Сочинение The National Parks of Great Britan
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School - ghymnasia №6
Project work
The Natieonal Parks of Great Britan
Dany by: Chernyshova Nastya
From
Teacher: Kestel O. V.
Semey 2009
Content
1. Introduction
2. Dartmoor National park
History
Pre-history
Beardown Man, Dartmoor
The historical period
Myths and literature
Towns
Physical geography
Rivers
3. Peak district national park
History
Early history
Medieval to modern history
Transport
History
Totley Tunnel on the Manchester to Sheffield line
Road network
Public transport
Geography
4. The Broads National Park
History
Geography
5. Queen Elizabeth Park, British Columbia
History
Attractions
6. History of the New Forest
New Forest National Park
Geography
7. Exmoor
History
Geology
Coastline
Flora
Fauna
Places of interest
8. Yorkshire Dales
Yorkshire Dales National Park
Geography
Cave systems
9. Lake District
General geography
Development of tourism
Conclusion
Additional material
Literature
1. Introduction
The theam of my project work “National parks of Great Britan".
National Parks of Great Britan cover approximately 7% of the country. They did not have any special exotic animals or plants, But such areas as Dartmoor, Peak District, Yorkshire, Valley Noth York, the New Forest and
In my project work, I will write about some of them.
Special attention I wiil pay to the study of history, culture and geography.
2. Dartmoor National park
Dartmoor is an area of moorland in the centre of Devon, England. Protected by National Park status, it covers 368 square miles (953 km2).
The granite upland dates from the Carboniferous period of geological history. The moorland is capped with many exposed granite hilltops (known as tors), providing habitats for Dartmoor wildlife. The highest point is High Willhays, 621 m (2,037 ft) above sea level. The entire area is rich in antiquities and archaeology.
Parts of
History
Pre-history
The majority of the prehistoric remains on
The climate at the time was warmer than today, and much of today’s moorland was covered with trees. The prehistoric settlers began clearing the forest, and established the first farming communities. Fire was the main method of clearing land, creating pasture and swidden types of fire-fallow farmland. Areas less suited for farming, tended to be burned for livestock grazing. Over the centuries these Neolithic practices greatly expanded the upland moors, contributed to the acidification of the soil and the accumulation of peat and bogs.
The nature of the soil, which is highly acidic, means that no organic remains have survived. However, by contrast, the high durability of the natural granite means that their homes and monuments are still to be found in abundance, as are their flint tools. It should be noted that a number of remains were “restored" by enthusiastic Victorians and that, in some cases, they have placed their own interpretation on how an area may have looked.
Beardown Man, Dartmoor
Numerous menhirs (more usually referred to locally as standing stones or longstones), stone circles, kistvaens, cairns and stone rows are to be found on the moor. The most significant sites include:
Beardown Man, near Devil’s Tor - isolated standing stone 3.5 m (11 ft) high, said to have another 1 m (3.3 ft) below ground. grid reference SX596796
Challacombe, near the prehistoric settlement of Grimspound - triple stone row. grid reference SX689807
Drizzlecombe, east of Sheepstor village - stone circles, rows, standing stones, kistvaens and
Grey Wethers, near Postbridge - double circle, aligned almost exactly north south. grid reference SX638831
Laughter Tor, near Two Bridges - standing stone 2.4 m (7.9 ft) high and two double stone rows, one 164 m (540 ft) long. grid reference SX652753
Merrivale, between Princetown and Tavistock - includes a double stone row 182 m (600 ft) long, 1.1 m (3.6 ft) wide, aligned almost exactly east-west), stone circles and a kistvaen. grid reference SX554747
Scorhill, west of Chagford - circle, 26.8 m (88 ft) in circumference, and stone rows. grid reference SX654873
Shovel Down, north of Fernworthy reservoir - double stone row approximately 120 m (390 ft) long. grid reference SX660859
There are also an estimated 5,000 hut circles still surviving today, despite the fact that many have been raided over the centuries by the builders of the traditional dry stone walls. These are the remnants of Bronze Age houses. The smallest are around 1.8 m (6 ft) in diameter, and the largest may be up to five times this size.
Some have L-shaped porches to protect against wind and rain - some particularly good examples are to be found at Grimspound. It is believed that they would have had a conical roof, supported by timbers and covered in turf or thatch.
