81-817: The Monsal Trail is a cycling, horse riding and walking trail in the Derbyshire Peak District . It was constructed from a section of the former Manchester, Buxton, Matlock and Midland Junction Railway , which was built by the Midland Railway in 1863 to link Manchester with London and closed in 1968. The Monsal Trail is about 8.5 miles (13.7 km) long and opened in 1981. It starts at the Topley Pike junction in Wye Dale , 3 miles (4.8 km) east of Buxton , and runs to Coombs Viaduct, 1 mile (1.6 km) south-east of Bakewell . It follows
162-607: A continuous flow in the River Etherow , which was essential for local industry and provided drinking water for Manchester. In a report for the Manchester Corporation , John Frederick Bateman wrote in 1846: Within ten or twelve miles of Manchester, and six or seven miles from the existing reservoirs at Gorton, there is this tract of mountain land abounding with springs of the purest quality. Its physical and geological features offer such peculiar features for
243-418: A cotton mill in 1783, powered by water from Cressbrook stream. It was built on the site of a distillery by William Newton of Abney. The original building was destroyed by fire. Litton Mill was a large cotton spinning mill that opened in 1782. It was notorious for the harsh treatment of child labourers by the owner, Ellis Needham. Many of the children, brought from London and other large cities, died young from
324-590: A few of the foods available). Some of the largest populations of water voles in Britain can also be found along the River Wye. It is possible to walk alongside much of the length of the river, mostly following a former railway line, part of which is now the Monsal Trail and provides views of the river. In Monsal Dale the former railway line emerges from a tunnel at Monsal Head, over a viaduct high above
405-533: A higher standard. The early Arkwright mills were of light construction, narrow, about 9 feet (2.7 m) wide and low, the ceiling height being only 6 to 8 feet (1.8 to 2.4 m) and lit by daylight. The new machines were powered by water wheels . The Peak was the ideal location, with its rivers and humid atmosphere. The local pool of labour was quickly exhausted and Litton Mill and Cressbrook Mill in Millers Dale brought in children as young as four from
486-487: A journey through the Peak in 1697, wrote of: ...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 is a great deale of silver. Coal measures occur on the Peak's western and eastern fringes. Evidence of past workings can be found from Glossop to The Roaches , and from Stocksbridge to Baslow . The coal measures in
567-620: A railway is not supported by the council, and was last rejected in October 2022. The Monsal Trail is about 8.5 miles (13.7 km) long and opened in 1981. It starts at the Topley Pike junction (in Wye Dale, 3 miles (4.8 km) east of Buxton ) and runs to Coombs Viaduct, 1 mile (1.6 km) south-east of Bakewell . It follows the valley of the River Wye and runs parallel to the A6 . From
648-717: A section of the former Manchester, Buxton, Matlock and Midlands Junction Railway , built by the Midland Railway in 1863 to link Manchester with London. The line was closed in 1968 by the Labour Minister for Transport Barbara Castle , not by the Beeching Axe , and remained unused for twelve years before being taken over by the Peak District National Park . The route through the Wye valley
729-540: Is a show cave . Small-scale mining takes place in Treak Cliff Cavern . Industrial limestone quarrying to make soda ash started around Buxton in 1874. In 1926 the operation of the Buxton lime industry became part of ICI . Large-scale limestone and gritstone quarrying flourished as lead mining declined, and is an important if contentious industry. Of the twelve large limestone quarries in operation, Tunstead
810-510: Is a by-product of fluorite, baryte and calcite mining. Bell pits were sunk to access ore that lay close to the surface. Fluorite or fluorspar is called Blue John locally, its name possibly from the French bleu et jaune describing its colour. Blue John is scarce and now only a few hundred kilograms are mined each year for ornamental and lapidary use. The Blue John Cavern in Castleton
891-496: Is a native perennial of limestone cliffs discovered by J. N. Mills in 1966 and described as a new species in 1968; and leek-coloured hawkweed ( H. subprasinifolium ), which was believed extinct until rediscovered on banks beside the Monsal Trail in Chee Dale in 2017. The endemic Derbyshire feather moss ( Thamnobryum angustifolium ) occurs in one Derbyshire limestone dale, its sole world location intentionally kept confidential;
