82-664: Whernside is a mountain in the Yorkshire Dales in Northern England . It is the highest of the Yorkshire Three Peaks , the other two being Ingleborough and Pen-y-ghent . It is the highest point in the ceremonial county of North Yorkshire and the historic West Riding of Yorkshire with the summit lying on the county boundary with Cumbria . It is the fifteenth most prominent hill in England. In shape Whernside forms
164-732: 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
246-436: 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
328-468: 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
410-464: 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
492-401: A long ridge, running roughly north-north-east to south-south-west. The mountain is 6 miles (10 km) north west of Ingleton and 6 miles (10 km) north of Horton-in-Ribblesdale . The name, first recorded in 1208 as Querneside , is of Old English origin. It is derived from cweorn ' quern ' or 'millstone' and sīde 'hillside', so means "hillside where millstones are found". The name
574-676: A major area for caving in the UK. The word dale , like dell , is derived from the Old English word dæl . It has cognates in the Nordic / Germanic words for valley ( dal , tal ), and occurs in valley names across Yorkshire and Northern England. Usage here may have been reinforced by Nordic languages during the time of the Danelaw . Most of the dales are named after their river or stream (e.g., Arkengarthdale , formed by Arkle Beck ). The best-known exception
656-599: A mobile-device software app for those who wish to explore the relevant areas. In this primarily agricultural area, tourism has become an important contributor to the economy. In 2016, there were 3.8 million visits to the Yorkshire Dales National Park including 0.48 million who stayed at least one night. The park authority estimates that this contributed £252 million to the economy and provided 3,583 full-time equivalent jobs. The wider Yorkshire Dales area received 9.7 million visitors who contributed £644 million to
738-492: A splendid exercise for the legs"; a 10 + 1 ⁄ 2 -mile (17 km) route from Dent (alternatively, 7 + 1 ⁄ 2 miles or 12 kilometres from a car parked nearer), following what is now the Dales High Way route onto the ridge and descending steeply west to Deepdale, "a fine walk on a fine day with excellent views ... the best of all routes up Whernside because of the lovely countryside from which it springs"; and
820-430: 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
902-543: Is Wensleydale , which is named after the small village and former market town of Wensley , rather than the River Ure , although an older name for the dale is Yoredale. River valleys all over Yorkshire are called "(name of river)+ dale "—but only the more northern valleys (and only the upper, rural, reaches) are included in the term "The Dales". The Yorkshire Dales are surrounded by the North Pennines and Orton Fells in
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#1733085599898984-433: 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
1066-519: 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
1148-523: 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
1230-524: 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
1312-572: 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
1394-535: 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
1476-578: Is of the same origin as Great Whernside , 17 miles (27 km) to the east, with which it is sometimes confused. Whernside lies about two miles (three kilometres) northwest of Ribblehead Viaduct on the Settle–Carlisle Railway , and the mountain is commonly ascended from Ribblehead. There is a public footpath from Ribblehead that heads north via Smithy Hill and Grain Ings before turning west to Knoutberry Haw and then south to Whernside itself. From
1558-510: 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
1640-487: The 7 + 1 ⁄ 2 -mile (12 km) ascent from Ribblehead, via Force Gill with a direct return via Winterscales. On a clear day the views from the summit to the west can be spectacular, with views of the Lake District and Morecambe Bay , including (with the aid of binoculars) Blackpool Tower , some 40 miles (65 km) away. Yorkshire Dales The Yorkshire Dales are a series of valleys, or dales , in
1722-654: 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
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#17330855998981804-501: 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
1886-580: The Discover England websites, for example, were using the tagline "Discover 'All Creatures Great and Small' in Yorkshire". The dales are U- and V-shaped valleys, the former enlarged and shaped by glaciers , mainly in the most recent Devensian ice age . The underlying rock is mainly Carboniferous Limestone , which results in a large areas of karst topography, in places overlain with shale and sandstone and topped with Millstone Grit , although to
1968-558: 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
2050-616: 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
2132-569: 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
2214-651: 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
2296-569: The Nidderdale AONB , but without the towns listed above apart from Settle. The lower reaches of Airedale and Wharfedale are not usually included in the area, and Calderdale , south of Airedale and in the South Pennines, is not often considered part of the Dales (even though it is a dale, is in Yorkshire, and its upper reaches are as scenic and rural as many further north). Additionally, although
