Lake District facts for kids
|UNESCO World Heritage Site|
|Criteria||Cultural: ii, v, vi|
|Inscription||2017 (41st Session)|
The Lake District, also known as the Lakes or Lakeland, is a mountainous region in North West England. A popular holiday destination, it is famous for its lakes, forests and mountains (or fells), and its associations with William Wordsworth and other Lake Poets and also with Beatrix Potter and John Ruskin. The Lake District National Park was established in 1951 and covers an area of 2,362 square kilometres (912 sq mi). It was designated a UNESCO World Heritage Site in 2017.
The Lake District is today completely within Cumbria, a county and administrative unit created in 1974 by the Local Government Act 1972. However, it was historically divided between three English counties (Cumberland, Westmorland and Lancashire), sometimes referred to as the Lakes Counties. The three counties met at the Three Shire Stone on Wrynose Pass in the southern fells west of Ambleside.
All the land in England higher than 3,000 feet (914 m) above sea level lies within the National Park, including Scafell Pike, the highest mountain in England. It also contains the deepest and largest natural lakes in England, Wast Water and Windermere respectively.
- Lake District National Park
- Human geography
- Physical geography
- Literature and art
- Images for kids
Lake District National Park
The Lake District National Park includes nearly all of the Lake District, though the town of Kendal and the Lakeland Peninsulas are currently outside the park boundary.
The area, which was designated a national park on 9 May 1951 (less than a month after the first UK national park designation — the Peak District), is the most visited national park in the United Kingdom with 15.8 million annual visitors and more than 23 million annual day visits, the largest of the thirteen national parks in England and Wales, and the second largest in the UK after the Cairngorms. Its aim is to protect the landscape by restricting unwelcome change by industry or commerce. Most of the land in the park is in private ownership, with about 55% registered as agricultural land. Landowners include:
- Individual farmers and other private landowners, with more than half of the agricultural land farmed by the owners.
- The National Trust owns about a quarter of the total area (including some lakes and land of significant landscape value).
- The Forestry Commission and other investors in forests and woodland.
- United Utilities owns 8%
- Lake District National Park Authority (3.9%) The National Park Authority 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. It is reducing its landholding.
In common with all other national parks in England, there is no restriction on entry to, or movement within the park along public routes, but access to cultivated land is usually restricted to public footpaths, bridleways and byways. Much of the uncultivated land has statutory open access rights, which cover around 50% of the park.
The lakes and mountains combine to form impressive scenery. Farmland and settlement have altered the natural scenery, and the ecology has been modified by human influence for millennia and includes important wildlife habitats. The Lake District failed in a previous attempt to gain World Heritage status as a natural World Heritage Site, because of human activities, such as commercial forestry, which have adversely impacted the park's assessment. However, in 2016 the English Lake District bid for World Heritage Status was submitted to UNESCO in the category of cultural landscape. A decision is expected in 2017.
Extension to the National Park
In December 2009, Natural England proposed extending the National Park in the direction of the Yorkshire Dales National Park. This would include land of high landscape value in the Lune Valley. The proposal was opposed by Cumbria County Council who said it would lead to less democratic control and would make local housing less affordable. A public inquiry was held into the proposals, which required a decision by the Secretary of State. The decision to recommend approval was announced on October 23, 2015, and the size of the park increased by 3% on 1 August 2016.
The precise extent of the Lake District was not defined traditionally, but is slightly larger than that of the National Park, the total area of which is about 912 square miles (2,362 km2). The park extends just over 32 miles (51 km) from east to west and nearly 40 miles (64 km) from north to south, with areas such as the Lake District Peninsulas to the south lying outside the National Park.
The Lake District is one of the most highly populated national parks. There are, however, only a handful of major settlements within this mountainous area, the towns of Keswick, Windermere, Ambleside, and Bowness-on-Windermere being the four largest. Significant towns immediately outside the boundary of the national park include Millom, Barrow-in-Furness, Kendal, Ulverston, Cockermouth, Penrith, and Grange-over-Sands; each of these has important economic links with the area. Villages such as Coniston, Threlkeld, Glenridding, Pooley Bridge, Broughton-in-Furness, Grasmere, Newby Bridge, Staveley, Lindale, Gosforth and Hawkshead are more local centres. The economies of almost all are intimately linked with tourism. 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 National Park is almost contained within a box of trunk routes. It is flanked to the east by the A6 road which runs from Kendal to Penrith (though the extension approved in 2015 will be east of the A6). The A590 which connects the M6 to Cumbria's largest town, Barrow-in-Furness, and the A5092 trunk roads cut across its southern fringes and the A66 trunk road between Penrith and Workington cuts across its northern edge. Finally the A595 trunk road runs through the coastal plains to the west of the area linking the A66 with the A5092.
