This category has the following 152 subcategories, out of 152 total. The fusion of Norse and Old English was important in the formation of Middle English and hence Modern English, and many individual words of Norse descent remain in use in local dialects, such as that of Yorkshire, and in local place names.  The Pennines are fringed by extensive lowlands including the Eden Valley, West Lancashire Coastal Plain, Cheshire Plain, Vale of York, and the Midland Plains. The Howgill Fells and Orton Fells are sometimes considered to be part of the Pennines, both inside the Yorkshire Dales National Park. There are also significant challenges for managing tourism, farming and other developments within the National Park. The line was closed in 1981. The region is widely considered to be one of the most scenic areas of the United Kingdom. Celtic speech remained in most areas of the Pennines longer than it did in the surrounding areas of England. The related and declining black grouse is still found in northern parts of the Pennines. The Pennines (), also known as the Pennine Chain or Pennine Hills, is a range of hills and mountains separating North West England from Yorkshire Pennines (), also known as the Pennine Chain or Pennine Hills, is a range of hills and mountains separating North West England from Yorkshire The Pennine uplands contained Bronze Age settlements, and evidence remains of Neolithic settlement including many stone circles and henges, such as Long Meg and Her Daughters.. Erosion of the limestone has led to geological formations, such as the limestone pavements at Malham Cove. Sléibhte Pennine Thuaidh; Sléibhte Pennine Theas; Is síol faoi thíreolaíocht Shasana é an t-alt seo. The A66 road, its summit at 1,450 feet (440 m), follows the course of a Roman road from Scotch Corner to Penrith through the Stainmore Gap between the Eden Valley in Cumbria and Teesdale in County Durham. Subcategories. Our Geology. The South Pennines is a region of moorland and hill country in northern England lying towards the southern end of the Pennines.In the west it includes the Rossendale Valley and the West Pennine Moors.It is bounded by the Greater Manchester conurbation in the west and the Bowland Fells and Yorkshire Dales to the north. The Pennines are a mountain range in England.Often said to be the "backbone of England", they form an unbroken range stretching from the Peak District in the Midlands, through the Yorkshire Dales, parts of Greater Manchester, the West Pennine Moors of Lancashire and Cumbrian Fells to the Cheviot Hills on the Scottish border.Their total length is about 250 mi (402 km). It is believed that the north Pennines were under the control of the kingdom of Rheged. Penniner - Pennines. The name of the Pennines, the Backbone of Britain, is taken from that of the Apennines, the Backbone of Italy.  In fact, Redmonds found repeated comparisons with the Italian Apennines going back at least as early as William Camden (1551–1623), many of whose placenames and ideas Bertram incorporated into his work. The route passes through the counties of Derbyshire, West Yorkshire, Lancashire, North Yorkshire, Cumbria and Northumberland.It is part of the National Cycle Network (NCN). English Wikipedia has an article on: Pennines. Zone 8 is common throughout most of the UK, and zone 7 is the UK's coldest hardiness zone. The northern Pennine range is bordered by the foothills of the Lake District, and uplands of the Howgill Fells, Orton Fells and Cheviot Hills. The Aire Gap links Lancashire and Yorkshire via the valleys of the Aire and Ribble. The Peak District consists of hills, plateaus and valleys, divided into the Dark Peak with moorlands and gritstone edges, and the White Peak with limestone gorges. Wikipedia is a free online encyclopedia, created and edited by volunteers around the world and hosted by the Wikimedia Foundation.  The South Pennines is an area of hills and moorlands with narrow valleys between the Peak District and Yorkshire Dales. Here tree suppression combined with the heavier rainfall results in blanket bog up to 7 ft (2 m) thick. Dywedir yn aml eu bod yn ffurfio "asgwrn cefn Lloegr", gan ffurfio cadwyn ddidor o fryniau sy'n ymestyn o Ardal y Copaon yn Swydd Derby, trwy'r Dyffrynnoedd Swydd Efrog, rhannau o Fanceinion Fwyaf, Rhosdiroedd Gorllewin Pennine yn Swydd Gaerhirfryn a bryniau Cumbria i Fryniau Cheviot ar y ffin rhwng Lloegr a'r Alban. Higher elevations have a tundra climate. Water has carved out gorges, caves and limestone landscapes in the Yorkshire Dales and Peak District. They include some of the largest caves in England at Gaping Gill, more than 350 ft (107 m) deep and Rowten Pot, 365 ft (111 m) deep. 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