Many ancient structures, including the hut circles at Grimspound, were reconstructed during the 19th century - most notably by civil engineer and historian Richard Hansford Worth. Some of this work was based more on speculation than archaeological expertise, and has since been criticised for its inaccuracy.
The historical period
The climate worsened over the course of a thousand years from around 1000 BC, so that much of high
It was not until the early medieval period that the weather again became warmer, and settlers moved back onto the moors. Like their ancient forebears, they also used the natural granite to build their homes, preferring a style known as the longhouse - some of which are still inhabited today, although they have been clearly adapted over the centuries. Many are now being used as farm buildings, while others were abandoned and fell into ruin.
The earliest surviving farms, still in operation today, are known as the Ancient Tenements. Most of these date back to the 14th century and sometimes earlier.
Some way into the moor stands the town of Princetown, the site of the notorious Dartmoor Prison, which was originally built both by, and for, prisoners of war from the Napoleonic Wars. The prison has a (now misplaced) reputation for being escape-proof, both due to the buildings themselves and its physical location.
The Dartmoor landscape is scattered with the marks left by the many generations who have lived and worked there over the centuries - such as the remains of the once mighty Dartmoor tin-mining industry, and farmhouses long since abandoned. Indeed the industrial archaeology of Dartmoor is a subject in its own right.
Myths and literature
Many landmarks have ancient legends and ghost stories associated with them, such as Jay’s Grave, the ancient burial site at Childe’s Tomb, the rock pile called Bowerman’s Nose, and the stone crosses that mark mediaeval routes across the moor.
A few stories have emerged in recent decades, such as the ‘hairy hands’, that are said to attack travellers on the B3212 near Two Bridges.
Dartmoor has inspired a number of artists and writers, such as Sir Arthur Conan Doyle in The Hound of the Baskervilles and The Adventure of Silver Blaze, Eden Phillpotts, Beatrice Chase, Agatha Christie and the Reverend Sabine Baring-Gould.
Towns
and villages
Physical geography
Tors.
The highest points on Dartmoor are High Willhays (grid reference SX580895) at 621 m (2,040 ft) and Yes Tor (grid reference SX581901) 619 m (2,030 ft) on the northern moor. Ryder’s Hill (grid reference SX690660), 515 m (1,690 ft), Snowdon 495 m (1,620 ft), and an unnamed point at (grid reference SX603645),493 m (1,620 ft) are the highest points on the southern moor. Probably the best known tor on Dartmoor is Haytor (also spelt Hey Tor) (grid reference SX757771), 457 m (1,500 ft). For a more complete list see List of Dartmoor tors and hills.
Rivers
The levels of rainfall on
In areas where water accumulates, dangerous bogs or mires can result. Some of these, up to 12 feet (3.7 m) across and topped with bright green moss, are known to locals as “feather beds” or “quakers", because they shift (or ‘quake’) beneath your feet. This is the result of accumulations of sphagnum moss growing over a hollow in the granite filled with water.
Another consequence of the high rainfall is that there are numerous rivers and streams on
The Moor takes its name from the River Dart, which starts as the East Dart and West Dart and then becomes a single river at Dartmeet.
For a full list, expand the Rivers of Dartmoor navigational box at the bottom of this page.
Angling.
Angling is a popular pastime on the moor, especially for migratory fish such as salmon.
Kayaking and canoeing.
3. Peak district national park
The Peak District is an upland area in central and northern England, lying mainly in northern Derbyshire, but also covering parts of Cheshire, Greater Manchester, Staffordshire, and South and West Yorkshire.
Most of the area falls within the Peak District National Park, whose designation in 1951 made it the earliest national park in the
History
Early history
The Peak District has been settled from the earliest periods of human activity, as is evidenced by occasional finds of Mesolithic flint artefacts and by palaeoenvironmental evidence from caves in Dovedale and elsewhere. There is also evidence of Neolithic activity, including some monumental earthworks or barrows (burial mounds) such as that at Margery Hill. [12] In the Bronze Age the area was well populated and farmed, and evidence of these people survives in henges such as Arbor Low near Youlgreave or the Nine Ladies Stone Circle at Stanton Moor. In the same period, and on into the Iron Age, a number of significant hillforts such as that at Mam Tor were created. Roman occupation was sparse but the Romans certainly exploited the rich mineral veins of the area, exporting lead from the Buxton area along well-used routes. There were Roman settlements, including one at Buxton which was known to them as “Aquae Arnemetiae” in recognition of its spring, dedicated to the local goddess.