2378-583: 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
2460-584: The Pennines , an upland range in England. They are mostly located in the ceremonial county of North Yorkshire , but extend into Cumbria and Lancashire ; they are entirely within the historic boundaries of Yorkshire . The majority of the dales are within the Yorkshire Dales National Park , created in 1954. The exception is the area around Nidderdale , which forms the separate Nidderdale Area of Outstanding Natural Beauty . The landscape of
2542-485: 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
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2624-598: 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
2706-453: The Trip Advisor site include Aysgarth Falls , Malham Cove (scenic walking areas), Ingleborough (hiking trails) and Ribblehead Viaduct . The DalesBus service provides service in the Dales on certain days in summer, "including the Yorkshire Dales National Park and Nidderdale Area of Outstanding Natural Beauty". In summer, these buses supplement the other services operating year-round in
2788-537: The Washburn Valley whose tributary streams and rivers feed into the larger valleys, and Barbondale , Dentdale , Deepdale and Garsdale which feed west to the River Lune . The characteristic scenery of the Dales is green upland pastures separated by dry-stone walls and grazed by sheep and cattle. A survey carried out in 1988 estimated that there were just over 4,971 miles (8,000 km) of dry-stone walling in
2870-536: The triangulation pillar to reach Deepdale Lane near White Shaw Moss. An alternative route heads directly north across Knoutberry Haw to pass Whernside Tarns and reaches the Craven Way at Boot of the Wold. Following the southern descent for 3 ⁄ 4 mile (1.2 kilometres), instead of turning steeply south-east towards Bruntscar a path continues south-west running adjacent to the wall passing Combe Scar and West Fell to reach
2952-526: 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
3034-661: 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
3116-572: 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
3198-655: The Dales. Tourism in the region declined because of restrictions implemented in relation to the COVID-19 pandemic in 2020, and into 2021. Later in 2021, the volume of visits was expected to increase as a result of the 2020 TV series All Creatures Great and Small , largely filmed within the Dales. The first series aired in the UK in September 2020 and in the US in early 2021. One source stated that visits to Yorkshire websites had increased significantly by late September 2020. By early 2021,
3280-689: 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
3362-511: 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
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3444-440: 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
3526-592: The National Park includes the Howgill Fells and Orton Fells, they are not usually considered part of the Dales. Most of the larger southern dales – Ribblesdale, Malhamdale and Airedale, Wharfedale and Nidderdale – run roughly parallel from north to south. The more northerly dales – Wensleydale and Swaledale – run generally from west to east. There are many other smaller or lesser-known dales such as Arkengarthdale , Bishopdale , Clapdale, Coverdale , Kingsdale , Littondale , Langstrothdale , Raydale Waldendale and
3608-532: The Yorkshire Dales consists of sheltered glacial valleys separated by exposed moorland . The predominant rock is Carboniferous Limestone , which is particularly visible in the south-west in features such as Malham Cove . It is overlain in many areas by the Yoredale Series of alternating weak shales and hard limestones and sandstones, which give the dales their characteristic 'stepped' appearance. Most of
3690-698: The Yorkshire Dales. Many upland areas consist of heather moorland, used for grouse shooting from 12 August (the Glorious Twelfth ). Much of the rural area is used for agriculture, with residents living in small villages and hamlets or in farmsteads. Miles of dry-stone walls and much of the traditional architecture have remained, including some field barns, though many are no longer in active use. Breeding of sheep and rearing of cattle remain common. To supplement their incomes, many farmers have diversified, with some providing accommodations for tourists. A number of agricultural shows are held each year. Lead mining
3772-540: 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
3854-558: 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,
3936-410: 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
4018-541: 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
4100-574: 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
4182-600: 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
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#17330855998984264-637: The dales contain rivers, and the area contains seven primary catchments : the Swale , Ure , Wharfe , Aire , Nidd , Ribble , and Lune . There are several notable cave systems in the area, including the longest system in the United Kingdom, the Three Counties . Agriculture and other land management has significantly affected the appearance of the Dales, through the creation of pastures and meadows for livestock grazing and moorland for red grouse shooting. Dry stone walls and field barns are characteristic of
4346-624: 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
