From Wikipedia, the free encyclopedia

The Pennines are a low-rising mountain range in England. Often said ^{[1] [2][3]} to be the "backbone of England", they form an unbroken range stretching from the Peak District in Derbyshire, through the Yorkshire Dales, parts of Greater Manchester, the West Pennine Moors of Lancashire and Cumbrian Fells to the Cheviot Hills on the Anglo-Scottish border.North of the Aire Gap the Pennines give out a western spur into Lancashire, the Forest of Bowland and south of the gap is a similar spur, the Rossendale Fells. ^[4] It is an important water catchment area with numerous reservoirs in the head streams of the major river valleys. The region is widely considered to be one of the most scenic areas of Britain. The North Pennines have been declared an Area of Outstanding Natural Beauty (AONB) as has Nidderdale, while portions of the Pennines are incorporated into the Peak District National Park, the Yorkshire Dales National Park and the Northumberland National Park.^[5] Britain's first long distance footpath, the Pennine Way, runs the full length of the Pennine chain. Their total length is about 250 miles (402 km).

Contents 1 Etymology 2 Toponomy 3 Geology and landscape 4 Drainage 4.1 Reservoirs 5 Altitude 6 Character Areas of the Pennines 7 Dales 8 Demography 9 Economy 10 Main Settlements 11 Transport 12 History 13 Early Inhabitants 14 Celtic and Roman times 15 Dark ages 16 Norse times to middle ages 17 Other history 18 Language 19 Folklore and Customs 20 See also 21 References 22 External Links

The earliest written reference to the name dates only from the 18th century. The name is arguably influenced by the name of the Apennine Mountains of Italy, whose acquaintance many English gentry made on the Grand Tour at the same period and whose name is attributed to the same Celtic linguistic root.

The names of towns and geographical features retain some evidence of the Celts who were here before, and after, the Romans: for example the town Penrith, the fell Pen-y-ghent, the river Eden, or the name Cumbria. More commonly the local names result from the later Anglo-Saxon and Norse settlements. And in both Yorkshire and Cumbria many Norse words not commonly used in standard English are part of everyday speech: for example, gill (narrow steep valley), beck (brook or stream), fell (hill), dale (valley). ^[6]

The Pennines form an anticline which extends in a north-south direction, consisting of Millstone Grit and the underlying Carboniferous Limestone. The limestone is exposed at the surface to the north of the range in the North Pennines AONB and to the South in the Derbyshire Peak District. In the Yorkshire Dales this limestone exposure has led to the formation of large underground cave systems and watercourses, known as "gills" and "pots" in the Yorkshire dialect. These potholes are more prevalent on the eastern side and are amongst the largest in England; notable examples are the chasms of Gaping Gill, which is over 350 ft (107 m) deep and Rowten Pot, which is 365 ft (111 m) deep. The presence of limestone has also led to some unusual geological formations in the region, such as the limestone pavements of the Yorkshire Pennines. Between the Northern and Southern areas of exposed limestone, between Skipton and the Peak, lies a narrow belt of gritstone country. Here the shales and sandstones of the Millstone Grit form high hills occupied by moors and peat-mosses with the higher ground being uncultivable and barely fit for pastures.

The landscape of the Pennines is generally upland areas of high moorland indented by the more fertile valleys of the region's various rivers.

The Pennines are a distinct physiographic province of the Central European Uplands division.

The Pennines constitute the main watershed in northern England, dividing the eastern and western parts of the country. The rivers Eden, Ribble, and Mersey all rise in the Pennines and flow westwards towards the Irish Sea. On the other side of the watershed, the rivers Tyne, Tees, Wear, Swale, Ure, Calder, Aire, Don, and Trent also rise in the region but flow eastwards to the North Sea.

Kielder Water

Ladybower Reservoir

The mountains are not very high and are often referred to as fells - or sometimes, rather inaccurately, as hills. The highest is Cross Fell in eastern Cumbria, at 2,930 feet (893 m) while other principal peaks include Mickle Fell 2,585 ft (788 m), Whernside 2,415 ft (736 m), Ingleborough 2,372 ft (723 m), High Seat 2,328 ft (710 m) and Wild Boar Fell 2,324 ft (708 m), both in Mallerstang, Pen-y-ghent 2,274 ft (693 m), and Kinder Scout 2,087 ft (636 m).

