98-729: The A591 is a major road in Cumbria, which lies almost entirely within the Lake District national park. A 2009 poll by satellite navigation firm Garmin named the stretch of the road between Windermere and Keswick as the most popular road in Britain. The 29.8 mile stretch between Kendal and Keswick was also named the UK's best driving road, according to a specially devised driving ratio formulated by car rental firm Avis . The road begins (at its southern end) 3.5 miles (5.6 km) north-west of junction 36 of
196-732: A box of trunk routes and major A roads. It is flanked to the east by the A6 road , which runs from Kendal to Penrith (though the National Park extension approved in 2015 is east of the A6); across its southern fringes by the A590 , which connects the M6 to Barrow-in-Furness, and the A5092 , and across its northern edge by the A66 trunk road between Penrith and Workington . The A595 (linking
294-457: A circular walk from Patterdale: up Striding Edge, down to Grisedale Tarn and back over St Sunday Crag . Helvellyn is a popular area for winter climbing in the Lake District. The steep headwall above Red Tarn contains several graded routes, clustered around the prow-shaped buttress on the right-hand side of the face, known to climbers as Viking Buttress, and in a couple of gullies which lead to
392-436: A further 200 days with some rain, and 145 completely dry days. Hill fog is common at any time of year, and the fells average only around 2.5 hours of sunshine per day, increasing to around 4.1 hours per day on the coastal plains. The Lake District is home to a great variety of wildlife, because of its varied topography, lakes, and forests. It provides a home for the red squirrel and colonies of sundew and butterwort , two of
490-468: A general " right to roam " in open country, which includes approximately 50% of the national park. Many of these tracks arose centuries ago and were used either as ridge highways (such as along High Street ) or as passes for travelling across the ridges between settlements in the valleys. Historically these paths were not planned for reaching summits, but more recently they are used by fell walkers for that purpose. The Coast to Coast Walk , which crosses
588-403: A leat was constructed to capture the water of Helvellyn Gill, so that it is now directed into the reservoir. A never-failing spring called Brownrigg Well exists 90 m (300 ft) below the summit of Helvellyn, about 500 m (550 yd) due west of the highest point, at the head of Whelpside Gill. In the nineteenth century a leat was constructed to direct the water of this spring into
686-514: A length of 11 miles (18 km) and an area of 5.69 square miles (14.73 km ) is the longest and largest lake in England, and Wast Water , which at 79 metres (259 ft) is the deepest lake in England. The Lake District National Park was established in 1951, and covers an area of 2,362 km (912 square miles), the bulk of the region. It was designated a UNESCO World Heritage Site in 2017. The Lake District National Park includes all of
784-415: A scramble on Eagle Crag, or this part can be bypassed by taking the path to Nethermost Cove before joining the ridge. From Patterdale a long but safe and easy walk ( 11.5 km or 7 + 1 ⁄ 4 mi) on a good path follows the track up Grisedale to the tarn, and then takes the old pony track up the south ridge of Helvellyn. The second part of this walk takes a safe route well away from crags on
882-582: A species of whitefish found in only four bodies of water in the Lake District. A second reservoir was built around 1860 in Brown Cove, between Swirral Edge and Lower Man, along with one further down the valley in Keppel Cove. These provided water to generate hydroelectric power for the lead mine. The dam in Keppel Cove is still in place, but water now leaks through its base. The remains of the dam in Brown Cove can be seen, but again water leaks freely through it. It
980-430: A system of permits operates on Gatescarth Pass . Most of the land within the national park is in private ownership, with about 55% registered as agricultural land. Landowners include: The Lake District is a roughly circular upland massif , deeply dissected by a broadly radial pattern of major valleys which are largely the result of repeated glaciations over the last 2 million years. The apparent radial pattern
1078-502: A traverse of the full length of the Helvellyn range in either direction, but with a greater sense of climax when starting from the north. Most of the ridge track is a bridleway and so the route can be completed by mountain bike in a challenging six-hour circular route of 16 miles (26 kilometres) off-road and 10 miles (16 kilometres) on-road riding. This may begin (and finish) at Mill Bridge near Grasmere. Helvellyn can also be included in
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#17328449641151176-433: Is England's deepest lake. The Central Fells are lower in elevation than surrounding areas of fell, peaking at 762 m (2,500 ft) at High Raise . They take the form of a ridge running between Derwent Water in the west and Thirlmere in the east, from Keswick in the north to Langdale Pikes in the south. A spur extends southeast to Loughrigg Fell above Ambleside. The central ridge running north over High Seat
