The National Parks of Great Britan (стр. 3 из 5)
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 New Forest National Park which has similar boundaries. Additionally the New Forest local government district is a subdivision of Hampshire which covers most of the forest, and some nearby areas although it is no longer the planning authority for the National Park. There are many small villages dotted around the area.
The highest point in the New Forest is Piper’s Wait, just west of Bramshaw. Its summit is at 125 m (410 ft) above mean sea level
6. History of the New Forest
Like much of England, the New Forest was originally woodland, but parts were cleared for cultivation from the Stone Age and into the Bronze Age. However, the poor quality of the soil in the new forest meant that the cleared areas turned into heathland “waste”. There are around 250 round barrows [1] within its boundaries, and scattered boiling mounds, and it also includes about 150 scheduled ancient monuments.
The New Forest was created as a royal forest around 1080by William the Conqueror for the hunting of (mainly) deer. It was first recorded as “Nova Foresta" in the Domesday Book in 1086, and is the only forest that the book describes in detail. Twelfth-century chroniclers alleged that William had created the forest by evicting the inhabitants of thirty-six parishes, reducing a flourishing district to a wasteland; however, this account is dubious, as the poor soil in much of the forest is incapable of supporting large-scale agriculture, and significant areas appear to have always been uninhabited. Two of William’s sons died in the forest, Prince Richard in 1081 and William Rufus in 1100. The reputed spot of the Rufus’ death is marked with a stone known as the Rufus Stone.
As of 2005, roughly ninety per cent of the New Forest is still owned by the Crown. The Crown lands have been managed by the Forestry Commission since 1923. Around half of the Crown lands fall inside the new National Park.
Formal commons rights were confirmed by statute in 1698. Over time, the New Forest became a source of timber for the Royal Navy, and plantations were deliberately created in the 18th century for this specific purpose. In the Great Storm of 1703, about four thousand oak trees were lost in the New Forest.
The naval plantations encroached on the rights of the Commoners, but the Forest gained new protection under an Act of Parliament in 1877. The New Forest Act 1877 confirmed the historic rights of the Commoners and prohibited the enclosure of more than 16,000 acres (65 km²) at any time. It also reconstituted the Court of Verderers as representatives of the Commoners (rather than the Crown).
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 New Forest became a Site of Special Scientific Interest in 1971, and was granted special status as the “New Forest Heritage Area” in 1985, with additional planning controls added in 1992. The New Forest was proposed as a UNESCO World Heritage Site in June 1999,and it became a National Park in 2005.
Edward Rutherfurd’s work of historical fiction, The Forest, is based in the New Forest in the time period from 1099 through 2000.
New Forest National Park
Consultations on the possible designation of a National Park in the New Forest were commenced by the Countryside Agency in 1999. An order to create the park was made by the Agency on 24 January 2002 and submitted to the Secretary of State for confirmation in February 2002. Following objections from seven local authorities and others, a Public Inquiry was held from 8 October 2002 to 10 April 2003, concluding with that the proposal should be endorsed with some detailed changes to the boundary of the area to be designated.
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 New Forest was established on 1 April 2005 and assumed its full statutory powers on 1 April 2006. The Forestry Commission retain their powers to manage the Crown land within the Park, and the Verderers under the New Forest Acts also retain their responsibilities, and the Park Authority is expected to co-operate with these bodies, the local authorities, English Nature and other interested parties.
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 Hinton Admiral Park is therefore excluded from the New Forest National Park.
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 Britain. It includes roughly:
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 England. The park straddles two counties, with 71% of the park located in Somerset and 29% located in Devon. The total area of the park, which includes the Brendon Hills and the Vale of Porlock, covers 267 square miles (691.5 km2) of hilly open moorland and includes 34 miles (55 km) of coast. It is primarily an upland area with a dispersed population living mainly in small villages and hamlets. The largest settlements are Porlock, Dulverton, Lynton, and Lynmouth, which together contain almost 40% of the National Park population. Lynton and Lynmouth are combined into one parish and are connected by the Lynton and Lynmouth Cliff Railway.