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#1732793652931972-645: Is an upland area in central-northern England, at the southern end of the Pennines . Mostly in Derbyshire , it extends into Cheshire , Greater Manchester , Staffordshire , West Yorkshire and South Yorkshire . It is subdivided into the Dark Peak , moorland dominated by gritstone , and the White Peak , a limestone area with valleys and gorges. The Dark Peak forms an arc on the north, east and west of
1053-604: Is gone, and the Gods with it; and now, every fool in Buxton can be in Bakewell in half an hour, and every fool in Bakewell at Buxton; which you think a lucrative process of exchange – you Fools everywhere. His words are displayed on the viaduct. When the railway closed and there was talk of demolishing the viaduct, there was considerable opposition. In 1970 it was designated as a Grade II listed building. Cressbrook Mill opened as
1134-498: Is higher. The higher rainfall does not affect the temperature, which averages the same as the rest of England and Wales at 10.3 °C (50.5 °F). In the 1970s, the Dark Peak regularly had more than 70 days of snowfall. Since then the number has fallen. The hills still see long periods of continuous snow cover in some winters. Snow in mid-December 2009 on some hill summits created some snow patches that lasted until May 2010. In
1215-467: Is marked by millstone grit outcrops and broad swathes of moorland. Earth movements after the Carboniferous period resulted in the up-doming of the area and, particularly in the west, the folding of the rock strata along north–south axes. The region was raised in a north–south line which resulted in the dome-like shape and the shales and sandstones were worn away until limestone was exposed. At
1296-565: Is on a track near Deer Hill in Meltham ; its southernmost point is on the A52 road near Ashbourne . The boundaries were drawn to exclude built-up and industrial areas; in particular Buxton and the quarries at the end of the Peak Dale corridor are surrounded on three sides by the park. Bakewell and many villages are in the national park, as is much of the rural west of Sheffield. In 2010 it became
1377-453: Is one of the largest in Europe. Total limestone output was substantial: at the 1990 peak, 8.5 million tonnes was produced. Textiles have been exported for hundreds of years. In the 14th century, the area traded in unprocessed wool. There were several skilled hand spinners and weavers in the area. By the 1780s, Richard Arkwright had developed machinery to produce textiles faster and to
1458-519: Is one of the more impressive structures on the line, although when built it was seen as destroying the beauty of the dale. John Ruskin , a poet and conservationist of the time, criticised the building of the railway: There was a rocky valley between Buxton and Bakewell, once upon a time, divine as the Vale of Tempe... You Enterprised a Railroad through the valley – you blasted its rocks away, heaped thousands of tons of shale into its lovely stream. The valley
1539-403: Is popular with anglers because of the large numbers of wild brown , rainbow trout and grayling it contains. The alkalinity of the Wye provides a rich source of nutrients that leads to an abundance of insects, invertebrates and other wildlife. This ensures that the trout and grayling grow quickly on a diet of freshwater shrimp, caddisfly (also known as sedge-flies) and mayfly (to name but
1620-643: Is the largest settlement and only town in the national park and the site of the National Park Authority offices. Its five-arched bridge over the River Wye dates from the 13th century. Castleton is the centre of production of a semi-precious mineral, Blue John . Eyam village is known for a self-imposed quarantine during the Black Death . Edale is the southern end of the Pennine Way , a 268-mile national trail which traverses most of
1701-749: Is the most prominent. It rises on Bleaklow just east of Glossop and flows through the Upper Derwent Valley , where it is constrained by the Howden , Derwent and Ladybower reservoirs . The reservoirs of the Upper Derwent Valley were built from the early to mid-20th century to supply drinking water to the East Midlands and South Yorkshire. The rivers Noe and the Wye are tributaries. The River Manifold and River Dove in