Theories as to the derivation of the Peak District name include the idea that it came from the Pecsaetan or peaklanders, an Anglo-Saxon tribe who inhabited the central and northern parts of the area from the 6th century AD when it fell within the large Anglian
Medieval to modern history
In medieval and early modern times the land was mainly agricultural, as it still is today, with sheep farming, rather than arable, the main activity in these upland holdings. However, from the 16th century onwards the mineral and geological wealth of the Peak became increasingly significant. Not only lead, but also coal, copper (at Ecton), zinc, iron, manganese and silver have all been mined here. Celia Fiennes, describing her journey through the Peak in 1697, wrote of ‘those craggy hills whose bowells are full of mines of all kinds off black and white and veined marbles, and some have mines of copper, others tinn and leaden mines, in w [hi] ch is a great deale of silver. ’ Lead mining peaked in the 17th and 18th centuries and began to decline from the mid-19th century, with the last major mine closing in 1939, though lead remains a by-product of fluorspar, baryte and calcite mining (see Derbyshire lead mining history for details). Limestone and gritstone quarries flourished as lead mining declined, and remain an important industry in the Peak.
Large reservoirs such as Woodhead and Howden were built from the late 19th century onward to supply the growing urban areas surrounding the Peak District, often flooding large areas of farmland and depopulating the surrounding land in an attempt to improve the water purity.
The northern moors of Saddleworth and Wessenden gained notoriety in the 1960s as the burial site of several children murdered by the so-called Moors Murderers, Ian Brady and Myra Hindley.
Transport
History
The first roads in the Peak were constructed by the Romans, although they may have followed existing tracks. The Roman network is thought to have linked the settlements and forts of Aquae Arnemetiae (Buxton), Chesterfield, Ardotalia (Glossop) and Navio (Brough-on-Noe), and extended outwards to Danum (Doncaster), Manucium (Manchester) and Derventio (Little Chester, near Derby). Parts of the modern A515 and A53 roads south of Buxton are believed to run along Roman roads.
Packhorse routes criss-crossed the Peak in the Medieval era, and some paved causeways are believed to date from this period, such as the Long Causeway along Stanage. However, no highways were marked on Saxton’s map of Derbyshire, published in 1579. Bridge-building improved the transport network; a surviving early example is the three-arched gritstone bridge over the River Derwent at Baslow, which dates from 1608 and has an adjacent toll-shelter. [18] Although the introduction of turnpike roads (toll roads) from 1731 reduced journey times, the journey from Sheffield to Manchester in 1800 still took 16 hours, prompting Samuel Taylor Coleridge to remark that ‘a tortoise could outgallop us! ’From around 1815 onwards, turnpike roads both increased in length and improved in quality. An example is the Snake Road, built under the direction of Thomas Telford in 1819-21 (now the A57); the name refers to the crest of the Dukes of Devonshire. The Cromford Canal opened in 1794, carrying coal, lead and iron ore to the Erewash Canal.
Totley Tunnel on the Manchester to Sheffield line
The improved roads and the
By the second half of the 20th century, the pendulum had swung back towards road transport. The
Road network
The main roads through the Peak District are the A57 (Snake Pass) between Sheffield and Manchester, the A628 (Woodhead Pass) between Barnsley and Manchester via Longdendale, the A6 from Derby to Manchester via Buxton, and the Cat and Fiddle road from Macclesfield to Buxton. These roads, and the pretty minor roads and lanes, are attractive to drivers, but the Peak’s popularity makes road congestion a significant problem especially during summer.
