Longsleddale
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Longsleddale
Longsleddale () is a valley and civil parish in the South Lakeland district of the English county of Cumbria. It includes the hamlet of Sadgill. The parish has a population of 73. As the population taken at the 2011 Census was less than 100, details are maintained in the civil parish of Whitwell and Selside. The valley is bounded to the west by Kentmere Pike and Shipman Knotts, one arm of the ''Kentmere Horseshoe'', and to the east by Sleddale Fell and its summits of Grey Crag and Tarn Crag; one of several Cumbrian hills named Great Howe is on the east of the valley above Sadgill. The River Sprint starts on the slopes of Harter Fell and Branstree, and flows south through the valley before joining the River Kent to the north of the town of Kendal. Half-way between Garnett Bridge and Sadgill, Ubarrow Hall is a mediaeval pele tower, reduced in height, adjoining a 17th-century farmhouse. Haweswater aqueduct The aqueduct carrying water from Haweswater Reservoir to Heaton Park R ...
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Tarn Crag (Far Eastern Fells)
Tarn Crag is a fell in the English Lake District. It stands to the east of Longsleddale in the Far Eastern Fells. Topography North of Sadgill, the valley of Longsleddale narrows considerably with walls of crag on either side, the most prominent feature on the eastern side being Buckbarrow Crag. Above this and set back out of sight from the valley is a second tier of rock, Tarn Crag. Being near to the summit, this has given its name to the fell as a whole. Tarn Crag is generally held to mark the transition from Lakeland to Pennine country. Away from the fierce western flank, the fell falls in long easy slopes of coarse grass and heather, with little outcropped rock in evidence. The northern boundary of the fell is formed by the walkers pass from Longsleddale to Mosedale, which crosses a marshy depression at 1,555 ft. Mosedale beck has its source here, beginning its long journey north east to Swindale. Beyond the depression the ground rises again northward up Selside Brow t ...
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Harter Fell, Mardale
Harter Fell is a fell in the far eastern part of the England, English Lake District. The summit at lies the meeting point of three ridges, and Harter Fell forms the head of three valleys: Mardale, Longsleddale and the valley of the River Kent. Topography In plan section the summit area forms a horseshoe, open to the south east. This ridge is narrow and grassy, with a relatively new fence in place. There are subsidiary tops on both horns of the horseshoe. The southern ridge passes over The Knowe and then Brown Howe, before connecting to Kentmere Pike. The eastern branch includes the rocky top of Little Harter Fell (2,234 ft), and Adam Seat (2,185 ft) which is marked by a prominent boundary stone. This ridge continues down to Gatescarth Pass before rising again to Branstree. Connecting to the centre of the summit horseshoe, producing a shape not unlike a tuning fork in plan, is Harter Fell's third ridge. This starts lower down the fell-side and cannot be seen from the s ...
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Shipman Knotts
Shipman Knotts is a fell in the English Lake District in Cumbria, England. It reaches a height of and is situated in one of the quieter areas of the national park, north-east of Kentmere village. Although not one of the best-known Lake District fells (and strictly speaking it is just the southern shoulder of Kentmere Pike), it earned a separate chapter in Alfred Wainwright’s Pictorial Guide to the Lakeland Fells due to ''“Its characteristic roughness . . . rocky outcrops are everywhere on its steep slopes”''. Topography The ridge from Shipman Knotts to Kentmere Pike climbs due north as far as the cairned top of Goat Scar (), before turning north-west to reach the summit of Kentmere Pike. A dry-stone wall follows the ridge, although in places it zigzags abruptly off the watershed. The eastern face above Longsleddale is steeper and includes Rough Crags and Goat Scar itself. The western face is rough but, after the initial climb out of Kentmere, has shallower gradients. The ...
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Grey Crag
Grey Crag is a fell in the English Lake District. It stands to the east of Longsleddale in the Far Eastern Fells. Topography North of Sadgill, the valley of Longsleddale narrows considerably with walls of crag on either side. Grey Crag is the first fell encountered above the eastern side, although the top is not visible from below. What is in sight is a short flat-topped spur at a height of around 1,600 ft which juts out southwards from the body of the fell. This is Great Howe, and its steep flanks provide the east wall of Longsleddale, together with further outcrops above the side valley of Stockdale. Grey Crag proper is a second tier of crags, set back from Great Howe and just below the summit, thus giving its name to the entire fell. Grey Crag is the focus of an extensive ridge system stretching out eastwards to the distant Lune and Eden Valleys. Grey Crag lies on the main watershed of the Cumbrian hills, its runoff reaching the sea at both the Solway Firth and Mor ...
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Branstree
Branstree is a fell in the Far Eastern part of the English Lake District. It overlooks the valley of Mardale and Haweswater Reservoir. Topography A circuit of high fells surrounds the head of Mardale, beginning at High Raise in the north and curving around over High Street and Harter Fell to Branstree and Selside Pike in the south. As the ridge is travelled in this direction, the countryside changes from crag and scree to more rounded fellsides clothed with grass. Branstree is the first fell moving east where grass prevails, and a Pennine character begins to take over from Lakeland. From many directions the fell appears as a smooth domed hill with a wide top. Branstree has a connection southwestward to Harter Fell: the ridge crosses Gatescarth Pass (1,900 ft) which was the route of pedestrian traffic between Mardale and Longsleddale, its well-graded zig-zags still used by walkers today. The ancient trade between the two valleys ended when the level of Haweswater was ...
