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.
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.
The improved roads and the Cromford Canal both shortly came under competition from new railways, with work on the first railway in the Peak commencing in 1825. Although the Cromford and High Peak Railway (from Cromford Canal to Whaley Bridge) was an industrial railway, passenger services soon followed, including the Woodhead Line (Sheffield to Manchester via Longdendale) and the Manchester, Buxton, Matlock and Midlands Junction Railway. Not everyone regarded the railways as an improvement. John Ruskin wrote of the Monsal Dale line: ‘You enterprised a railroad through the valley, you blasted its rocks away, heaped thousands of tons of shale into its lovely stream. The valley is gone, and the gods with it; and now, every fool in Buxton can be at Bakewell in half-an-hour, and every fool in Bakewell at Buxton.
By the second half of the 20th century, the pendulum had swung back towards road transport. The Cromford Canal was largely abandoned in 1944, and several of the rail lines passing through the Peak were closed as uneconomic in the 1960s as part of the Beeching Axe. The Woodhead Line was closed between Hadfield and Penistone; parts of the trackbed are now used for the Trans-Pennine Trail, the stretch between Hadfield and Woodhead being known specifically as the Longdendale Trail. The Manchester, Buxton, Matlock and Midlands Junction Railway is now closed between Rowsley and Buxton where the trackbed forms part of the Monsal Trail. The Cromford and High Peak Railway is now completely shut, with part of the trackbed open to the public as the High Peak Trail. Another disused rail line between Buxton and Ashbourne now forms the Tissington Trail.
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.
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 Derby, Nottingham and Manchester, and there are regular buses from the nearest towns such as Sheffield, Glossop, Stoke, Leek and Chesterfield. The nearest airports are Manchester, East Midlands and Doncaster-Sheffield.
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 Hope Valley and Buxton Line trains also serves many local stations (including Hathersage, Hope and Edale).
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 high point on Kinder Scout of 2,087 feet (636 m). Despite its name, the landscape lacks sharp peaks, being characterised by rounded hills and gritstone escarpments (the “edges”). The area is surrounded by major conurbations, including Huddersfield, Manchester, Sheffield, Derby and Stoke-on-Trent.
The National Park covers 555 square miles (1,440 km2) of Derbyshire, Staffordshire, Cheshire, Greater Manchester and South and West Yorkshire, including the majority of the area commonly referred to as the Peak. The Park boundaries were drawn to exclude large built-up areas and industrial sites from the park; in particular, the town of Buxton and the adjacent quarries are located at the end of the Peak Dale corridor, surrounded on three sides by the Park. The town of Bakewell and numerous villages are, however, included within the boundaries, as is much of the (non-industrial) west of Sheffield. As of 2006, it is the fourth largest National Park in England and Wales. As always in Britain, the designation “National Park” means that there are planning restrictions to protect the area from inappropriate development, and a Park Authority to look after it-but does not imply that the land is owned by the government, or is uninhabited.
High Peak panorama between Hayfield and Chinley
12% of the Peak District National Park is owned by the National Trust, a charity which aims to conserve historic and natural landscapes. It does not receive government funding. The three Trust estates (High Peak, South Peak and Longshaw) include the ecologically or geologically significant areas of Bleaklow, Derwent Edge, Hope Woodlands, Kinder Scout, Leek and Manifold, Mam Tor, Dovedale, Milldale and Winnats Pass. The Peak District National Park Authority directly owns around 5%, and other major landowners include several water companies.
The Broads is a network of mostly navigable rivers and lakes (known locally as broads) in the English counties of Norfolk and Suffolk. The Broads, and some surrounding land was constituted as a special area with a level of protection similar to a UK National Park by The Norfolk and Suffolk Broads Act of 1988. The Broads Authority, a Special Statutory Authority responsible for managing the area, became operational in 1989
The total area is 303 km² (188 sq.miles), most of which is in Norfolk, with over 200 km (125 miles) of navigable waterways. There are seven rivers and sixty three broads, mostly less than twelve feet deep. Thirteen broads are generally open to navigation, with a further three having navigable channels. Some broads have navigation restrictions imposed on them in autumn and winter.
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 England and Wales but as well as the Broads Authority having powers and duties almost identical to the national parks it is also the third largest inland navigation authority. Because of its navigation role the Broads Authority was established under its own legislation on 1 April 1989. More recently the Authority wanted to change the name of the area to The Broads National Park in recognition of the fact that the status of the area is equivalent to the rest of the national park family but was unable to get agreement from all the different parties. The Private Bill the Authority is promoting through Parliament is largely about improving public safety on the water and the Authority did not want to delay or jeopardise these provisions for the name issue, so the provision was dropped before the Bill was deposited in Parliament.
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 Broads landscape of today, with its reed beds, grazing marshes and wet woodland.
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 Broads as some specimens have been preserved and restored.
Ted Ellis, a local naturalist, referred to the Broads as “the breathing space for the cure of souls”.
A great variety of boats can be found on the Broads, from Edwardian trading wherries to state-of-the-art electric or solar-powered boats.
The point at which the River Yare and the River Waveney merge into Breydon Water
Yachts on the Norfolk Broads
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 Lake Lothing are connected by Mutford Lock, the only lock on the broads and necessary because of the different tidal ranges and cycles in the two lakes.
In the lists below, names of broads are emboldened to help distinguish them from towns and villages.
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 Vancouver’s first roadways.
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 Canada’s first civic arboretum, with a generous donation from the Canadian Pulp and Paper Association. The popular quarry gardens were designed by Park Board Deputy Superintendent Bill Livingstone and were unveiled in the early 1960s.
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.
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.