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 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 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 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 the B5289 at Buttermere. Wasdale is served by a cul-de-sac minor road, as are 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.
Railways and ferries
The West Coast Main Line skirts the eastern edge of the Lake District and the Cumbrian Coast Line passes through 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 narrow gauge Ravenglass and Eskdale Railway runs from Ravenglass on 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.
Footpaths and bridleways
There are many paths over which the public has a right of way, all of which should be signposted. 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 a general "right to roam" in open country.
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.
Cycling and horse riding are allowed on bridleways, but cyclists must give way to all other 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 a system of permits operates on Gatesgarth Pass.
As the highest ground in England, Scafell Pike naturally has a very extensive view on a clear day, ranging from the Mourne Mountains in Northern Ireland to Snowdonia in Wales. The Lake District takes the form of a roughly circular upland massif deeply dissected by a broadly radial pattern of major valleys whose character is largely the product of repeated glaciations over the last 2 million years. Most of these valleys display the U-shaped cross-section characteristic of glacial origin, and often contain elongate lakes occupying sizeable bedrock hollows, often with tracts of relatively flat ground at their heads. Smaller lakes known as tarns occupy glacial cirques at higher elevations. It is the abundance of both which has led to the area becoming known as the Lake District.
The mountains of the Lake District are also known as the "Cumbrian Mountains", although this name is less frequently used than terms like "the Lake District" or "the Lakeland Fells". Many of the higher fells are rocky, while moorland predominates at lower altitudes. Vegetation cover across better drained areas includes bracken and heather, though much of the land is boggy, due to the high rainfall. Deciduous native woodland occurs on many steeper slopes below the tree line, but with native oak supplemented by extensive conifer plantations in many areas, particularly Grizedale Forest in the generally lower southern part of the area.
The principal radial valleys are (clockwise from the south) Dunnerdale, Eskdale, Wasdale, Ennerdale, Lorton Vale and the Buttermere valley, the Derwent Valley and Borrowdale, the valleys containing Ullswater and Haweswater, Longsleddale, the Kentmere valley and those radiating from the head of Windermere including Great Langdale. The valleys break the mountains up into separate 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.
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 is found in the Lake District and in 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 four highest mountains in the Lake District exceed 3,000 feet (910 m). These are:
- Scafell Pike, 978 m (3,209 ft)
- Scafell, 965 m (3,166 ft)
- Helvellyn, 951 m (3,120 ft)
- Skiddaw, 931 m (3,054 ft)
The Northern Fells are a clearly defined range of hills contained within a 13 km (8 mi) diameter circle between Keswick in the south west and Caldbeck in the north east. 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 the valley between this massif and the North Western Fells.
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 the range at 852 m (2,795 ft), Grisedale Pike and the hills around the valley of Coledale, and in the far north west 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 the area, which consists of the High Stile ridge north of Ennerdale, the Loweswater Fells in the far north west, the Pillar group in the south west, 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, 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 south east to Loughrigg Fell above Ambleside. The central ridge running north over High Seat 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 the Patterdale valley. It culminates in the height of Red Screes overlooking the Kirkstone Pass.
Far Eastern Fells
The Far Eastern Fells refer 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 which runs broadly north–south and overlooks the hidden valley of Haweswater to its east. In 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 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 the southwest. Though it is slightly lower it has a 700 ft (210 m) rockface, Scafell Crag, on its northern side. It 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 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 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 is 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; 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.
- See also: List of lakes in the Lake District
Only one of the lakes in the Lake District 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.