1274-508: Is a broad plateau, trending roughly from north-west to south-east for about a kilometre between Lower Man and the start of Striding Edge. Throughout this distance it remains more than 900 m (3,000 ft) high. To the west the ground drops gently at first but then more steeply down to Thirlmere , while on the eastern side three deep glacial coves , each backed by high cliffs, are separated by two spectacular sharp ridges or arêtes . The middle of these coves contains Red Tarn . Like much of
1372-524: Is a cross-shaped stone shelter; to the north is an Ordnance Survey trig point , slightly lower than the summit at 949 m (3,114 ft). The view from the top on a clear day extends across the whole of the Lake District to the Solway Firth and hills of south-west Scotland to the north-west, Cheviot and the Pennine Hills to the north-east, Morecambe Bay, Blackpool and the coast of North Wales to
1470-513: Is a notorious accident spot among hikers and scramblers. In winter conditions the climb from Striding Edge up to the summit plateau can involve crossing steep icy ground and a snow cornice , and can be the most dangerous part of the walk. Without an ice axe or crampons this presents a serious obstacle. In January 2008 two walkers died after falling from the ridge in separate incidents. Another walker died after falling from Striding Edge in May 2008. Over
1568-519: Is called by that name, Bassenthwaite Lake . All the others such as Windermere , Coniston Water , Ullswater and Buttermere are meres, tarns and waters, with mere being the least common and water being the most common. The major lakes and reservoirs in the National Park are given below. Below the tree line are wooded areas, including British and European native oak woodlands and introduced softwood plantations. The woodlands provide habitats for native English wildlife. The native red squirrel
1666-523: Is exceptionally boggy. The Eastern Fells consist of a long north-to-south ridge , the Helvellyn range , running from Clough Head to Seat Sandal with the 950 m (3,118 ft) Helvellyn at its highest point. The western slopes of these summits tend to be grassy, with rocky corries and crags on the eastern side. The Fairfield group lies to the south of the range and forms a similar pattern with towering rock faces and hidden valleys spilling into
1764-468: Is found in the Lake District and a few other parts of England. In parts of the Lake District, the rainfall is higher than in any other part of England. This gives Atlantic mosses , ferns , lichen , and liverworts the chance to grow. There is some ancient woodland in the National Park. Management of the woodlands varies: some are coppiced , some pollarded , some left to grow naturally, and some provide grazing and shelter. The Lake District extends to
1862-572: Is not from a central dome, but from an axial watershed extending from St Bees Head in the west to Shap in the east. Most of these valleys display the U-shaped cross-section characteristic of glacial origin and often contain long narrow lakes in bedrock hollows, with tracts of relatively flat ground at their infilled heads, or where they are divided by lateral tributaries (Buttermere-Crummock Water; Derwent Water-Bassenthwaite Lake). Smaller lakes known as tarns occupy glacial cirques at higher elevations. It
1960-535: Is now the Scottish border during the Caledonian orogeny . The northern central peaks, such as Great Rigg, were produced by considerable lava flows. These lava eruptions were followed by a series of pyroclastic eruptions which produced a series of calderas, one of which includes present-day Scafell Pike. These pyroclastic rocks give rise to the craggy landscapes typical of the central fells. The southeastern band comprises
2058-410: Is particularly narrow in places, so care is needed when driving on it. The road was badly damaged during Storm Desmond on 5 December 2015 including a part washed away at Dunmail Raise and landslip adjacent to Thirlmere. The closed section of road between Grasmere and Legburthwaite reopened on 11 May 2016. While the road was closed a new tarmac path for walkers, cyclists, and horseriders was built to
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#17328449641152156-510: Is the abundance of both which has led to the area becoming known as the Lake District. Many of the higher fells are rocky, while moorland predominates lower down. Vegetation cover in better-drained areas includes bracken and heather , although much of the land is boggy , due to the high rainfall. Deciduous native woodland occurs on many of the steeper slopes below the tree line , but with native oak supplemented by extensive conifer plantations in many areas, particularly Grizedale Forest in
2254-439: Is the starting point for the bridleway to Sticks Pass, from which Helvellyn can be approached along the main ridge track from the north. From Thirlspot two routes lead up Helvellyn. The old pony route took a very safe and steady route for the benefit of early visitors, who took horses and a guide from the inn. The route traverses the flank of White Side to join the ridge at the col just below Lower Man. The other route, known as
2352-405: Is unclear whether there ever was a natural tarn in Brown Cove. Guidebook writers before 1860 refer only to Keppel Cove Tarn to the north of Swirral Edge. A total of five ridges diverge from the summit ridge of Helvellyn at different points. The north-west ridge continues from Lower Man over Browncove Crags, becoming almost insignificant when it reaches the shore of Thirlmere, yet still separating