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#17327936529311782-556: Is used for recreation purposes by cyclists, walkers, horse riders, wheelchair users and joggers. A 5 km Parkrun , run entirely on the Monsal Trail, takes place every Saturday morning at 9am; it starts at Hassop railway station, passing Thornbridge Hall , continuing to Headstone tunnel and then turning around to finish where it began. 53°14′41″N 1°43′54″W / 53.2447°N 1.7317°W / 53.2447; -1.7317 Peak District The Peak District
1863-459: The Dark Peak and White Peak , but the wider Peak District is less well defined. The Dark Peak is largely uninhabited moorland and gritstone escarpments in the northern Peak District and its eastern and western margins. It encloses the central and southern White Peak, which is where most settlements, farmland and limestone gorges are found. Three of Natural England 's National Character Areas (NCAs) cover parts of it. The Dark Peak NCA includes
1944-606: The Mesolithic era; it was largely used for agricultural purposes until mining arose in the Middle Ages. During the Industrial Revolution , several cotton mills were constructed in the area's valleys by Richard Arkwright . As mining declined, quarrying grew. Tourism came with the railways, spurred by the landscape, spa towns and Castleton 's show caves. The Peak District forms the southern extremity of
2025-820: The RSPB 's publication of Peak Malpractice , a 2006 report highlighting wildlife crime, the Peak District Bird of Prey Initiative was set up in 2011 by conservationists and shooting bodies to try to boost populations of birds of prey. The park authorities expressed disappointment at the limited results and the RSPB withdrew from the partnership in January 2018 citing continued efforts by the Moorland Association and National Gamekeepers’ Organisation which together had "frustrated any possibility of progress" on
2106-481: The anomalous , broom moth , dot moth , garden dart , mouse moth and white ermine . Other invertebrates include the bilberry bumblebee , broad groove-head spider , mole cricket , northern yellow splinter , shining guest ant , violet oil beetle and white-clawed crayfish . The Peak District National Park was the first national park to be designated in the United Kingdom, on 17 April 1951 (following
2187-488: The coal measures that occur only on the margins and infrequent outcrops of igneous rocks , including lavas , tuffs and volcanic vent agglomerates . The general geological structure is that of a broad dome , whose western margins have been intensely faulted and folded . Uplift and erosion have sliced the top off the Derbyshire Dome to reveal a concentric outcrop pattern with coal-measured rocks on
2268-473: The workhouses of London as apprentices. As technology advanced, narrow valleys proved unsuited to larger steam-driven mills, but Derbyshire mills remained to trade in finishing and niche products. Glossop benefited from the textile industry. Its economy was tied to a spinning and weaving tradition that evolved from developments in textile manufacture during the Industrial Revolution . Until
2349-680: The 1940s onwards, but may now be extinct. Red deer herds, assumed to be derived from animals escaped from deer parks at Lyme Park and Chatsworth , are established in the upper reaches of the Goyt valley and on the moors above Baslow , and a herd on Wharncliffe Crags outside the national park north of Sheffield may derive from hunting stock of Wharncliffe Chase. Biodiversity action plans have been prepared for mountain hare, brown hare , brown long-eared bat , dormouse , harvest mouse , hedgehog , noctule bat , otter , pine marten , polecat , soprano pipistrelle and water vole . The status of
2430-600: The First World War, Glossop was the headquarters of the largest textile printworks in the world, but after the Wall Street crash its product lines became vulnerable and the industry declined. River Wye, Derbyshire The River Wye is a limestone river in the Peak District of Derbyshire , England. It is 22 miles long (widely but incorrectly attributed as 15 miles/24 km, which refers to
2511-628: The National Parks and Access to the Countryside Act of 1949 and a resulting public enquiry to establish its boundary). It was one of ten parks created in the 1950s in the wake of the 1945 Dower Report and 1947 Hobhouse Report, which recommended the creation of national parks in England and Wales. The park has an area of 1,438 square kilometres (555 sq mi) and receives approximately 13 million visitors each year. 90% of