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 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, the divisions between which run south west to north east. Generally speaking the rocks become younger from north west to south east. The north western band is composed of early to mid-Ordovician sedimentary rocks, largely mudstones and siltstones of marine origin. Together they comprise 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 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 south eastern band comprises 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 rocks sequence 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 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 very large local variation. Although the entire region receives above average rainfall, there is a wide disparity between the amount of rainfall in the western and eastern lakes, as the Lake District experiences relief rainfall. Seathwaite in 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 the 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 sheltered valleys experience gales on an average of only five days a year, the Lake District is generally very windy with the coastal areas having 20 days of gales, and the fell tops around 100 days of gales per year. The maritime climate means that the Lake District experiences relatively moderate temperature variations through the year. 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 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 snow fall only occurs between November and April. On average, snow falls on Helvellyn 67 days per year. During the year, valleys typically experience 20 days with snow falling, a further 200 wet days, and 145 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.
|Climate data for Keswick, Lake District|
|Average high °C||7.2||7.4||9.4||11.9||15.6||17.9||19.7||19.1||16.7||13.3||9.7||7.5||13.0|
|Average low °C||1.6||1.4||2.8||4.2||6.4||9.3||11.5||11.1||9.0||6.7||3.9||1.5||5.8|
|Average high °F||45||45.3||48.9||53.4||60.1||64.2||67.5||66.4||62.1||55.9||49.5||45.5||55.4|
|Average low °F||34.9||34.5||37||39.6||43.5||48.7||52.7||52||48.2||44.1||39||34.7||42.4|
|Avg. rainy days||16.8||13.1||15.8||12.5||12.0||12.2||12.9||14.4||13.9||17.8||17.7||17.0||176.1|
The Lake District is home to a great variety of wildlife, due to its range of varied topography, lakes and forests. It provides a home for the red squirrel and colonies of sundew and butterwort, two of 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).
The Lake District is home to a range of bird species, and the RSPB maintain a reserve in Haweswater. England's only nesting pair of golden eagles can be found in the Lake District. The female golden eagle has not been seen since 2004 although the male still remains. Conservationists believe he is now the only resident golden eagle in England. Following recolonisation attempts, a pair of ospreys nested in the Lake District for the first time in over 150 years near Bassenthwaite Lake during 2001. Ospreys now frequently migrate north from Africa in the spring to nest in the Lake District, and a total of 23 chicks have fledged in The Lakes since 2001. Another bird species which has had recolonisation attempts is the red kite which, as of 2012, have a population of approximately 90 in the dense forest areas near Grizedale. Conservationists hope the reintroduction will create a large red kite population in the Lake District and in North West England where the red kite population is low. Other bird species resident to the Lake District include the buzzard, dipper, peregrine and raven. Seasonal birds include the ring ouzel and the redstart.
The lakes of the Lake District support three rare and endangered species of fish: the vendace, which can be found only in Derwent Water and until 2008 in Bassenthwaite Lake. Vendace have struggled in recent years with naturally occurring algae becoming a threat and the lakes gradually getting warmer. Vendace have been moved to higher lakes on a number of occasions to preserve the species, notably in 2005 and 2011. The Lakes are also home to two other rare species: the schelly, which lives in Brothers Water, Haweswater, Red Tarn and Ullswater, and the Arctic charr, which can be found in Buttermere, Coniston Water, Crummock Water, Ennerdale Water, Haweswater, Loweswater, Thirlmere, Wast Water, and Windermere.
In recent years, some important changes have been made to fisheries byelaws covering the north west region of England, to help protect some of the rarest fish species. In 2002, the Environment Agency introduced a new fisheries byelaw, banning the use of all freshwater fish as live or dead bait in 14 of the lakes in the Lake District. Anglers not complying with the new byelaw can face fines of up to £2,500. There are 14 lakes in the Lake District which are affected. These are: Bassenthwaite Lake, Brothers Water, Buttermere, Coniston Water, Crummock Water, Derwent Water, Ennerdale Water, Haweswater, Loweswater, Red Tarn, Thirlmere, Ullswater, Wast Water and Windermere.
The lakes and waters of the Lake District do not naturally support as many species of fish as other similar habitats in the south of the country and elsewhere in Europe. Some fish that do thrive there are particularly at risk from introduction of new species.