2450-654: The B5343 . Other valleys such as Little Langdale , Eskdale and Dunnerdale are served by minor roads. The last of these is connected with the first two by the Wrynose and Hardknott passes respectively; both of these passes are known for their steep gradients and are together one of the most popular climbs in the United Kingdom for cycling enthusiasts. A minor road through the Newlands Valley connects via Newlands Hause with
2548-501: The Cumbrian mountains , and for its literary associations with Beatrix Potter , John Ruskin , and the Lake Poets . The Cumbrian mountains, or fells , include England's highest : Scafell Pike (978 m; 3,209 ft), Helvellyn (950 m; 3,120 ft) and Skiddaw (931 m; 3,054 ft). The region also contains sixteen major lakes. They include Windermere , which with
2646-558: The Furness Fells or Coniston Fells, have as their northern boundary the steep and narrow Hardknott and Wrynose passes. The highest are Old Man of Coniston and Swirl How which slightly exceed 800 m (2,600 ft). The third group to the west of the Duddon includes Harter Fell and the long ridge leading over Whitfell to Black Combe and the sea. The south of this region consists of lower forests and knolls, with Kirkby Moor on
2744-616: The Kirkstone Pass . Some valleys which are not penetrated by A roads are served by B roads . The B5289 serves Lorton Vale and Buttermere and links via the Honister Pass with Borrowdale . The B5292 ascends the Whinlatter Pass from Lorton Vale before dropping down to Braithwaite near Keswick. The B5322 serves the valley of St John's in the Vale whilst Great Langdale is served by
2842-427: The Lake District . It bypasses the town of Windermere , closely following the north-eastern bank of Windermere . It then travels through the centre of Ambleside , follows the northern side of Rydal Water , passes White Moss Common, follows the eastern edge of Grasmere and passes the village of Grasmere . The road continues over Dunmail Raise and along the eastern edge of Thirlmere . Shortly afterwards it reaches
2940-569: The Leven Estuary , and the western banks and tidal flats of the Kent Estuary . These areas are each characterised by sand and mudflats of scenic and wildlife interest. The coast is backed by extensive flats of raised marine deposits left when the relative sea level was higher. The Lake District's geology is very complex but well-studied. A granite batholith beneath the area is responsible for this upland massif, its relatively low density causing
3038-651: The Lune Valley . The national park received 18.14 million tourist visitors in 2022. This equates to 29.15 million tourist days, counting visits of greater than three hours. It is the largest of the thirteen national parks in England and Wales and the second largest in the UK after the Cairngorms National Park . Its aim is to protect the landscape by restricting unwelcome change by industry or commerce. The area of
A591 road - Misplaced Pages Continue
3136-471: The M6 motorway at Brettargh Holt roundabout with the A590 road ( 54°16′29″N 2°45′38″W / 54.2746°N 2.7605°W / 54.2746; -2.7605 ( A591 road (southern end) ) ), close to Sizergh Castle . It bypasses the town of Kendal as a dual carriageway , this £1.9m 3-mile (4.8 km) section opened on 29 August 1971. It becomes a busy single carriageway road as it enters
3234-583: The Patterdale valley. It culminates in the height of Red Screes overlooking the Kirkstone Pass . The Far Eastern Fells refers to all of the Lakeland fells to the east of Ullswater and the A592 road running south to Windermere. At 828 m (2,717 ft), the peak known as High Street is the highest point on a complex ridge that runs broadly north-south and overlooks the hidden valley of Haweswater to its east. In
3332-485: The Secretary of State for Environment, Food, and Rural Affairs . The precise extent of the Lake District is undefined, but it is sometimes considered to be slightly larger than that of the National Park, whose total area is about 2,362 square kilometres (912 sq mi). The park extends just over 51 kilometres (32 mi) from east to west and nearly 64 kilometres (40 mi) from north to south, with areas such as
3430-598: The Skiddaw Group and include the rocks traditionally known as the Skiddaw Slates . Their friability generally leads to mountains with relatively smooth slopes such as Skiddaw itself. The central band is a mix of volcanic and sedimentary rocks of mid-to-late Ordovician age comprising the lavas and tuffs of the Borrowdale Volcanic Group , erupted as the former Iapetus Ocean was subducted beneath what
3528-544: The gill to its north to serve the needs of the Helvellyn Mine further down. This leat has now fallen into disuse. The gill it led to is not named on any map, but some authors have referred to it as Mines Gill. Whelp Side, between Whelpside Gill and Mines Gill, appears as a distinct shoulder of the mountain when seen from the west, largely grassy though with a few crags and boulders in places, and with coniferous plantations on its lower slopes which were planted to stabilise
3626-526: The "Cumbrian Mountains", "Cumbrian Fells" or "Lakeland Fells". The four highest fells exceed 3,000 feet (914 m). These are: The Northern Fells are a clearly defined range of hills contained within a 13 km (8 mi) diameter circle between Keswick in the southwest and Caldbeck in the northeast. They culminate in the 931 m (3,054 ft) peak of Skiddaw . Other notable peaks are Blencathra (also known as Saddleback) (868 m (2,848 ft)) and Carrock Fell . Bassenthwaite Lake occupies