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2592-480: The Peak District was once inhabited by an eclectic mix of species, many of them no longer found in Britain, such as alpine swift , demoiselle crane and long-legged buzzard . Species lost from the Peak District through human activity include hazel grouse , capercaillie and golden eagle . Amphibians and reptiles such as common lizards , grass snakes , great crested newts and slow worms are found in
2673-551: The Pennines and ends at Kirk Yetholm in the Scottish border . The park also contains the highest village in the United Kingdom, Flash , at 1,519 feet (463 m). Other villages in the park include Hathersage , Hartington , Ilam and Tideswell . The towns of Glossop , Chapel-en-le-Frith , Buxton , Macclesfield , Leek , Ashbourne, Matlock and Chesterfield are on the national park's fringes. The spa town of Buxton
2754-517: The Pennines. Much of it is upland above 1,000 feet (300 m), its highest point being Kinder Scout at 2,087 ft (636 m). Despite its name, the landscape has fewer sharp peaks than rounded hills, plateaus , valleys, limestone gorges and gritstone escarpments (the "edges"). The mostly rural area is surrounded by conurbations and large urban areas, including Manchester , Huddersfield , Sheffield , Derby and Stoke-on-Trent . The national park has formal boundaries. It covers most of
2835-977: The South West Peak NCA. The limestone plateaus of the White Peak are more intensively farmed, with mainly dairy usage of improved pastures. Woodland forms some 8 per cent of the Peak National Park. Natural broad-leaved woodland appears in the steep dales of the White Peak and cloughs of the Dark Peak. Reservoir margins often have coniferous plantations. White Peak habitats include calcareous grassland , ash woodlands and rock outcrops for lime-loving species. They include early purple orchid ( Orchis mascula ), dark-red helleborine ( Epipactis atrorubens ) and fly orchid ( Ophrys insectifera ), common rockrose ( Helianthemum nummularium ), spring cinquefoil ( Helianthemum nummularium ) and grass of parnassus ( Parnassia palustris ). Lead rakes,
2916-611: The White Peak fed the Cromford Canal . The Peak Forest Canal brought lime from the quarries at Dove Holes for the construction industry. It terminated at Bugsworth Basin and the journey was completed using the Peak Forest Tramway . The Cromford Canal, from Cromford to the Erewash Canal , served lead mines at Wirksworth and Sir Richard Arkwright 's cotton mills. The Caldon Canal from Froghall
2997-643: The Wyedale car park, the easiest access point for the northern end of the trail, there is a walk of about 1 kilometre (0.62 mi), with the last part up steps, to reach the trail. Starting at the south of the trail, "from Market Place in Bakewell, follow Sheffield Road and cross the five-arched bridge of the River Wye, turn right and ascend Station Road to the former Bakewell railway station and car park on your left." The trail passes through Blackwell Mill , Millers Dale , Cressbrook , Monsal Dale , Great Longstone , Hassop and Bakewell. At Longstone and Hassop
3078-449: The area have been found in several caves. Various rock-types beneath the soil strongly influence the landscape; they determine the type of vegetation and ultimately the type of animal inhabiting the area. Limestone has fissures and is soluble in water, so that rivers could carve deep, narrow valleys. These often find routes underground, creating cave systems. Millstone grit is insoluble but porous , absorbing water that seeps through
3159-405: The area. It was not iced over in the last glacial period , which peaked about 20,000–22,000 years ago. A mix of Irish Sea and Lake District ice abutted its western margins. Glacial meltwaters eroded a complex of sinuous channels along this margin of the district. Glacial meltwaters contributed to the formation and development of many caves in the limestone area. Remains of wild animal herds roaming
3240-399: The coal and dewatered the mines. Coal from the east was used in lead smelting and from the west for lime burning. Lead mining peaked in the 17th and 18th centuries; high concentrations were found in the area from this period, along with peat on Kinder Scout, suggesting that lead smelting occurred. Lead mining declined from the mid-19th century, with the last major mine closing in 1939. Lead
3321-748: The collection, storage and supply of water for the use of the towns in the plains below that I am surprised that they have been overlooked. The western Peak District is drained by the Etherow, the Goyt and the Tame , all tributaries of the River Mersey . The north-east is drained by tributaries of the River Don . Of the tributaries of the River Trent draining south and east, the River Derwent