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 Exmoor was also designated as an Environmentally Sensitive Area.
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 “Cow Castle", which is where White Water meets the River Barle, is an Iron Age fort at the top of a conical hill. [25] Tarr Steps are a prehistoric (circa 1000 BC) clapper bridge across the River Barle, about 2.5 miles (4 km) south east of Withypool and 4 miles (6 km) north west of Dulverton. The stone slabs weigh up to 5 long tons (5,080 kg) apiece and the bridge has been designated by English Heritage as a grade I listed building, to recognise its special architectural, historical or cultural significance. There is little evidence of Roman occupation apart from two fortlets on the coast
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 Royal Forest was sold off in 1818. The Simonsbath House was bought along with the accompanying farm by John Knight for the sum of £50,000. Knight set about converting the Royal Forest into agricultural land. He and his family built most of the large farms in the central section of the moor, and built 22 miles (35 km) of metalled access roads to Simonsbath. He built a 29-mile (47 km) wall around his estate, much of which still survives.
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 Devon, as rocks of that age were first studied and described here). As this area of Britain was not subject to glaciation, the plateau remains as a remarkably old landform. Quartz and iron mineralisation can be detected in outcrops and subsoil. The Glenthorne area demonstrates the Trentishoe Formation of the Hangman Sandstone Group. The Hangman Sandstone represents the Middle Devonian sequence of North Devon and Somerset. These unusual freshwater deposits in the Hangman Grits, were mainly formed in desert conditions. The underlying rocks are covered by moors and supported by wet, acid soil. The highest point on Exmoor is Dunkery Beacon; at 1,704 feet (519 m) it is also the highest point in Somerset.
Coastline
Exmoor has 34 miles (55 km) of coastline, including the highest cliffs in England, which reach a height of 1,350 feet (411 m) at Culbone Hill. However, the crest of this coastal ridge of hills is more than a mile (1.6 km) from the sea. If a cliff is defined as having a slope greater than 60 degrees, the highest cliff on mainland Britain is Great Hangman near Combe Martin at 1,043 feet (318 m) high, with a cliff face of 800 feet (244 m). Its sister cliff is the 716 feet (218 m) Little Hangman, which marks the edge of Exmoor.
Exmoor’s woodlands sometimes reach the shoreline, especially between Porlock and The Foreland, where they form the single longest stretch of coastal woodland in England and Wales. The Exmoor Coastal Heaths have been recognised as a Site of Special Scientific Interest due to the diversity of plant species present.
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 UK. The South West Coast Path, at 630 miles (1,014 km) the longest National Trail in England and Wales, starts at Minehead and runs along all of Exmoor’s coast. There are small harbours at Lynmouth, Porlock Weir, and Combe Martin. Once crucial to coastal trade, the harbours are now primarily used for pleasure; individually owned sail boats and non-commercial fishing boats are often found in the harbours
Flora
Dunkery Beacon, with heather in bloom
Uncultivated heath and moorland cover about a quarter of Exmoor landscape. Some moors are covered by a variety of grasses and sedges, while others are dominated by heather. There are also cultivated areas including the Brendon Hills, which lie in the east of the National Park. There are also 32.4 square miles (84 km2) of woodland, comprising a mixture of broad-leaved (oak, ash and hazel) and conifer trees. Horner Woodlands and Tarr Steps woodlands are prime examples. The country’s highest beech wood, 1, 200 feet (366 m) above sea level, is at Birch Cleave at Simonsbath. At least two species of whitebeam tree: Sorbus subcuneata and Sorbus ‘Taxon D’ are unique to Exmoor. These woodlands are home to lichens, mosses and ferns. Exmoor is the only national location for the lichens Biatoridium delitescens, Rinodina fimbriata and Rinodina flavosoralifera, the latter having been found only on one individual tree.