3724-661: The A66 with the A5092) forms the park boundary from Calder Bridge to Holmrook, then crosses the coastal plain of the park until turning inland at the Whicham Valley, forming much of the park boundary again until joining the A5092 at Grizebeck. Besides these, a few A roads penetrate the area itself, notably the A591 which runs north-westwards from Kendal to Windermere and then on to Keswick. It continues up
3822-729: The August Bank Holiday weekend in 2017, Patterdale Mountain Rescue attended a fatal fall from Striding Edge on the Saturday and helped rescue a seriously injured walker and his dog on the Sunday. Swirral Edge offers a shorter but equally exciting scramble along a similar sharp arête. The main path to it comes up from Red Tarn, which is linked by a surprisingly level path to Hole-in-the-Wall, making this ridge equally accessible from Patterdale as from Glenridding. The ridge walk can be extended to include
3920-572: The B5289 at Buttermere. Wasdale is served by a cul-de-sac minor road, as is Longsleddale and the valleys at Haweswater and Kentmere . There are networks of minor roads in the lower-lying southern part of the area, connecting numerous communities between Kendal, Windermere, and Coniston. The West Coast Main Line skirts the eastern edge of the Lake District and the Cumbrian Coast Line passes through
4018-505: The English Lake District , the highest point of the Helvellyn range , a north–south line of mountains to the north of Ambleside , between the lakes of Thirlmere and Ullswater . Helvellyn is the third-highest point both in England and in the Lake District , and access to Helvellyn is easier than to the two higher peaks of Scafell Pike and Scafell . The scenery includes three deep glacial coves and two sharp-topped ridges on
A591 road - Misplaced Pages Continue
4116-446: The Helvellyn summit plateau. This starting point is accessible from both Glenridding and Patterdale. Hole-in-the-Wall used to be a prominent gap in the stone wall on the top of the ridge where a gate was missing. Today the gap has been filled in and a ladder stile crosses the wall. From here the initial part of the ridge is relatively rounded and has a solid path running along the right-hand side. This changes upon reaching High Spying How,
4214-689: The Lake District Peninsulas to the south lying outside the National Park. There are only a few major settlements within this mountainous area: the towns of Keswick ; Windermere and Bowness-on-Windermere (which are contiguous); and Ambleside, are the three largest. The economies of all these are heavily dependent on tourism. Significant settlements close to the boundary of the national park include Carlisle , Barrow-in-Furness , Kendal , Ulverston , Dalton-in-Furness , Whitehaven , Workington , Cockermouth , Penrith , Millom and Grange-over-Sands ; each of these has important economic links with
4312-511: The Lake District is generally very windy: the coastal areas have 20 days of gales, and the fell tops around 100 days of gales per year. The maritime climate means that the Lake District has relatively moderate temperature variations throughout the year. The mean temperature in the valleys ranges from about 3 °C (37 °F) in January to around 15 °C (59 °F) in July. (By comparison, Moscow , at
4410-440: The Lake District. They can be regarded as comprising a northern grouping between Wasdale, Eskdale, and the two Langdale valleys, a southeastern group east of Dunnerdale and south of Little Langdale, and a southwestern group bounded by Eskdale to the north and Dunnerdale to the east. The first group includes England's highest mountains: Scafell Pike in the centre, at 978 m (3,209 ft) and Scafell one mile (1.6 km) to
4508-550: The White Stones Route, originally marked by stones painted white, crosses the fellside at a lower level and fords Helvellyn Gill to join the path from Swirls. Swirls is the start of the most direct route to the top of Helvellyn, "the modern pedestrian highway" which has been paved where necessary. It zigzags up the fellside above Helvellyn Gill, over Browncove Crags and joins the main ridge at Lower Man. Several possible routes begin at Wythburn church . A bridleway winds up
4606-540: The area to be "buoyed up". The granite can be seen at the surface as the Ennerdale, Skiddaw, Carrock Fell, Eskdale, and Shap granites. Broadly speaking the area can be divided into three bands, divisions which run southwest to the northeast. Generally speaking, the rocks become younger from the northwest to the southeast. The northwestern band is composed of early to mid- Ordovician sedimentary rocks , largely mudstones and siltstones of marine origin. Together they comprise
4704-558: The area, which consists of the High Stile ridge north of Ennerdale, the Loweswater Fells in the far northwest, the Pillar group in the southwest, and Great Gable (899 m (2,949 ft)) near Sty Head. Other tops include Seatallan , Haystacks and Kirk Fell . This area is craggy and steep, with the impressive pinnacle of Pillar Rock its showpiece. Wastwater , located in this part,
4802-410: The area. Other villages are Coniston , Threlkeld , Glenridding , Pooley Bridge , Broughton-in-Furness , Grasmere , Newby Bridge , Staveley , Lindale , Gosforth and Hawkshead . Beyond these are a scattering of hamlets and many isolated farmsteads, some of which are still tied to agriculture; others now function as part of the tourist economy. The Lake District is very nearly contained within
