Yorkshire Dales

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Yorkshire Dales (The Dales)
Protected Area
YorkshireDalesSign.jpg
National park entrance sign, near Skipton
CountryUnited Kingdom
PartEngland
CountiesNorth Yorkshire, Cumbria
Highest point
 - locationWhernside
 - elevation736 m (2,415 ft)
Area1,769 km2 (683 sq mi)
National Park of England1954
IUCN categoryV - Protected Landscape/Seascape
Yorkshire Dales National Park within North Yorkshire
 
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Yorkshire Dales (The Dales)
Protected Area
YorkshireDalesSign.jpg
National park entrance sign, near Skipton
CountryUnited Kingdom
PartEngland
CountiesNorth Yorkshire, Cumbria
Highest point
 - locationWhernside
 - elevation736 m (2,415 ft)
Area1,769 km2 (683 sq mi)
National Park of England1954
IUCN categoryV - Protected Landscape/Seascape
Yorkshire Dales National Park within North Yorkshire

The Yorkshire Dales (also known simply as The Dales) is an upland area of Northern England dissected by numerous valleys.

The area lies within the county boundaries of historic Yorkshire, though it spans the ceremonial counties of North Yorkshire and Cumbria. Most of the area falls within the Yorkshire Dales National Park, created in 1954 and now one of the fifteen National parks of Britain, but the term also includes areas to the east of the National Park, notably Nidderdale.[1]

The Dales is a collection of river valleys and the hills among them, rising from the Vale of York westwards to the hilltops of the main Pennine watershed. In some places the area extends westwards across the watershed, but most of the valleys drain eastwards to the Vale of York, into the Ouse and then the Humber.

The word dale comes from the Nordic/Germanic word for valley (dal, tal), and occurs in valley names across Yorkshire and Northern England. but the name Yorkshire Dales is generally used to refer specifically to the dales west of the Vale of York and north of the West Yorkshire Urban Area.

Geography[edit]

Most of the dales in the Yorkshire Dales are named after their river or stream (e.g., Arkengarthdale, formed by Arkle Beck). The best-known exception to this rule is Wensleydale, which is named after the small village and former market town of Wensley, rather than the River Ure, although an older name for the dale is Yoredale. In fact, valleys all over Yorkshire are called "(name of river)+dale"—but only the more northern Yorkshire valleys (and only the upper, rural, reaches) are included in the term "The Dales"[citation needed]. For example, the southern boundary area lies in Wharfedale and Airedale. The lower reaches of these valleys are not usually included in the area, and Calderdale, much further south, would not normally be referred to as part of "The Dales" even though it is a dale, is in Yorkshire, and the upper reaches are as scenic and rural as many valleys further north.

Geographically, the classical Yorkshire Dales spread to the north from the market and spa towns of Settle, 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 such as Wensleydale and Swaledale run generally from west to east. There are also many other smaller or lesser known dales such as Arkengarthdale, Bishopdale, Clapdale, Coverdale, Kingsdale, Littondale, Langstrothdale, Raydale, Waldendale and the Washburn Valley whose tributary streams and rivers feed into the larger valleys, and Barbondale, Dentdale, Deepdale and Garsdale which feed west to the River Lune.

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. To the north and west of the Dent Fault, the hills are principally formed from 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').

Cliffs of Carboniferous Limestone are a common geological feature in the Yorkshire Dales, this panoramic image shows the western face of Thwaites Scars taken from Long Lane.

Tourism[edit]

The majority of visitors are sightseers, with 75% visiting to drive around and 65% walking around[citation needed]. This indicates that most are there to take in the beauty of the surroundings. 26% also partake in hiking nature trails and spotting wildlife. 45% visit an information centre and 35% visit a castle or other historic site. 94% of visitors travel in a private mode of transport, with 90% using a car. The remaining 6% travel using public transport.

Cave systems[edit]

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 UK. Some of these are open to the public for cave tours.[2]

The systems include:

Yorkshire Dales National Park[edit]

Stone houses in Hawes, a typical example of Dales architecture
Limestone hills and dry-stone walls in the west of the Yorkshire Dales. This part of the national park is popular with walkers due to the presence of the Yorkshire three peaks.

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. The whole park lies within the historic 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, Darlington to the north-east and Harrogate to the south-east.[6] A proposed westward extension of the park into Lancashire and Cumbria would encompass much of the area between the current park and the M6 motorway, coming close to the towns of Kirkby Lonsdale, Kirkby Stephen and Appleby-in-Westmorland.[7] This proposal to add 162 square miles to the park has now been agreed by all interested parties and merely awaits ministerial approval. For the first time the Yorkshire Dales and Lake District national parks will be contiguous.[8]

Over 20,000 residents live and work in the park, which attracts over eight million visitors every year.[9] 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 Walk and the latest national trail — the Pennine Bridleway.[10] Cycling is also popular and there are several cycleways.[11]

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 area.[12] The park has five visitor centres located in major destinations in the park.[13] These are at:

Other places and sights within the National Park include:

See also[edit]

Janet's Foss, near Malham
Ingleborough as seen from the peat bog below

References[edit]

External links[edit]


Coordinates: 54°16′N 2°05′W / 54.267°N 2.083°W / 54.267; -2.083