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3402-518: The colony covers about 3 square metres (32 sq ft) of a rock face with small subsidiary colonies nearby. Jacob's-ladder ( Polemonium caeruleum ), a rarish species characteristic of limestone dales in the White Peak, has been Derbyshire's county flower since 2002. It grows on grassland, light woodland, screes and rock ledges, and by streams in Lathkill , Wolfscote, Taddington, Wye Dale and other dales. Pollen evidence from peat bogs shows it
3483-468: The cruel treatment. Hassop railway station was situated about two miles from the village. It was opened in 1862 by the Midland Railway on its extension of the Manchester, Buxton, Matlock and Midlands Junction Railway from Rowsley. The trail passes through the following tunnels: A further tunnel, Haddon Tunnel , is currently closed on safety grounds but has been proposed for reopening. The route
3564-679: The dales of the Wye Valley , along a route roughly followed by the A6 road . It enters the Peak District , flows just south of Tideswell , then through Ashford in the Water and Bakewell , and south of Haddon Hall , before meeting the River Derwent at Rowsley . The main tributary of the river is the River Lathkill , which enters approximately one mile from its mouth. The River Wye is one of Derbyshire's best-known rivers and
3645-512: The district, and the White Peak covers central and southern areas. The highest point is Kinder Scout (2,087 ft (636 m)). Most of the area is within the Peak District National Park , a protected landscape designated in 1951. A 2021 report states that "the Park’s own population numbers around 40,000 and supports an estimated 18,000 jobs, predominantly through farming, manufacturing and, inevitably, tourism". The area has been inhabited since
3726-549: The district. The eastern moors are a stronghold for adders . Native fish in the Peak District include Atlantic salmon , brown trout , European eel , bullhead , brook lamprey and grayling . A possibly unique population of "wild" rainbow trout survives on the Derbyshire Wye , following their introduction at the turn of the 20th century. Butterflies in the region include the dingy skipper , brown argus , small blue and white-letter hairstreak . Moths include
3807-689: The east are at the western edge of the South Yorkshire Coalfield . Those in the west are part of the Cheshire section of the Lancashire Coalfield . Mining started in medieval times , was at its most productive in the 18th and early 19th centuries, and continued into the early 20th century. The earliest mining took place around outcrops , where miners followed the seams deeper into the hillsides. At Goyt's Moss and Axe Edge , deep seams were worked and steam engines raised
3888-525: The eastern and western margins, carboniferous limestone at the core and rocks of millstone grit between them. The southern edge of the Derbyshire dome is overlain by sandstones of Triassic age, though they barely impinge on the National Park. The White Peak forms a central and southern section with carboniferous limestone found at or near the surface. The Dark Peak to the north, east and west
3969-605: The end of this period, the Earth's crust sank here which led to the area being covered by sea, depositing a variety of new rocks. Some time after its deposition, mineral veins were formed in the limestone. The veins and rakes have been mined for lead since Roman times . The Peak District was iced over in at least one of the ice ages of the last two million years, probably the Anglian glaciation of some 450,000 years ago, as shown by patches of glacial till or boulder clay found across
4050-509: The fifth largest national park in England and Wales. In the UK, designation as a national park means that planning and other functions are provided by a national park authority, with additional restrictions that enhance protection from inappropriate development. Land within this national park as in others is in a mix of public and private ownership. The National Trust , a charity that conserves historic and natural landscapes, owns about 12 per cent of
4131-417: The grits, until it meets the less porous shales beneath, creating springs where it reaches the surface. The shales are friable and easily attacked by frost, forming areas vulnerable to landslides, as on Mam Tor. The gritstone and shale of the Dark Peak supports heather moorland and blanket bog , with rough sheep pasture and grouse shooting as the main land uses, though parts are also farmed, especially
