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The Peak District is an upland area in England, at the southern end of the Pennines. Mostly in Derbyshire, it extends into Cheshire, Greater Manchester, Staffordshire, West Yorkshire and South Yorkshire. It is subdivided into the Dark Peak, moorland dominated by gritstone, and the White Peak, a limestone area with valleys and gorges. The Dark Peak forms an arc on the north, east and west of the district, and the White Peak covers central and southern areas. The highest point is Kinder Scout. Most of the area is within the Peak District National Park, a protected landscape designated in 1951.
South Yorkshire is a ceremonial county in the Yorkshire and the Humber region of England. It borders North Yorkshire and West Yorkshire to the north, the East Riding of Yorkshire to the north-east, Lincolnshire to the east, Nottinghamshire to the south-east, and Derbyshire to the south and west. The largest settlement is the city of Sheffield.
The Midlands is the central part of England, bordered by Wales, Northern England, Southern England and the North Sea. The Midlands correspond broadly to the early-medieval kingdom of Mercia, and later became important in the Industrial Revolution of the 18th and 19th centuries. They are now split into two official regions, the West Midlands and East Midlands. The Midlands' biggest city, Birmingham, is the second-largest in the United Kingdom. Other important cities include Coventry, Derby, Leicester, Lincoln, Nottingham, Stoke-on-Trent, Wolverhampton, and Worcester.
The Pennines, also known as the Pennine Chain or Pennine Hills, are a range of uplands mainly located in Northern England. Commonly described as the "backbone of England" because of its length and position, the range runs from Derbyshire and Staffordshire in the North Midlands to Northumberland in North East England, near the Anglo-Scottish border. The range starts near the valley of the River Trent to the south and extends northwards across the Peak District, South Pennines, Yorkshire Dales, and North Pennines, ending at the Tyne Gap. Beyond the gap are the Border Moors and Cheviot Hills, which are included in some definitions of the range.
The Dark Peak is the higher and wilder part of the Peak District in England, mostly forming the northern section but also extending south into its eastern and western margins. It is mainly in Derbyshire but parts are in Staffordshire, Cheshire, Greater Manchester, West Yorkshire and South Yorkshire.
England comprises most of the central and southern two-thirds of the island of Great Britain, in addition to a number of small islands of which the largest is the Isle of Wight. England is bordered to the north by Scotland and to the west by Wales. It is closer to continental Europe than any other part of mainland Britain, divided from France only by a 33 km (21 mi) sea gap, the English Channel. The 50 km (31 mi) Channel Tunnel, near Folkestone, directly links England to mainland Europe. The English/French border is halfway along the tunnel.
England is divided by a number of different regional schemes for various purposes. Since the creation of the Government Office Regions in 1994 and their adoption for statistical purposes in 1999, some historical regional schemes have become obsolete. However, many alternative regional designations also exist and continue to be widely used.
The mountains and hills of England comprise very different kinds of terrain, from a mountain range which reaches almost 1,000 metres high, to several smaller areas of lower mountains, foothills and sea cliffs. Most of the major upland areas have been designated as Areas of Outstanding Natural Beauty (AONB) or national parks. The highest and most extensive areas are in the north and west, while the midlands, south-east and east of the country tend to be low-lying.
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. To the east it is fringed by the towns of West Yorkshire whilst to the south it is bounded by the Peak District. The rural South Pennine Moors constitutes both a Site of Special Scientific Interest and Special Area of Conservation.
Longridge Fell is the most southerly fell in England, near the town of Longridge, Lancashire. It lies at the southern end of the Forest of Bowland Area of Outstanding Natural Beauty. As its name suggests, it takes the form of a long ridge which rises in a north-easterly direction from within the town of Longridge to its summit 4.5 miles distant. As the ridge curves towards the east, it comes to a sudden end and drops into the Hodder Valley. The fell is an example of a cuesta; the ridge has a sharp drop or escarpment on its northern side, and a gentler, more varying slope on its southern side. These features make it a popular takeoff for hang-gliders and paragliders on the relatively infrequent occurrences of a northerly wind.
In Yorkshire there is a very close relationship between the major topographical areas and the geological period in which they were formed. The Pennine chain of Hills in the west is of Carboniferous origin. The central vale is Permo-Triassic. The North York Moors in the north-east of the county are Jurassic in age while the Yorkshire Wolds to the south east are Cretaceous chalk uplands. The plain of Holderness and the Humberhead levels both owe their present form to the Quaternary ice ages.
The Geology of Yorkshire in northern England shows a very close relationship between the major topographical areas and the geological period in which their rocks were formed. The rocks of the Pennine chain of hills in the west are of Carboniferous origin whilst those of the central vale are Permo-Triassic. The North York Moors in the north-east of the county are Jurassic in age while the Yorkshire Wolds to the south east are Cretaceous chalk uplands. The plain of Holderness and the Humberhead levels both owe their present form to the Quaternary ice ages. The strata become gradually younger from west to east.
The Natural Areas of England are regions, officially designated by Natural England, each with a characteristic association of wildlife and natural features. More formally, they are defined as "biogeographic zones which reflect the geological foundation, the natural systems and processes and the wildlife in different parts of England...".
The Mid Severn Sandstone Plateau is a rural landscape and one of the natural regions of central England, straddling the border between the counties of Shropshire and Staffordshire. It stretches from the western fringes of the Birmingham conurbation to Telford in the north and Kidderminster in the south. The major feature of the plateau is the valley of the River Severn, which cuts through it from north to south. It consists of Permian and Triassic-age New Red Sandstone getting older as one goes west until one reaches Silurian and Carboniferous-age siltstones and coals west of the river.
References
- ↑ "National Character Areas – defining England's natural boundaries". Natural England. Retrieved 26 June 2013.