The introduction of non-native fish can lead to the predation of the native fish fauna or competition for food. There is also the risk of disease being introduced, which can further threaten native populations. In some cases, the introduced species can disturb the environment so much that it becomes unsuitable for particular fish. For example, a major problem has been found with ruffe. This non-native fish has now been introduced into a number of lakes in recent years. It is known that ruffe eat the eggs of vendace, which are particularly vulnerable because of their long incubation period. This means that they are susceptible to predators for up to 120 days. The eggs of other fish, for example roach, are only at risk for as little as three days.
Literature and art
The Lake District is intimately associated with English literature of the 18th and 19th centuries. Thomas Gray was the first to bring the region to attention, when he wrote a journal of his Grand Tour in 1769, but it was William Wordsworth whose poems were most famous and influential. Wordsworth's poem "I Wandered Lonely as a Cloud", inspired by the sight of daffodils on the shores of Ullswater, remains one of the most famous in the English language. Out of his long life of eighty years, sixty were spent amid its lakes and mountains, first as a schoolboy at Hawkshead, and afterwards living in Grasmere (1799–1813) and Rydal Mount (1813–50). Wordsworth, Coleridge and Southey became known as the Lake Poets.
The poet and his wife lie buried in the churchyard of Grasmere and very near to them are the remains of Hartley Coleridge (son of the poet Samuel Taylor Coleridge), who himself lived for many years in Keswick, Ambleside and Grasmere. Robert Southey, the Poet Laureate and friend of Wordsworth (who would succeed Southey as Laureate in 1843), was a resident of Keswick for forty years (1803–43), and was buried in Crosthwaite churchyard. Samuel Taylor Coleridge lived for some time in Keswick, and also with the Wordsworths at Grasmere. From 1807 to 1815 John Wilson lived at Windermere. Thomas de Quincey spent the greater part of the years 1809 to 1828 at Grasmere, in the first cottage which Wordsworth had inhabited. Ambleside, or its environs, was also the place of residence both of Thomas Arnold, who spent there the vacations of the last ten years of his life and of Harriet Martineau, who built herself a house there in 1845. At Keswick, Mrs Lynn Linton (wife of William James Linton) was born, in 1822. Brantwood, a house beside Coniston Water, was the home of John Ruskin during the last years of his life. His assistant W. G. Collingwood the author, artist and antiquarian lived nearby, and wrote Thorstein of the Mere, set in the Norse period.
In addition to these residents or natives of the Lake District, a variety of other poets and writers made visits to the Lake District or were bound by ties of friendship with those already mentioned above. These include Percy Bysshe Shelley, Sir Walter Scott, Nathaniel Hawthorne, Arthur Hugh Clough, Henry Crabb Robinson, "Conversation" Sharp, Thomas Carlyle, John Keats, Lord Tennyson, Matthew Arnold, Felicia Hemans, and Gerald Massey.
During the early 20th century, the children's author Beatrix Potter was in residence at Hill Top Farm, setting many of her famous Peter Rabbit books in the Lake District. Her life was made into a biopic film, starring Renée Zellweger and Ewan McGregor. Arthur Ransome lived in several areas of the Lake District, and set five of his Swallows and Amazons series of books, published between 1930 and 1947, in a fictionalised Lake District setting. So did Geoffrey Trease with his five Black Banner school stories (1949–56), starting with No Boats on Bannermere.
The novelist Sir Hugh Walpole lived at "Brackenburn" on the lower slopes of Catbells overlooking Derwent Water from 1924 until his death in 1941. Whilst living at "Brackenburn" he wrote The Herries Chronicle detailing the history of a fictional Cumbrian family over two centuries. The noted author and poet Norman Nicholson came from the south west lakes, living and writing about Millom in the 20th century – he was known as the last of the Lake Poets and came close to becoming the Poet Laureate.
The Lakes has been an inspirations for many notable artists. Some of the most famous artists to depict the region in their work have been Alfred Heaton Cooper and William Heaton Cooper.
Writer and author Melvyn Bragg was brought up in the region and has used it as the setting for some of his work, such as his novel A Time to Dance, later turned into a television drama.
The Lake District has been the setting for crime novels by Reginald Hill, Val McDermid and Martin Edwards. The region is also a recurring theme in Ernest Hemingway's 1926 novella The Torrents of Spring and features prominently in Ian McEwan's Amsterdam, which won the 1998 Booker Prize.
The Lake District is mentioned in Jane Austen's Pride and Prejudice; Elizabeth Bennet looks forward to a holiday there with her aunt and uncle and is "excessively disappointed" upon learning they cannot travel that far.