4900-541: The boundaries of the national park (and additionally Drigg , about a third of a mile from the park boundary). The line gives railway enthusiasts and others a flavour of a pre- Beeching railway line, with features like manually operated level crossing gates, as well as giving a good connection to the steam railway into Eskdale and providing access for cyclists and serious walkers to the Western Fells. The narrow gauge Ravenglass and Eskdale Railway runs from Ravenglass on
4998-645: The central Lake District, though the town of Kendal , some coastal areas and the Cartmel and Furness peninsulas are outside the park boundary. The area was designated a national park on 9 May 1951, a month after the Peak District , the first UK national park. It retained its original boundaries until 2016, when it was extended by 3% to the east, in the direction of the Yorkshire Dales National Park , to incorporate areas land of high landscape value around
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#17328449641155096-600: The coast of the Irish Sea from Drigg in the north to Silecroft in the south, encompassing the estuaries of the Esk and its tributaries, the Irt and the Mite . The intertidal zone of the combined estuaries includes sand, shingle and mudflats, and saltmarsh . The dune systems on either side of the estuary are protected as nature reserves; Drigg Dunes and Gullery to the north and Eskmeals Dunes to
5194-624: The east side of Bassenthwaite Lake . "The A591, Grasmere, Lake District" was short-listed in the 2011 Google Street View awards in the Most Romantic Street category. The A593 and A5084 link the Ambleside and Coniston areas with the A590 to the south whilst the A592 and A5074 similarly link Windermere with the A590. The A592 also continues northwards from Windermere to Ullswater and Penrith by way of
5292-442: The eastern side (Striding Edge and Swirral Edge). Helvellyn was one of the earliest fells to prove popular with walkers and explorers; beginning especially in the later 18th century. Among the early visitors to Helvellyn were the poets Samuel Taylor Coleridge and William Wordsworth , both of whom lived nearby at one period. Many routes up the mountain are possible so that it may be approached from all directions. However, traversing
5390-534: The edges of these Ordovician and Silurian rocks on the northern, eastern, and southern fringes of the area is a semi-continuous outcrop of Carboniferous Limestone seen most spectacularly at places like Whitbarrow Scar and Scout Scar . The Lake District's location on the northwest coast of England, coupled with its mountainous geography, makes it the wettest part of England. The UK Met Office reports average annual precipitation of more than 2,000 mm (80 in), but with considerable local variation. Although
5488-452: The entire region receives above-average rainfall, there is a wide disparity between the amounts of rainfall in the western and eastern lakes, as the Lake District experiences relief rainfall . Seathwaite, Borrowdale is the wettest inhabited place in England with an average of 3,300 mm (130 in) of rain a year, while nearby Sprinkling Tarn is even wetter, recording over 5,000 mm (200 in) per year; by contrast, Keswick, at
5586-440: The fellside, over Comb Crags and traverses the slopes of Nethermost Pike to arrive on the ridge at Swallow Scarth, the col just below Helvellyn. Other routes from Wythburn follow Comb Gill or Whelpside Gill, or Middle Tongue between these two gills. The shortest route of all follows the gill past the old lead mine, perhaps better used as a descent. Wainwright warned walkers with weak ankles to avoid it. Helvellyn may be included in
5684-409: The few carnivorous plants native to Britain. The Lake District is a major sanctuary for the red squirrel and has the largest population in England (out of the estimated 140,000 red squirrels in the United Kingdom, compared with about 2.5 million grey squirrels ). Helvellyn Helvellyn ( / h ɛ l ˈ v ɛ l ɪ n / ; possible meaning : pale yellow moorland ) is a mountain in
5782-442: The final rock tower to rejoin the path. At this point the ridge connects with the main Helvellyn massif. Reaching the summit plateau involves a steep walk or scramble up about 80 m (260 ft) of rough rocky terrain, known as The Abyss by W. A. Poucher , author of a popular series of mountain guide books between 1940 and the late 1960s. From the top of this climb the summit is only 200 m (220 yd) away. Striding Edge
5880-456: The form of a broad plateau , sloping gently to the south-west, but dropping abruptly to the north-east into Red Tarn cove. So smooth and large is this summit that a small aeroplane was able to land on it in 1926 (see History below). The highest point, 950 m (3,120 ft) above sea level, is the top of a small rocky knoll, marked by a loose cairn. In former times this knoll used to be known as Helvellyn High Man (or Higher Man.) Nearby there
5978-685: The generally lower southern part of the area. The Lake District extends to the sea to the west and south. The highest mountain in England, Scafell Pike (978 m or 3209 feet), has a far-reaching view on a clear day, ranging from the Galloway Hills of Scotland, the Mourne Mountains in Northern Ireland, the Isle of Man, and Snowdonia in Wales. The mountains (or ' fells ') of the Lake District are known as