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#17327936529314212-598: The heather moorlands of the Dark Peak, where the red grouse population is maintained by gamekeepers employed by shooting estates. A population of black grouse became extinct in 2000, but reintroduction was attempted in 2003. Quarries and rock outcrops provide nest sites for peregrine falcon and common raven . Ravens and common buzzards are increasingly found as their British range expands eastwards, perhaps because of general reductions in persecution. Illegal persecution has limited populations of rare raptors such as Eurasian goshawk , peregrine and hen harrier . Following
4293-535: The high moors. After decades of decline due to pollution, Sphagnum mosses are returning, with species such as S. cuspidatum particularly dominant. Most Peak District mammals are generalists and widespread across the UK, but the mountain hares on heather moorland in the Dark Peak form the only wild population in England. They were reintroduced in the Victorian era for sporting purposes. A feral population of red-necked wallabies lived around The Roaches from
4374-435: The issue. Fast-flowing rivers attract specialists such as grey wagtail , dipper , common sandpiper , mandarin duck and goosander . Wooded and semi-wooded areas attract redstart , pied flycatcher , wood warbler and tree pipit , and coniferous plantations house siskin and common crossbill . Upland reservoirs in the Dark Peak are generally oligotrophic and attract few birds, but lower-lying reservoirs on
4455-458: The land in the national park. Its three estates ( High Peak , White Peak and Longshaw ) include ecologically or geologically significant areas at Bleaklow , Derwent Edge , Hope Woodlands , Kinder Scout , the Manifold valley, Mam Tor , Dovedale , Milldale and Winnats Pass . The park authority owns around 5 per cent; other major landowners include several water companies. Bakewell
4536-400: The local authorities covered by the park. The local authorities and the number of members they appoint are as follows: The Peak has been inhabited from the earliest periods of human activity, as shown by finds of Mesolithic flint artefacts and palaeo-environmental evidence from caves in Dovedale and elsewhere. Signs of Neolithic activity include monumental earthworks or barrows such as
4617-409: The moorland plateaux of the Dark Peak and the high ridges of the White Peak. Many rivers in the Dark Peak and outer fringes were dammed to create reservoirs for supplying drinking water. Streams were dammed to provide headwater for water driven mills ; weirs were built for the same purpose. The reservoirs of the Longdendale Chain were completed in February 1877 to provide compensation water, ensuring
4698-453: The moorlands are a net carbon sink or source, based on the fact that Britain's upland areas contain a major global carbon store in the form of peat . Human interaction in terms of direct erosion and fire, with the effects of global warming, are the main variables they considered. The Peak District is formed almost wholly of sedimentary rocks of the Carboniferous period. They make up the carboniferous limestone overlying gritstone , and
4779-407: The national park is privately owned, with the largest single owner being the National Trust (12%). The national park is governed by the Peak District National Park Authority, which was established under the 1995 Environment Act, replacing the Peak Park Planning Board. The authority has 30 members, 14 appointed by the Secretary of State for Environment, Food, and Rural Affairs and 16 appointed by
4860-443: The northern and eastern parts of the Dark Peak and the White Peak NCA most of the White Peak. The western margins of the Dark Peak are in the South West Peak NCA, where farmland and pastured valleys are found with gritstone edges and moorland. Outside the park, the wider Peak District often includes the area approximately between Disley and Sterndale Moor, encompassing Buxton and the Peak Dale corridor. It may also include some of
4941-415: The one at Margery Hill . The Bronze Age saw the area well populated and farmed. Evidence remains in henges such as Arbor Low near Youlgreave and the Nine Ladies stone circle at Stanton Moor . In the same period and into the Iron Age , hill forts such as Mam Tor's were created. The Romans drew on the area's rich mineral veins, exporting lead from the Buxton area along well-used routes. Buxton