Public transport
The Peak District is readily accessible by public transport, which reaches even central areas. Train services into the area are the Hope Valley Line from Sheffield and Manchester; the Derwent Valley Line from Derby to Matlock; and the Buxton Line and the Glossop Line linking those towns to Manchester. Coach (long-distance bus) services provide access to Matlock, Bakewell and Buxton from
For such a rural area, the smaller villages of the Peak are relatively well served by internal transport links. There are many minibuses operating from the main towns (Bakewell, Matlock, Hathersage, Castleton, Tideswell and Ashbourne) out to the small villages. The
Geography
The Peak District forms the southern end of the Pennines and much of the area is uplands above 1,000 feet (300 m), with a
The National Park covers 555 square miles (1,440 km2) of Derbyshire, Staffordshire,
High Peak panorama between Hayfield and Chinley
12% of the
4. The Broads National Park
The Broads is a network of mostly navigable rivers and lakes (known locally as broads) in the English counties of Norfolk and Suffolk. The
The total area is 303 km² (188 sq.miles), most of which is in
Although the terms Norfolk Broads and Suffolk Broads are used to identify those areas within the two counties respectively, the whole area is sometimes referred to as the “Norfolk Broads”. The Broads has the same status as the national parks in
History
For many years the broads were regarded as natural features of the landscape. It was only in the 1960s that Dr Joyce Lambert proved that they were artificial features, the effect of flooding on early peat excavations. The Romans first exploited the rich peat beds of the area for fuel, and in the Middle Ages the local monasteries began to excavate the peat lands as a turbary business, selling fuel to Norwich and Great Yarmouth. The Cathedral took 320,000 tonnes of peat a year. Then the sea levels began to rise, and the pits began to flood. Despite the construction of windpumps and dykes, the flooding continued and resulted in the typical
The Broads have been a favourite boating holiday destination since the early 20th century. The waterways are lock-free, although there are three bridges under which only small cruisers can pass. The area attracts all kinds of visitors, including ramblers, artists, anglers, and bird-watchers as well as people “messing about in boats". There are a number of companies hiring boats for leisure use, including both yachts and motor launches. The Norfolk Wherry, the traditional cargo craft of the area, can still be seen on the
Ted Ellis, a local naturalist, referred to the
A great variety of boats can be found on the
Geography
The point at which the River Yare and the River Waveney merge into Breydon Water
Yachts on the
How Hill
St. Benet’s Abbey
The Broads largely follows the line of the rivers and natural navigations of the area. There are seven navigable rivers, the River Yare and its (direct and indirect) tributaries the Rivers Bure, Thurne, Ant, Waveney, Chet and Wensum. There are no locks on any of the rivers (except for Mutford lock in Oulton Broad that links to the saltwater Lake Lothing in Lowestoft), all the waterways are subject to tidal influence. The tidal range decreases with distance from the sea, with highly tidal areas such as Breydon Water contrasted with effectively non-tidal reaches such as the River Ant upstream of Barton Broad.
The broads themselves range in size from small pools to the large expanses of Hickling Broad, Barton Broad and Breydon Water. The broads are unevenly distributed, with far more broads in the northern half of Broadland (the Rivers Bure, Thurne and Ant) than in the central and southern portions (the Rivers Yare, Waveney, Chet and Wensum). Individual broads may lie directly on the river, or are more often situated to one side and connected to the river by an artificial channel or dyke.
Besides the natural watercourses of the rivers, and the ancient but artificial broads, there is one more recent navigation canal, the lock-less New Cut which connects the Rivers Yare and Waveney whilst permitting boats to by-pass Breydon Water.
There is also a second navigable link to the sea, via the River Waveney and its link to Oulton Broad. Oulton Broad is part of the Broads tidal system, but is immediately adjacent to Lake Lothing which is itself directly connected to the sea via the harbour at Lowestoft. Oulton Broad and
In the lists below, names of broads are emboldened to help distinguish them from towns and villages.
5. Queen Elizabeth Park, British Columbia
Queen Elizabeth Park is a municipal park located in Vancouver, British Columbia, on Little Mountain (elevation approximately 168 metres (550 feet) above sea level). Its surface was scarred at the turn of the twentieth century when it was quarried for its rock, which served to build
History
In 1930, the park’s floral future was somewhat revealed when the BC Tulip Association suggested the notion of transforming the quarries into sunken gardens. By the end of that decade, the site had been turned over to the Vancouver Park Board for park and recreation purposes, and was dedicated as such by King George VI and his consort, Queen Elizabeth (the present Queen’s late mother) on their much lauded visit to Vancouver in 1939, as King and Queen of Canada. From that time, Park staff incrementally transformed the overgrown hillsides into
Prentice Bloedel’s $1.25 million covered the open reservoirs and built the country’s first geodesic conservatory surrounded by covered walkways, lighted fountains and a magnificent sculpture (Knife Edge - Two Piece) by modern artist Henry Moore. The Bloedel Floral Conservatory opened on December 6, 1969 amidst much jubilation with its many climatic zones, displaying a huge variety of plants and a superb selection of free flying tropical birds.