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#17328449641156076-468: The gills and shoulders on the west side of the range. Walkers can choose between many routes. In January 2018 Helvellyn was named 'Britain's Best Walk' in an ITV show presented by Julia Bradbury . Striding Edge is a popular route which involves some scrambling , linking the summit ridge of Birkhouse Moor to Helvellyn's summit by what becomes a sharp arête . Striding Edge begins at Hole-in-the-Wall and then stretches for over 1.5 km (1 mi) to
6174-523: The head of Windermere - Grasmere, Great Langdale and Little Langdale, and the Coniston Water valley. The valleys break the mountains up into blocks, which have been described by various authors in different ways. The most frequently encountered approach is that made popular by Alfred Wainwright who published seven separate area guides to the Lakeland Fells. Only one of the lakes in the Lake District
6272-449: The highest point on the ridge — 863 m (2,831 ft). At this point a narrow path continues close to the top of the ridge, which becomes increasingly narrow, and scramblers will often follow the very top of the arête. The path on the right-hand side continues until near the end of the ridge where it switches over to the left-hand side. Scramblers who continue on the top of the ridge are forced to descend an awkward short gully down from
6370-491: The land around the reservoir. North of Mines Gill are the Helvellyn Screes, a more craggy stretch of hillside, beneath the north-west ridge, with a loose scree covering in places. The deep coves on the rocky eastern side of Helvellyn drain into Ullswater . Water from Brown Cove and Red Tarn unite below Catstye Cam to form Glenridding Beck, which flows through Glenridding village to the lake, while Nethermost Cove drains into
6468-504: The landforms seen today. Since the end of the last ice age, small populations of arctic-alpine plants have survived in favourable spots on rock ledges high in the eastern coves. Rare to Britain species of alpine butterfly, the mountain ringlet , also live on and around Helvellyn. Mineral veins , some with deposits of the lead ore galena , do exist within Helvellyn's rocks, but attempts to find sufficient quantities of lead to be worth mining have not been successful. The top of Helvellyn
6566-458: The lower end of Borrowdale , receives 1,470 mm (58 in) every year, and Penrith (just outside the Lake District) only 870 mm (34 in). March to June tend to be the driest months, with October to January the wettest, but at low levels, there is relatively little difference between months. Although there are gales in the sheltered valleys on only five days a year on average,
6664-511: The main ridge of the Helvellyn range over Nethermost Pike , High Crag and Dollywagon Pike to terminate at Grisedale Tarn . The former county boundary between Cumberland and Westmorland lay along the Helvellyn Ridge; this meant that the summit of Helvellyn was the highest point in Westmorland, making it a Historic County Top. The whole of Helvellyn, above the conifer plantations to
6762-497: The main ridge of the range, Helvellyn stands on the watershed between Thirlmere and the Derwent river system to the west, and Ullswater and the Eden river system to the east. Streams on the west side drain directly into Thirlmere, apart from Helvellyn Gill which flows into a parallel valley to the east of Great How and empties into St John's Beck. However, when Thirlmere reservoir was built,
6860-512: The mountain conditions. Many people camp on Helvellyn throughout the year, often near Red Tarn which gives good views of Striding Edge, Swirral Edge, and the summit of Helvellyn itself. Although camping in England is illegal without the permission of the landowner, there is a tradition of wild camping in the Lake District. This has often been tolerated so long as people have camped unobtrusively, for no more than one night, and have left no trace of their campsite behind. The summit of Helvellyn takes
6958-453: The mountain is not without dangers; over the last two hundred years there have been a number of fatalities. The artist Charles Gough is more famous for his death on Striding Edge in 1805 than for what he achieved in his life. Among many human feats upon the mountain, one of the strangest was the landing and take-off of a small aeroplane on the summit in 1926. Since early 2018 the summit of Helvellyn including both Striding and Swirral Edges and
7056-551: The mudstones and wackes of the Windermere Supergroup and which includes (successively) the rocks of the Dent, Stockdale, Tranearth, Coniston, and Kendal groups. These are generally a little less resistant to erosion than the sequence of the rock to the north and underlie much of the lower landscapes around Coniston and Windermere. Later intrusions have formed individual outcrops of igneous rock in each of these groups. Around
7154-737: The national park, with the exception of the 2016 extension, was designated a World Heritage Site in 2017 as a cultural landscape . This was the fourth attempt to list the park, after two attempts in the 1980s and one in 2012 failed. The park is governed by the Lake District National Park Authority, which is based at offices in Kendal . It runs a visitor centre on Windermere at a former country house called Brockhole , Coniston Boating Centre, and information centres. The park authority has 20 members: six appointed by Westmorland and Furness Council, four by Cumberland Council, and ten by