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#17327936529315022-488: The outer fringes and foothills, such as the Churnet and lower Derwent Valleys. The region is mostly surrounded by lowlands with gritstone moorlands of the South Pennines to the north, separated approximately by the Tame Valley , Standedge and Holme Valley . The national park covers 555 square miles (1,440 km ), including most of the region in Derbyshire and extends into Staffordshire, Cheshire, Greater Manchester and South and West Yorkshire. Its northern limit
5103-591: The pine marten is unclear, though confirmed sightings have occurred in recent decades in Derbyshire and north Staffordshire and a specimen from an introduced Welsh population was found dead outside the national park on a road between Ripley and Belper in 2018. As with mammals, many Peak bird species are widespread generalists. The Dark Peak moors still support breeding populations of several upland specialists, such as twite , short-eared owl , golden plover , dunlin , ring ouzel , northern wheatear and merlin . The populations of twite and golden plover are
5184-555: The railway station design, with leaded glass windows, reflected the architecture of the hall. For many years the trail could not follow the trackbed through the tunnels at Monsal Head and Cressbrook which were closed for safety reasons and the trail was diverted to avoid them. The tunnels were walked by Julia Bradbury in BBC TV's Railway Walks: The Peak Express . Many access points and diversion paths were unsuitable for cyclists, wheelchairs or people with walking difficulties because of steep uneven stone steps or narrow paths. Plans to make
5265-468: The railway stations were some distance from the villages. Derbyshire County Council support the creation of a circular cycle route linking Buxton, Bakewell and Matlock with the High Peak Trail . Dubbed the White Peak Loop , it includes extending the Monsal Trail to Matlock, a proposal which received strong support from a public consultation exercise in 2014. The 5-mile (8.0 km) section between Rowsley and Matlock opened in March 2018, running adjacent to
5346-454: The railway trackbed except for minor diversions just north of Rowsley South, at Darley Dale, and at Matlock. The remaining 2.5-mile (4.0 km) section of the route between Bakewell (Coombs Viaduct) and Rowsley is at the design stage. When complete, the section will run for the most part along the railway trackbed and require new bridges at Rowsley and the refurbishment and opening up of the 1-km Haddon Tunnel. Headstone Viaduct, at Monsal Head,
5427-457: The same winter, the A635 (Saddleworth Moor) and A57 (Snake Pass) were closed due to snow for almost a month. Frost cover is seen for 20–30 per cent of the winter on moorland in the Dark Peak and 10 per cent in the White Peak. The Moorland Indicators of Climate Change Initiative was set up in 2008 to collect data in the area. Students investigated the interaction between people and the moorlands and their effect on climate change, to discover whether
5508-422: The section within the National Park), and is one of the major tributaries of the River Derwent , which flows into the River Trent , and ultimately into the Humber and the North Sea . The river rises just west of Buxton , on Axe Edge Moor . Part of the flow passes underground through Poole's Cavern before rising at Wye Head , and flowing through the Pavilion Gardens in Buxton. It then flows east through
5589-413: The south-west, whose sources are on Axe Edge Moor , flow into the Trent. The River Dane flows into the River Weaver in Cheshire. There are no canals in the national park, although the Standedge Tunnels on the Huddersfield Narrow Canal run underneath the extreme north of it. Outside the park, waters from the Dark Peak feed the Macclesfield , Ashton , and Huddersfield Narrow Canals and waters from
5670-452: The southern fringes such as Carsington Water and Ogston Reservoir regularly attract rare migrants and wintering rarities such as various waders, wildfowl, gulls and terns. The area is regularly overflown by wintering populations of pink-footed geese moving between East Anglia and Morecambe Bay. Dipper, golden plover, hen harrier, merlin and short-eared owl are local biodiversity action plan priority species. Fossil records show that
5751-503: The southernmost confirmed breeding populations in England, and the Peak District Moors Special Protection Area (SPA) is a European designation for its populations of merlin, golden plover and short-eared owl. The Peak District lacks the concentrations of breeding waders found further north in the Pennines, though the moors and their fringes accommodate breeding curlew and lapwing , and less noticeable wading birds such as dunlin and snipe . Commercial driven grouse shooting occurs on