Attractions
There are several other attractions in the park. These include a pitch and putt golf course, a disc golf course, tennis courts, a lawn bowling club, and a restaurant.
A view of the park
New Forest
The New Forest is an area of southern England which includes the largest remaining tracts of unenclosed pasture land, heathland and forest in the heavily-populated south east of England. It covers south west Hampshire and some of contiguous southeast Wiltshire.
The name also refers to the
The highest point in the
6. History of the New Forest
Like much of
The
As of 2005, roughly ninety per cent of the
Formal commons rights were confirmed by statute in 1698. Over time, the
The naval plantations encroached on the rights of the Commoners, but the
Felling of broadleaf trees, and replacement by conifers, began during the First World War to meet the wartime demand for wood. Further encroachments were made in the Second World War. This process is today being reversed in places, with some plantations being returned to heathland or broadleaf woodland.
Further New Forest Acts followed in 1949, 1964 and 1970. The
Edward Rutherfurd’s work of historical fiction, The Forest, is based in the
New Forest National Park
Consultations on the possible designation of a National Park in the
On 28 June 2004, Rural Affairs Minister Alun Michael confirmed the government’s intention to designate the area as a National Park, with further detailed boundary adjustments. The area was formally designated as such on 1 March 2005. A National Park Authority for the
The designated area of the National Park covers 571 km² (141097 acres) and includes many existing SSSIs. It has a population of approximately 38,000 (excluding most of the 170,256 people who live in the New Forest local government district). As well as most of the New Forest district of Hampshire, it takes in the South Hampshire Coast Area of Outstanding Natural Beauty, a small corner of Test Valley district around the village of Canada and part of the Salisbury district in Wiltshire south-east of Redlynch.
However, the area covered by the park does not include all the areas which were initially proposed; excluding most of the valley of the River Avon to the west of the forest and Dibden Bay to the east. Two challenges were made to the designation order, by Meyrick Estate Management Ltd in relation to the inclusion of Hinton Admiral Park, and by RWE Npower Plc to the inclusion of Fawley Power Station. The second challenge was settled out of court, with the power station being excluded. The High Court upheld the first challenge; [13] but an appeal against the decision was then heard by the Court of Appeal in Autumn 2006. The final ruling, published on 15 February 2007, found in favour of the challenge by Meyrick Estate Management Ltd, [14] and the land at
Geography
The New Forest Heritage Area covers about 580 km² (143321 acres), and the New Forest SSSI covers almost 300 km² (74131 acres), making it the largest contiguous area of un-sown vegetation in lowland
146 km² (36077 acres) of broadleaf woodland
118 km² (29158 acres) of heathland and grassland
33 km² (8154 acres) of wet heathland
84 km² (20756 acres) of tree plantations (“inclosures”) established since the 18th century, including 80 km² (19768 acres) planted by the Forestry Commission since the 1920s.
It is drained to the south by two rivers, the Lymington and Beaulieu.
7. Exmoor
Exmoor is a National Park situated on the Bristol Channel coast of south west
Prior to being a park, Exmoor was a Royal Forest and hunting ground, which was sold off in 1818. Exmoor was one of the first British National Parks, designated in 1954, under the 1949 National Parks and Access to the Countryside Act, [1] and is named after the main river that flows out of the district, the River Exe.