7252-498: The north of England from the Irish Sea to the North Sea, traverses the national park from west to east. Bridleways are intended for horse riding and walkers, with cyclists also permitted to use them. Cyclists must give way to all other bridleway users. Motor vehicles are only allowed on "byways open to all traffic" ( green lanes ) but in practice Traffic Regulation Orders have been brought in on several prohibiting motor traffic, although
7350-452: The north of this region are the lower fells of Martindale Common and Bampton Common whilst in the south are the fells overlooking the Kentmere valley. Further to the east, beyond Mardale and Longsleddale is Shap Fell, an extensive area consisting of high moorland , more rolling and Pennine in nature than the mountains to the west. The Southern Fells occupy the southwestern quarter of
7448-399: The public has a right of way , all of which are signposted at their origin on public roads and at some other points. Within the area of the National Park in 2012 there were 2,159 km (1,342 mi) of public footpaths , 875 km (544 mi) of public bridleways , 15 km (9 mi) of restricted byways and 30 km (19 mi) of byways open to all traffic . There is also
7546-403: The range at 852 m (2,795 ft), Grisedale Pike and the hills around the valley of Coledale , and in the far northwest is Thornthwaite Forest and Lord's Seat . The fells in this area are rounded Skiddaw slate , with few tarns and relatively few rock faces. The Western Fells lie between Buttermere and Wasdale , with Sty Head forming the apex of a large triangle. Ennerdale bisects
7644-459: The same lake via Grisedale Beck and Patterdale village. Red Tarn, enclosed between Striding Edge and Swirral Edge, is about 25 m (82 ft) deep, but in the mid-nineteenth century a dam was built to increase its capacity and supply the needs of the Greenside Mine near Glenridding. That dam has now gone and the tarn has returned to its natural size. It contains brown trout and schelly ,
7742-414: The same latitude, ranges from −10 to 19 °C (14 to 66 °F).) The relatively low height of most of the fells means that, while snow is expected during the winter, they can be free of snow at any time of the year. Normally, significant snowfall only occurs between November and April. On average, snow falls on Helvellyn 67 days per year. Snow typically falls on 20 days of the year in the valleys, with
7840-417: The side of the ridge (see The south ridge below.) From Glenridding a similar long but safe and easy walk ( 11.5 km or 7 + 1 ⁄ 4 mi) follows Greenside Road, past the old lead mine and towards Keppel Cove. This track, another old pony track, then zigzags up the fellside to join the main ridge path at the col between Raise and White Side . Grisedale Tarn is the starting point for
7938-437: The south ridge of Helvellyn, and may be reached from Grasmere or Patterdale, or from Dunmail Raise by a path alongside Raise Beck. Above the tarn the old pony track zigzags up the fellside, and takes a safe but unexciting route well away from crags on the side of the ridge, and avoiding all the intermediate tops. In suitable weather a more interesting and scenic route is to follow the edge of the crags as closely as possible, over
8036-517: The south. South of the estuary, the coast is formed in low cliffs of glacial till , sands, and gravels. The district also extends to the tidal waters of Morecambe Bay and several of its estuaries alongside the Furness and Cartmel Peninsulas , designated on M6 motorway signposts as the "Lake District Peninsulas", and the southern portions of which lie outside the park. These are the Duddon Estuary ,
8134-538: The southern and western fringes of the area. A single railway line, the Windermere Branch Line , penetrates from Kendal to Windermere via Staveley. Railways once served Broughton-in-Furness and Coniston (closed to passengers in 1958) and another ran from Penrith to Cockermouth via Keswick (closed west of Keswick in 1966 and completely in 1972). Part of the track of the latter is used by the improved A66 trunk road. The Cumbrian Coast line has three stations within
8232-567: The southern boundary. The southwestern Lake District ends near the Furness peninsula and Barrow-in-Furness, a town which many Lake District residents rely on for basic amenities. The southeastern area is the territory between Coniston Water and Windermere and east of Windermere towards Kendal and south to Lindale. There are no high summits in this area which are mainly low hills, knolls and limestone cuestas such as Gummer's How and Whitbarrow . Indeed, it rises only as high as 333 m (1,093 ft) at Top o' Selside east of Coniston Water;
8330-585: The southwest. Though it is slightly lower, Scafell has a 700 ft (210 m) rockface, Scafell Crag, on its northern side. This group also includes the Wastwater Screes overlooking Wasdale, the Glaramara ridge overlooking Borrowdale, the three tops of Crinkle Crags , Bowfell and Esk Pike . The core of the area is drained by the infant River Esk . Collectively these are some of the Lake District's most rugged hillsides. The second group, otherwise known as
8428-477: The summit of Catstye Cam . The climb up or down from the summit plateau onto Swirral Edge is another well known accident spot. In winter it involves climbing down another snow cornice onto steep icy ground. There have been a number of accidents at this spot in recent years, making it as dangerous as Striding Edge. Nethermost Pike also has an east ridge which gives an alternative route to Helvellyn from Grisedale, which many walkers overlook. It can be combined with