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Kentmere Pike
Kentmere Pike is a fell in the English Lake District, rising between the valleys of Kentmere and Longsleddale. It is the highpoint on the ridge between Harter Fell and Shipman Knotts. Topography The western Kentmere slopes fall over the rough ground of Hallow Bank Quarter to Ullstone Gill, a tributary of the River Kent. Beyond here Smallthwaite Knott, an outlier of Harter Fell, separates Kentmere Pike from the main valley. There is extensive evidence of former quarrying on this flank. By contrast the Longsleddale side wears a rim of crag above the narrow upper course of the River Sprint. Goat Scar, Raven Crag and Brown Crags are the main faces, while Steel Pike appears from the valley bridleway as an independent rocky peak. The remains of the large Wrengill Quarry are just north of here, together with a mine entrance a little higher up the slope. The ridge northwards to Harter Fell drops to a wet depression and then climbs up the grassy ridge, following first the wall and the ...
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River Sprint
The River Sprint is a river in Cumbria, England with its source high up on the south-facing side of Harter Fell. It flows into the River Kent just to the south of Burneside. The first two miles of the river is made up of a series of short flat sections interspersed by spectacular water falls, before it enters Longsleddale valley. When in Longsleddale, it begins to get wider as it is fed by a large number of streams (known as becks; a term derived from Old Norse). The River Sprint is the fastest rising river in England, and frequently floods in Longsleddale valley, making the road impassable. The river is spectacular at times of high flow, and is popular with canoeists and fishermen. Industry The river powered mills from medieval times to the twentieth century There were mills at Garnett Bridge and downstream at Sprint Mill near Burneside. Ecology Like other tributaries of the Kent, the Sprint is a stronghold of the white clawed crayfish, one of the reasons for the desi ...
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Kentmere
Kentmere is a valley, village and civil parish in the Lake District National Park, a few miles from Kendal in the South Lakeland district of Cumbria, England. Historically in Westmorland, at the 2011 census Kentmere had a population of 159. Geography The narrow valley spans about in length and begins with a bowl of hills known as the Kentmere Round; a horseshoe of high fells which surrounds Kentmere Reservoir. The River Kent, which gives Kendal its name, begins from Hall Cove, a corrie at the head of the valley, before flowing through the reservoir. Access to this part of the valley is available via the Roman High Street, over Nan Bield Pass, from Troutbeck over Garburn Pass ( Bridleway only. No motor vehicles), or along an old bridleway up from the village. The valley is sandwiched between Troutbeck on the west side and Longsleddale on the east. It can be reached by road only by travelling through the village of Staveley, which sits at its mouth where the river me ...
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Lancaster And Carlisle Railway
The Lancaster and Carlisle Railway was a main line railway opened between those cities in 1846. With its Scottish counterpart, the Caledonian Railway, the Company launched the first continuous railway connection between the English railway network and the emerging network in central Scotland. The selection of its route was controversial, and strong arguments were put forward in favour of alternatives, in some cases avoiding the steep gradients, or connecting more population centres. Generating financial support for such a long railway was a challenge, and induced the engineer Joseph Locke to make a last-minute change to the route: in the interests of economy and speed of construction, he eliminated a summit tunnel at the expense of steeper gradients. The sparseness of the population discouraged the addition of branch lines, with a small number of exceptions, although several east-west secondary routes made independent connection to the route. Establishing a joint station at Carl ...
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Outdoor Activities
Outdoor recreation or outdoor activity refers to recreation done outside, most commonly in natural settings. The activities that encompass outdoor recreation vary depending on the physical environment they are being carried out in. These activities can include fishing, hunting, backpacking, and horseback riding — and can be completed individually or collectively. Outdoor recreation is a broad concept that encompasses a varying range of activities and landscapes. Outdoor recreation is typically pursued for purposes of physical exercise, general wellbeing, and spiritual renewal. While a wide variety of outdoor recreational activities can be classified as sports, they do not all demand that a participant be an athlete. Rather, it is the collectivist idea that is at the fore in outdoor recreation, as outdoor recreation does not necessarily encompass the same degree of competitiveness or rivalry that is embodied in sporting matches or championships. Competition generally is les ...
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Rock Climbing
Rock climbing is a sport in which participants climb up, across, or down natural rock formations. The goal is to reach the summit of a formation or the endpoint of a usually pre-defined route without falling. Rock climbing is a physically and mentally demanding sport, one that often tests a climber's strength, endurance, agility and balance along with mental control. Knowledge of proper climbing techniques and the use of specialized climbing equipment is crucial for the safe completion of routes. Because of the wide range and variety of rock formations around the world, rock climbing has been separated into several different styles and sub-disciplines, such as scrambling, bouldering, sport climbing, and trad (traditional) climbing another activity involving the scaling of hills and similar formations, differentiated by the rock climber's sustained use of hands to support their body weight as well as to provide balance. Rock climbing competitions have the objectives of ...
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Caving
Caving – also known as spelunking in the United States and Canada and potholing in the United Kingdom and Ireland – is the recreational pastime of exploring wild cave systems (as distinguished from show caves). In contrast, speleology is the scientific study of caves and the cave environment.Caving in New Zealand
(from Te Ara: The Encyclopedia of New Zealand, Accessed 2012-11.)
The challenges involved in caving vary according to the cave being visited; in addition to the total absence of light beyond the entrance, negotiating pitches, squeezes,
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