Several areas of the moor have been declared a Site of Special Scientific interest due to the flora and fauna. This title earns the site some legal protection from development, damage, and neglect. In 1993
History
There is evidence of occupation of the area by people from times, onward. In the Neolithic period, people started to manage animals and grow crops on farms cleared from the woodland, rather than act purely as hunters and as gatherers It is also likely that extraction and smelting of mineral ores to make metal tools, weapons, containers and ornaments started in the late Neolithic, and continued into the bronze and iron ages. An earthen ring at Parracombe is believed to be a Neolithic henge dating from 5000-4000 BC, and “
Holwell Castle, at Parracombe, was a Norman motte and bailey castle built to guard the junction of the east-west and north-south trade routes, enabling movement of people and goods and the growth of the population Alternative explanations for its construction suggest it may have been constructed to obtain taxes at the River Heddon bridging place, or to protect and supervise silver mining in the area around Combe Martin. It was 131 feet (40 m) in diameter and 20 feet (6 m) high above the bottom of a rock cut ditch which is 9 feet (3 m) deep. It was built, in the late 11th or early 12th century, of earth with timber palisades for defence and a one or two storey wooden dwelling. It was probably built by either Martin de Tours, the first lord of Parracombe, William de Falaise (who married Martin’s widow) or Robert FitzMartin, although there are no written records to validate this. The earthworks of the castle are still clearly visible from a nearby footpath, but there is no public access to them. During the Middle Ages, sheep farming for the wool trade came to dominate the economy. The wool was spun into thread on isolated farms and collected by merchants to be woven, fulled, dyed and finished in thriving towns such as Dunster. The land started to be enclosed and from the 17th century onwards larger estates developed, leading to establishment of areas of large regular shaped fields. During the 16th and 17th centuries the commons were overstocked with agisted livestock, from farmers outside the immediate area who were charged for the privilege. This led to disputes about the number of animals allowed and the enclosure of land. During this period a Royal Forest and hunting ground was established, administered by a warden, so that king Charles I could benefit from the fines and rents.
In the mid-17th century John Boevey was the warden. He built a house at Simonsbath, and for 150 years it was the only house in the forest. The
In the mid-19th century a mine was developed alongside the River Barle. The mine was originally called Wheal Maria, then changed to Wheal Eliza. It was a copper mine from 1845-54 and then an iron mine until 1857, although the first mining activity on the site may be from 1552 At Simonsbath, a restored Victorian water-powered sawmill, which was damaged in the floods of 1992, has now been purchased by the National Park and returned to working order; it is now used to make the footpath signs, gates, stiles, and bridges for various sites in the park
Geology
Exmoor is an upland of sedimentary rocks classified as gritstones, sandstones, slate, shale and limestone, siltstones, and mudstones depending on the particle size. They are largely from the Devonian and early Carboniferous periods (the name Devonian comes from
Coastline
Exmoor has 34 miles (55 km) of coastline, including the highest cliffs in
Exmoor’s woodlands sometimes reach the shoreline, especially between Porlock and The Foreland, where they form the single longest stretch of coastal woodland in
The scenery of rocky headlands, ravines, waterfalls and towering cliffs gained the Exmoor coast recognition as a Heritage Coast in 1991. With its huge waterfalls and caves, this dramatic coastline has become an adventure playground for both climbers and for explorers. The cliffs provide one of the longest and most isolated seacliff traverses in the
Flora
Dunkery Beacon, with heather in bloom
Uncultivated heath and moorland cover about a quarter of
Fauna
A herd of
Sheep have grazed on the moors for more than 3,000 years, shaping much of the
Red deer have a stronghold on the moor and can be seen on quiet hillsides in remote areas, particularly in the early morning. The moorland habitat is also home to hundreds of species of birds and insects. Birds seen on the moor include Merlin, Peregrine Falcon, Eurasian Curlew, European Stonechat, Dipper, Dartford Warbler and Ring Ouzel. Black Grouse and Red Grouse are now extinct on
Beast of
The Beast of Exmoor is a cryptozoological cat (see phantom cat) that is reported to roam
Places of interest
The attractions of
Inland, many of the attractions are centred around small towns and villages or linked to the river valleys, such as the ancient clapper bridge at Tarr Steps and the Snowdrop Valley near Wheddon Cross, which is carpeted in snowdrops in Februaryand, later, displays bluebells. Withypool is also in the
Exmoor has been the setting for several novels including the 19th-century Lorna Doone: A Romance of Exmoor by Richard Doddridge Blackmore, and Margaret Drabble’s 1998 novel The Witch of Exmoor. The park was featured on the television programme Seven Natural Wonders twice, as one of the wonders of the West Country.