8526-443: The summit ridge at a point half-way along, and which terminates in the shapely pyramid of Catstye Cam . The east ridge is another sharp arête known as Striding Edge. This joins the summit ridge at its southern end, not far from Helvellyn's summit. It passes over the subsidiary top of High Spying How and leads to Birkhouse Moor before descending to its final top, Keldas, beside the south end of Ullswater . The south ridge continues
8624-587: The summit. Nethermost Cove also has some routes, including a large gully between Striding Edge and the back of the cove. Browncove Crags on the western side of the mountain has some north-facing routes. These are easier to access from a car park, and they can be linked with the Red Tarn routes. The Lake District National Park Authority employs two "Fell top assessors" during the winter months, usually between December and March. Working alternate weeks, one of these walks up Helvellyn each day during that period to check
8722-411: The tops of Dollywagon Pike , High Crag and Nethermost Pike . Shorter and quicker routes to the top of Helvellyn, though with less attractive scenery, begin from several points along the A591 road along the west side of the mountain. Two of these may be combined to create a circular walk. Incorporating the south ridge in the route can restore much of the scenic interest. Stannah at Legburthwaite
8820-649: The town of Keswick . It meets the A66 road at a grade-separated junction. Traffic then bypasses Keswick by following the A66 west for 2.2 km to a roundabout where the A591 resumes, continuing in a roughly north-westerly direction, with fine views over Bassenthwaite Lake . The road terminates at the village of Bothel , on the A595 road ( 54°44′09″N 3°16′24″W / 54.7357°N 3.2733°W / 54.7357; -3.2733 ( A591 road (northern end) ) ). The Bothel to Keswick section has many acute bends and
8918-530: The valley between this massif and the North Western Fells. The North Western Fells lie between Borrowdale and Bassenthwaite Lake to the east and Buttermere and Lorton Vale to the west. Their southernmost point is at Honister Pass . This area includes the Derwent Fells above the Newlands Valley and hills to the north amongst which are Dale Head , Robinson . To the north stand Grasmoor , highest in
9016-413: The valley of Helvellyn Gill from the reservoir, before finally rising again to the wooded height of Great How at its terminus. The north ridge, the main ridge of the range, also descends from Lower Man, passing over White Side and Raise to Sticks Pass , then over Stybarrow Dodd and Great Dodd to terminate at Clough Head . The north-east ridge is known as Swirral Edge, a sharp arête which joins
9114-504: The weather, snow and walking conditions. Their report and daily photograph appear on Weatherline, the Lake District weather forecast website and phone line service, which also includes a local weather forecast from the Met Office . The fell top assessors also put their assessments and photos on Twitter . This information is important for people who go out hillwalking and climbing in winter, helping them to plan their routes and get an idea of
9212-400: The west and the intake walls surrounding the valleys of Glenridding and Grisedale to the east, is Open Access land. Routes up Helvellyn can begin from the villages of Glenridding or Patterdale to the east, Grasmere to the south, or from a number of places along the A591 road to the west, and can follow any of the mountain's five ridges, or the ridges of its neighbours, as well as some of
9310-628: The west coast up Eskdale as far as Dalegarth Station near the hamlet of Boot, catering for tourists. Another heritage railway , the Lakeside and Haverthwaite Railway , runs between Lake Windermere and Haverthwaite , and tourists can connect at Lakeside with the boats up the lake to Bowness. A vehicle-carrying cable ferry , the Windermere Ferry , runs frequent services across Windermere. There are also seasonal passenger boats on Coniston Water, Derwent Water, and Ullswater. There are many paths over which
9408-530: The west of the road at Dunmail Raise. Download coordinates as: 54°29′38″N 3°02′19″W / 54.4939°N 3.0386°W / 54.4939; -3.0386 ( A591 road ) Lake District The Lake District , also known as the Lakes or Lakeland , is a mountainous region and national park in Cumbria , North West England . It is famous for its landscape, including its lakes, coast, and
9506-546: The wide expanse of Grizedale Forest stands between the two lakes. Kendal and Morecambe Bay stand at the eastern and southern edges of the area. The main radial valleys are (clockwise from the south) Dunnerdale , Eskdale , Wasdale , Ennerdale , the Vale of Lorton, and Buttermere valley, the Derwent Valley and Borrowdale , the Ullswater valley, Haweswater valley, Longsleddale , the Kentmere valley, those converging on
9604-636: The wider Glenridding Common have been managed by the John Muir Trust , a wild places conservation charity under a three-year lease with the Lake District Park Authority . The volcanic rocks of which the mountain is made were formed in the caldera of an ancient volcano, many of them in violently explosive eruptions, about 450 million years ago during the Ordovician period. During the last ice age these rocks were carved by glaciers to create
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