Film director Ken Russell lived in the Keswick/Borrowdale area until 2007 and used it in films such as Tommy and Mahler.
The former Keswick School of Industrial Art at Keswick was started by Canon Rawnsley, a friend of John Ruskin.
A number of words and phrases are local to the Lake District and are part of the Cumbrian dialect, though many are shared by other northern dialects. These include:
- Fell – from Old Norse fjallr, brought to England by Viking invaders and close to modern Norwegian fjell and Swedish fjäll meaning mountain
- Howe – place name from the Old Norse haugr meaning hill, knoll, or mound
- Tarn – a word that has been taken to mean a small lake situated in a corrie (the local name for which is cove), a local phrase for any small pool of water. The word is derived from the Old Norse, Norwegian and Swedish word tjern/tjärn, meaning small lake.
- Yan tan tethera – the name for a system of sheep counting which was traditionally used in the Lake District. Though now rare, it is still used by some and taught in local schools.
- Heaf (a variant of heft) – the "home territory" of a flock of sheep
Agriculture and forestry
Farming, and in particular sheep farming, has been the major industry in the region since Roman times. The breed most closely associated with the area is the tough Herdwick, with Rough Fell and Swaledale sheep also common. Sheep farming remains important both for the economy of the region and for preserving the landscape which visitors want to see. Features such as dry stone walls, for example, are there as a result of sheep farming. Some land is also used for silage and dairy farming.
The area was badly affected by the outbreak of foot-and-mouth disease across the United Kingdom in 2001. The outbreak started in Surrey in February, but had spread to Cumbria by end of March. Thousands of sheep, including the native Herdwicks which graze on the fellsides across the district, were destroyed. In replacing the sheep, one problem to overcome was that many of the lost sheep were heafed, that is, they knew their part of the unfenced fell and did not stray, with this knowledge being passed between generations. With all the sheep lost at once, this knowledge has to be relearnt and some of the fells have had discreet electric fences strung across them for a period of five years, to allow the sheep to "re-heaf". At the time of the outbreak, worries existed about the future of certain species of sheep such as Ryeland and Herdwick in the district, however these fears have been allayed and sheep now occupy the district in abundance.
Forestry has also assumed greater importance over the course of the last century with the establishment of extensive conifer plantations around Whinlatter Pass, in Ennerdale and at Grizedale Forest amongst other places. There are extensive plantations of non-native pine trees.
With its wealth of rock types and their abundance in the landscape, mining and quarrying have long been significant activities in the Lake District economy. In Neolithic times, the Lake District was a major source of stone axes, examples of which have been found all over Britain. The primary site, on the slopes of the Langdale Pikes, is sometimes described as a "stone axe factory" of the Langdale axe industry. Some of the earliest stone circles in Britain are connected with this industry.
Mining, particularly of copper, lead (often associated with quantities of silver), baryte, graphite and slate, was historically a major Lakeland industry, mainly from the 16th to 19th centuries. Coppiced woodland was used extensively to provide charcoal for smelting. Some mining still takes place today; for example, slate mining continues at the Honister Mines, at the top of Honister Pass. Abandoned mine workings can be found on fellsides throughout the district. The locally mined graphite led to the development of the pencil industry, especially around Keswick.
In the middle of the 19th century, half the world textile industry's bobbin supply came from the Lake District area. Over the past century, however, tourism has grown rapidly to become the area's primary source of income.
Excellent mutton and lamb has been produced locally for generations and traditionally formed the basis of the region's many rustic dishes, such as Tatie Pot, a potato-topped mutton casserole. The Traditional Cumberland Sausage is a spiced, unlinked pork sausage with Protected Geographical Status. The Lake District now has a growing reputation for its fine dining although standard pub and cafe fare continues to dominate. There are 5 Michelin Star restaurants within the World Heritage Site boundaries, with a further one less than a mile outside (L'Enclume). Those inside the area are: The Cottage in the Wood, Allium at Askham Hall, Old Stamp House (Ambleside), the Forest Side, and Hrishi, one of the two restaurants at the Gilpin Hotel, Cumbria has many microbreweries, together with Jennings Brewery they supply a variety of ales to pubs and restaurants throughout the region.
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