8. Yorkshire Dales
The Yorkshire Dales (also known as The Dales) is the name given to an upland area, in
The area lies within the historic county boundaries of Yorkshire, though it spans the ceremonial counties of North Yorkshire, West Yorkshire, and Cumbria. Most of the area falls within the Yorkshire Dales District National Park, created in 1954, and now one of the twelve National parks of England and Wales (not including the South Downs which is due to become one).
The Dales is a collection of river valleys and the hills in between them, rising from the Vale of York westwards to the hilltops of the main Pennine watershed (the British English meaning). In some places the area even extends westwards across the watershed, but most of the valleys drain eastwards to the Vale of
The word dale comes from a Nordic/Germanic word for valley, and occurs in valley names across Yorkshire (and northern England generally) but since the creation of the Yorkshire Dales National park, the name Yorkshire Dales has come to refer specifically to these western dales and the area of dales and hills east of the Vale of York is now called the North York Moors after the National Park created there
Yorkshire Dales National Park
In 1954 an area of 1,770 square kilometres (680 sq mi) was designated the Yorkshire Dales National Park. Most of the National Park is in North Yorkshire, though part lies within Cumbria. However, the whole park lies within the traditional boundaries of Yorkshire, divided between the North Riding and the West Riding. The park is 50 miles (80 km) north east of Manchester; Leeds and Bradford lie to the south, while Kendal is to the west and
Over 20,000 residents live and work in the park, which attracts over eight million visitors every year. The area has a large collection of activities for visitors. For example, many people come to the “Dales” for walking or exercise. The National Park is crossed by several long-distance routes including the Pennine Way, the Dales Way, the Coast to Coast Path and the latest national trail - the Pennine Bridleway. Cycling is also popular and there are several cycleways.
The Park has its own museum, the Dales Countryside Museum, housed in a conversion of the Hawes railway station in Wensleydale in the north of the Park. The park has 5 visitor centres located in major destinations in the park. These are at:
Geography
Most of the dales in the Yorkshire Dales are named after their river or stream (eg Arkengarthdale, formed by Arkle Beck). The best-known exception to this rule is Wensleydale, which is named after the town of
Geographically, the classical Yorkshire Dales spread to the north from the market and spa towns of Settle, Deepdale near Dent, Skipton, Ilkley and Harrogate in North Yorkshire, with most of the larger southern dales (e. g. Ribblesdale, Malhamdale and Airedale, Wharfedale and Nidderdale) running roughly parallel from north to south. The more northerly dales (e. g. Wensleydale, Swaledale and Teesdale) running generally from west to east. There are also many other smaller or lesser known dales (e. g. Arkengarthdale, Barbondale, Bishopdale, Clapdale, Coverdale, Dentdale and Deepdale, Garsdale, Kingsdale, Littondale, Langstrothdale, Raydale, Waldendale and the Washburn Valley) whose tributary streams and rivers feed into the larger valleys. [1]
The characteristic scenery of the “Dales” is green upland pastures separated by dry-stone walls and grazed by sheep and cattle. The dales themselves are ‘U’ and ‘V’ shaped valleys, which were enlarged and shaped by glaciers, mainly in the most recent, Devensian ice age. The underlying rock is principally Carboniferous limestone (which results in a number of areas of limestone pavement) in places interspersed with shale and sandstone and topped with millstone grit. However, to the north of the Dent fault, the hills are principally older Silurian and Ordovician rocks, which make up the Howgill Fells.
Many of the upland areas consist of heather moorland, used for grouse shooting in the months following 12 August each year (the ‘Glorious Twelfth’).
Cave systems
Gaping Gill
Because of the limestone that runs throughout the “Dales” there are extensive cave systems present across the area making it one of the major areas for caving in the
9. Lake District
The Lake District, also known as The Lakes or
The central and most-visited part of the area is contained in the Lake District National Park, one of fourteen National Parks in the United Kingdom. It lies entirely within Cumbria, and is one of
General geography
The
In Neolithic times, the Lake District was a major source of stone axes, examples of which have been found all over
Since Roman times, farming, in particular of sheep, was the major industry in the region. 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. There are extensive plantations of non-native pine trees.