England has been divided into areas with similar landscape character. These have been called Joint Character Areas (JCAs). The JCAs are a widely recognised national spatial framework but the boundaries of the JCAs are not precise and many of the boundaries should be considered as broad zones of transition.^[7]

The Pennines have ten Joint Character Areas . These are

1 Border Moors and Forests^[8]

2 Tyne Gap and Hadrians Wall^[9]

3 North Pennines^[10]

4 Howgill Fells^[11]

5 Yorkshire Dales^[12]

6 Bowland Fells^[13]

The Bowland area of the Pennines is dominated by a central upland landform of deeply incised gritstone fells. There are vast tracts of heather covered peat moorland and blanket bog on these fells. The lower slopes of the fells are dotted with stone built farms and small villages and are criss crossed by drystone walls enclosing reclaimed moorland pasture. Cloughs, steep sided wooded valleys, link the upland and lowland landscapes. To the south-east of the area are extensive coniferous plantations and the eastern limestone areas support high quality species rich meadows. ^[14]

7 Southern Pennines^[15]

8 Dark Peak^[16]

9 White Peak^[17]

10 South West Peak^[18]

Airedale

Dovedale

Nidderdale

Ribblesdale

Teesdale

Swaledale

Weardale

Wensleydale

Wharfedale

It is a relatively sparsely populated region by English standards.

The main economic activities include sheep farming, quarrying and tourism.

Hawes

Keld

Muker

Reeth

Stanhope

Thwaite

The three main gaps in the Pennines have always afforded communications links between the areas to the east and west. These gaps are the Tyne Gap between Carlisle and Newcastle upon Tyne followed by the A69 road,the Stainmoor Gap and the Aire Gap linking Lancashire and Yorkshire via the valleys of the rivers Aire and Ribble. The Pennines are also traversed by the Leeds and Liverpool Canal and the M62 motorway. Elsewhere, the Pennines remain a formidable barrier to be crossed by tunnel or roads which may be blocked by snow for several days in winter.

The area contains many examples of Bronze Age settlements, and evidence of Neolithic settlement (including many stone circles or henges, such as Long Meg and Her Daughters.) ^[19]

The Pennines would of come under the tribal federation of the Brigantes. This tribal federation was made up of mainly small tribes who inhabited the Pennines and cooperated for defence and external affairs. The Brigantes later evolved into a early form of Kingdom. During Roman times the Brigantes eventually came under Roman domination. The Romans exploited the Pennines for the natural resources and wild animals found there.

The Pennines were a major obstical for Angl-Saxon expansion west. Even when they were conquered they still retained a distimct Semi-Celtic identity, which they still hold today. During the Dark Ages the Pennines came under many Celtic and Anglo-Saxon kingdoms. First it came under the NorthWest based kingdom of Rheged. There were later three kingdoms which were solely based in the pennines though. These were: The Kingdom of the Pennines and later the Kingdom of the Pennines broke up and was succeeded by Dunoting / Kingdom of the North Pennines and The Peak / Kingdom of the South Pennines.

During Norse times the Pennines were lightly settled by Viking Danes in the east and Norwegian Vikings in the west. The vikings left a lot of influence on placenames, even though they did not settle in great numbers. When Englang was unified the Pennines were incorporated into England.

The Pennines were the major route for the Jacobite attack on England. They also became highly exploited in the Victorian age.

The language used in pre-Roman and Roman times was British. During the dark ages the Cumbric language developed, however it is not yet certain weather or not it was a language or a strong dialect of old Welsh. During Anglo-Saxon times Celtic speech remained in most areas of the Pennines longer than it did in the surrounding areas of England. Eventually the Celtic tongue of the Pennines was replaced by English. In Norse times Viking settlers brought their languages of Danish (mainly in the Yorkshire Dales and parts of the Peak district ) and Norwegian (Mainly in the Western Pennines). With the consolidation of England, the Norwegian and Danish languages died out in England, though they survived in the Pennines longer than in most areas. Norman French had little affect on the language of the Pennines though. All of the above languages have had a influence, either large or small on the modern placenames of the Pennines. The modern language of the Pennines is English.

The folklore and customs are mostly based on Celtic and Viking customs and folklore. Many customs and stories have their origin in christianized pagan traditions.

• Pennine Way
• Yorkshire three peaks
• Geology of the United Kingdom
• UK topics

Arthur Raistrick, 'The Pennine Dales', Eyre Methuen Ltd 1968, ISBN 041326760

EBK Dark age Britain maps Number 1

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