4428-516: The economy. Visitors are often attracted by the hiking trails, including some that lead to waterfalls and picturesque villages and small towns. These include Kirkby Lonsdale (just outside the area), Hawes , Appletreewick , Masham , Clapham , Long Preston and Malham . The 73-mile-long (117 km) Settle–Carlisle line railway, operated by Network Rail , runs through the National Park using tunnels and viaducts, including Ribblehead. The top-rated attractions according to travellers using
4510-534: 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
4592-452: 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
4674-475: The footpath from Blea Moor Sidings) is a distance of roughly 8 + 1 ⁄ 2 miles (13.5 km). Alfred Wainwright in his 1970 Walks in Limestone Country describes three walks titled "Ascent of Whernside": a 14 + 1 ⁄ 4 -mile (23-kilometre) route from Ingleton , up the southwest ridge and returning via Ellerbeck, which he describes as "an exhilarating walk, a tonic for jaded minds, and
4756-416: 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
4838-409: 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
4920-467: The limestone pavements at Ewe's Top. Finally, 275 yards (250 m) south of the triangulation pillar an old route (partly fenced off) descends (initially very steeply) for 1 + 1 ⁄ 4 miles (2 kilometres) to reach a road 275 yards (250 m) southwest of Winterscales Farm, this is the old route of the Three Peaks Challenge. Walkers should select this route with care as it is no longer maintained, boggy, badly eroded and requires extreme care over
5002-402: 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,
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#17330855998985084-441: 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
5166-609: 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
5248-405: The north and west of the Dent Fault the hills are formed from older Silurian and Ordovician rocks. The underlying limestone in parts of the Dales has extensive cave systems, including the 54-mile-long (87 km) Three Counties System , making it a major area for caving in the UK. There are over 2500 known caves; some are open to the public for tours. Visitors can try caving at one of
5330-446: 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
5412-402: 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
5494-420: The north, the Vales of York and Mowbray in the east, the South Pennines in the south, and the Lake District and Howgill Fells to the west. They spread to the north from the market and spa towns of Settle , Skipton , and Harrogate in North Yorkshire, to the southern boundary in Wharfedale and Airedale . Natural England define the area as most of the Yorkshire Dales National Park with fringes of
5576-399: 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
5658-403: 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
5740-414: 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
5822-445: The show caves: White Scar Cave, Ingleborough Cave or Stump Cross Caverns near Greenhow. The systems include: 54°16′N 2°05′W / 54.267°N 2.083°W / 54.267; -2.083 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
5904-517: 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 ,
5986-538: 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
6068-567: 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;
6150-585: 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
6232-581: The steep ascent/descent. The current route of the Three Peaks fell race runs approximately 440 yards (400 m) north of this old ascent along open moor. A walk solely around Whernside starting at the junction of the Blea Moor and Gauber roads near the Station Inn at Ribblehead, to the top of Whernside and back via the bridleway from Bruntscar via the farms at Broadrake, Ivescar, Winterscales and Gunnerfleet (or
6314-546: The summit the right of way heads initially south, then steeply south-east down a stepped path to the area known as Bruntscar. If climbed as part of the Yorkshire Three Peaks Challenge (which is normally done anti-clockwise ) Whernside is climbed following the route up from Ribblehead to descend to Bruntscar. There are, however, other routes up/down the mountain which are not rights of way but instead make use of open access land . A path heads directly west from
6396-530: 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
6478-618: The valley floors, particularly Wensleydale and Swaledale in the north. Wensleydale cheese is a particularly famous product from the region. The dales are popular for hiking, and are crossed by the Dales Way , Pennine Way , and Coast to Coast long-distance footpaths . The Yorkshire Three Peaks is a walking trail entirely within the area which takes in its three highest mountains: Ingleborough (723 m (2,372 ft)), Whernside (736 m (2,415 ft)), and Pen-y-ghent (694 m (2,277 ft)). The extensive cave systems are
6560-628: 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
6642-596: 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
6724-481: Was common in some areas of the Dales in the 19th century, particularly during 1821 to 1861, and some industrial remains can still be found, such as the Grassington miners' cottages. Certain former mining sites are maintained by Historic England . The Grassington Moor Lead Mining Trail, with its many remaining structures, has received funding from a variety of sources. The Yorkshire Dales National Park Authority provides
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