5832-495: The spoil heaps of ancient mining activity, form another distinctive White Peak habitat, supporting a range of rare metallophyte plants, including spring sandwort ( Minuartia verna ; also known as leadwort), alpine pennycress ( Thlaspi caerulescens ) and mountain pansy ( Viola lutea ). Two endemic vascular plants are found nowhere else in the world: Derby hawkweed ( Hieracium naviense ), found only in Winnats Pass ,
5913-489: The tunnels safe and re-open them to the public were given the go-ahead at a cost of £3.785 million. The tunnels were formally opened on 25 May 2011 at a ceremony at the Headstone Viaduct after being used from 13 May 2011. The trail can be used by wheelchair users with level access at Bakewell, Hassop railway station (disabled toilets at Bakewell and Millers Dale railway stations) and Millers Dale. Reopening as
5994-469: The valley of the River Wye . The trail passes through Blackwell Mill , Chee Dale , Millers Dale , Cressbrook , Monsal Dale , Great Longstone , Hassop and Bakewell . The trail has numerous landmarks including Headstone Viaduct, Cressbrook Mill, Litton Mill and Hassop railway station , and passes through six tunnels. It is a major part of the as yet incomplete White Peak Loop and is designated as National Cycle Route 680 . The Monsall Trail follows
6075-579: Was a Roman settlement known as " Aquae Arnemetiae " for its spring. Theories on how the name Peak derived cite the Pecsaetan or peaklanders, an Anglo-Saxon tribe inhabiting the central and northern parts of the area from the 6th century CE, when it belonged to the Anglian kingdom of Mercia . Barrows from the Anglo-Saxon period are present, including Benty Grange , where the eponymous helmet
6156-490: Was built to a grander design than normal and carried his coat of arms. The Duke of Devonshire later realised the value of the railway, and his offer for the Midland Railway to run through Chatsworth came too late. He was the force behind the construction of Hassop railway station , which, although nearer to Bakewell than Hassop village, meant he did not have to share a railway station with his neighbour. Great Longstone station (Longstone before 1913) served Thornbridge Hall , and
6237-403: Was built to transport limestone from quarries at Cauldon Low for the iron industry and flints for the pottery industry. Most of the area is over 1,000 feet (300 m) above sea level, in the centre of the country at a latitude of 53°N, bringing relatively high annual rainfall averaging 40.35 inches (1,025 mm) in 1999. The Dark Peak tends to receive more rainfall than the White Peak, as it
6318-695: Was built up by the Dukes of Devonshire as a genteel health resort in the 18th century while the spa at Matlock Bath , in the River Derwent valley, was popularised in Victorian times. Hayfield is at the foot of Kinder Scout, the area's highest summit. Other towns and villages fringing the park include Whaley Bridge , Hadfield , Tintwistle , Darley Dale and Wirksworth in Derbyshire, Stocksbridge in South Yorkshire and Marsden and Holmfirth in West Yorkshire. Several rivers have sources on
6399-400: Was found. In medieval and early modern times, the area was mainly agricultural, with sheep farming, rather than arable the main activity in upland holdings. From the 16th century, the mineral and geological wealth became increasingly significant. Not only lead, but coal, fluorite , copper from Ecton Mines , zinc , iron , manganese and silver have been mined. Celia Fiennes , describing
6480-489: Was necessitated by the Duke of Devonshire 's objection to the railway passing through his land (which included not only Chatsworth House , but extensive grounds north of Rowsley ). The route meant that the line had to pass above the town of Bakewell, rather than through it. The Duke of Rutland , of Haddon Hall , insisted on the construction of Haddon Tunnel to hide it from his view, but he used Bakewell railway station , which
6561-557: Was widespread throughout Britain just after the last ice age. Much planted in gardens from where it has established itself in other parts of the area, as a native it is restricted to the White Peak and the Yorkshire Dales . The Dark Peak heathlands, bogs, gritstone edges and acid grasslands contain relatively few species; heather ( Calluna vulgaris ), crowberry ( Empetrum nigrum ), bilberry ( Vaccinium myrtillus ) and hare's-tail cotton grass ( Eriophorum vaginatum ) dominate
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