named after its appearance as a pyramid from Wasdale, though it is dome-shaped from most other directions. It is one of the most popular of the Lakeland fells, and there are many different routes to the summit. Great Gable is linked by the high pass of Windy Gap to its smaller sister hill, Green Gable, and by the lower pass of Beck Head to its western neighbour, Kirk Fell. Topography The Western Fells occupy a triangular sector of the Lake District, bordered by the River Cocker to the north east and Wasdale to the south east. Westwards, the hills diminish toward the coastal plain of Cumbria. At the central hub of the high country are Great Gable and its satellites, while two principal ridges fan out on either flank of Ennerdale, the western fells forming a horseshoe around this valley.Alfred Wainwright: ''A Pictorial Guide to the Lakeland Fells, Volume 7 The Western Fells'': Westmorland Gazette (1966): Gr ... [...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] |
Walla Crag
Walla Crag is a fell in the English Lake District, near Keswick. The fell is a short walk from Keswick and overlooks Derwentwater. Topography The crag is the terminal cliff on a short ridge running north west from Bleaberry Fell, dropping about 400 ft from the plateau above. Below this are further steep slopes before the gradient slackens on the shore of Derwentwater. The face is heavily wooded — mainly with conifers — almost to the top. The trees continue down through Great Wood to the lake. Walla Crag has one major breach, Lady's Rake. The summit lies a little way back from the brink, the smooth heather-clad hinterland then dropping to the broad depression of Low Moss. Beyond here the ground rises again to Bleaberry Fell. The southern boundary of the fell is formed by Cat Gill, which flows west from Loss Moss to the lake. The gill separates Walla Crag from the neighbouring Falcon Crag, popular with rock climbers. Brockle Beck flows north from Low Moss, before turnin ... [...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] |
Catbells
Cat Bells is a fell in the English Lake District in the county of Cumbria. It has a height of and is one of the most popular fells in the area. It is situated on the western shore of Derwentwater within of the busy tourist town of Keswick. Its distinctive shape catches the attention of many visitors to the Lakes who feel compelled to climb to the summit after seeing it from the viewpoint of Friars' Crag on the opposite side of Derwentwater. The Lake District writer and walker Alfred Wainwright acknowledges the popularity of Cat Bells among fellwalkers of all abilities by saying: Name The fell's unusual name may well have come from a distortion of "Cat Bields" meaning shelter of the wild cat, although this is not certain. The fell's name is sometimes written as Catbells. Topography Cat Bells is the last fell on the ridge separating Derwentwater from the Newlands valley. It rises due south from Hawse End, reaching the summit in two distinct steps. The lower top is named Skelgi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