The area was badly affected by the foot-and-mouth outbreak across the United Kingdom in 2001. Thousands of sheep, grazing 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 re-learnt 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".
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 century to the 19th century. 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 fell-sides 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
Development of tourism
Early visitors to the Lake District, who travelled for the education and pleasure of the journey, include Celia Fiennes who in 1698 undertook a journey the length of England, including riding through Kendal and over Kirkstone Pass into Patterdale. Her experiences and impressions were published in her book Great Journey to Newcastle and Cornwall:
As I walked down at this place I was walled on both sides by those inaccessible high rocky barren hills which hang over one’s head in some places and appear very terrible; and from them springs many little currents of water from the sides and clefts which trickle down to some lower part where it runs swiftly over the stones and shelves in the way, which makes a pleasant rush and murmuring noise and like a snowball is increased by each spring trickling down on either side of those hills, and so descends into the bottoms which are a Moorish ground in which in many places the waters stand, and so form some of those Lakes as it did here.
In 1724, Daniel Defoe published the first volume of A Tour Thro' the Whole Island of Great Britain. He commented on Westmorland that it was:
the wildest, most barren and frightful of any that I have passed over in England, or even Wales itself; the west side, which borders on Cumberland, is indeed bounded by a chain of almost unpassable mountains which, in the language of the country, are called fells.
Towards the end of the 18th century, the area was becoming more popular with travellers. This was partly a result of wars in Continental Europe, restricting the possibility of travel there. In 1778 Father Thomas West produced A Guide to the Lakes, which began the era of modern tourism.
West listed "stations"-viewpoints where tourists could enjoy the best views of the landscape, being encouraged to appreciated the formal qualities of the landscape and to apply aesthetic values. At some of these stations, buildings were erected to help this process. The remains of Claife Station (on the western
William Wordsworth published his Guide to the Lakes in 1810, and by 1835 it had reached its fifth edition, now called A Guide through the District of the Lakes in the North of England. This book was particularly influential in popularising the region. Wordsworth's favourite valley was Dunnerdale or the Duddon Valley nestling in the south-west of the
The railways led to another expansion in tourism. The Kendal and Windermere Railway was the first to penetrate the
The growth in tourist numbers continued into the age of the motor car, when railways began to be closed or run down. The formation of the Lake District National Park in 1951 recognised the need to protect the
Whilst the roads and railways provided easier access to the area, many people were drawn to the Lakes by the publication of the Pictorial Guide to the Lakeland Fells by Alfred Wainwright. First published between 1952 and 1965, these books provided detailed information on 214 peaks across the region, with carefully hand-drawn maps and panoramas, and also stories and asides which add to the colour of the area. They are still used by many visitors to the area as guides for walking excursions, with the ultimate goal of bagging the complete list of Wainwrights. The famous guides are being revised by Chris Jesty to reflect changes, mainly in valley access and paths.
Since the early 1960s, the park has hired rangers to monitor the grounds to cope with increasing tourism and development, the first being John Wyatt, who has since written a number of guide books. He was joined two years later by a second, and since then the number of rangers has been rising.
The area has also become associated with writer Beatrix Potter. A number of tourists visit to see her family home, with particularly large numbers coming from Japan.
Tourism has now become the park's major industry, with about 14 million visitors each year, mainly from the
Cultural tourism is becoming an increasingly important part of the wider tourist industry. The
Conclusion
When I was doing this project I learned a lot of incredible and interesting information about the parks.
For exmaple: That Dartmoor has inspired a number of artists and writers, such as Sir Arthur Conan Doyle in The Hound of the Baskervilles and The Adventure of Silver Blaze, Eden Phillpotts, Beatrice Chase, Agatha Christie and the Reverend Sabine Baring-Gould. And that the first roads in the
After this I can do my own conclusion: despite the fact that all of the parks British, they are totally different. Each its own history, legends ect. Each is unique. Humanity must establish and maintain such beautiful place on Earth.
Additional material
Bovey Castle. Dartmoor National ParkVillarrica
Lake District ParkHotel
Queen Elizabeth Park
Yorkshire Dales National Park
Dartmoor National Park
Literature
1. www.wikipedia.com
2. www.travel.com
3. www.greatbritan.com
4. www.tour-england.net
5. www.visitnewforest.com
