Yorkshire Dales

Typical Dales barn, near Selside
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.
Janet's Foss, near Malham
Ingleborough as seen from the peat bog below

The Yorkshire Dales is an upland area of the Pennines in Northern England in the historic county of Yorkshire, most of it in the Yorkshire Dales National Park created in 1954.[1]

The Dales comprises river valleys and the hills, rising from the Vale of York westwards to the hilltops of the Pennine watershed. In Ribblesdale and Dentdale, the area extends westwards across the watershed, but most of the valleys drain eastwards to the Vale of York, into the Ouse and the Humber. The extensive limestone cave systems are a major area for caving in the UK.

Etymology

The word dale, like dell, is derived from the Old English word dæl. It has cognates in the Nordic/Germanic words for valley (dal, tal), and occurs in valley names across Yorkshire and Northern England. Usage here may have been reinforced by Nordic languages during the time of the Danelaw.

Most of the dales are named after their river or stream (e.g., Arkengarthdale, formed by Arkle Beck). The best-known exception 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. River valleys all over Yorkshire are called "(name of river)+dale"—but only the more northern valleys (and only the upper, rural, reaches) are included in the term "The Dales" .

Geography

The Yorkshire Dales spread to the north from the market and spa towns of Settle, Skipton, Ilkley and Harrogate in North Yorkshire, to the southern boundary in Wharfedale and Airedale. The lower reaches of these valleys are not usually included in the area, and Calderdale, much further south, is not part of the Dales even though it is a dale, is in Yorkshire, and its upper reaches are as scenic and rural as many further north. Most of the larger southern dales, Ribblesdale, Malhamdale and Airedale, Wharfedale and Nidderdale, run roughly parallel from north to south. The more northerly dales, Wensleydale and Swaledale run generally from west to east. There are 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. Many upland areas consist of heather moorland, used for grouse shooting from 12 August (the Glorious Twelfth).

Geology

Main article: Geology of Yorkshire

The dales are 'U' and 'V' shaped valleys enlarged and shaped by glaciers, mainly in the most recent Devensian ice age. The underlying rock is 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 formed from older Silurian and Ordovician rocks, which make up the Howgill Fells.

Tourism

The majority of visitors are sightseers, with 75% visiting to drive around and 65% walking around. 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

Gaping Gill

The underlying limestone in parts of the Dales has extensive cave systems making it a major area for caving in the UK. Some caves are open to the public for tours.[2]

The systems include:

See also

References

Wikimedia Commons has media related to Yorkshire Dales.
Wikivoyage has a travel guide for Yorkshire Dales.


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

This article is issued from Wikipedia - version of the 11/15/2016. The text is available under the Creative Commons Attribution/Share Alike but additional terms may apply for the media files.