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 and includes 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 sides; the White Peak covers central and southern tracts. The Peak District was the first of the national parks of England and Wales in 1951. The historic Peak District extends beyond the National Park, which excludes major towns, quarries and industrial areas. Nearby Manchester, Stoke-on-Trent, Derby and Sheffield send millions of visitors. Inhabited from the Mesolithic era, it shows evidence of the Neolithic, Bronze and Iron Ages. Settled by the Romans and Anglo-Saxons, it remained largely agricultural; mining arose in the Middle Ages. Richard Arkwright built cotton mills in the Industrial Revolution. As mining declined, quarrying grew. Tourism came with the railways, spurred by the landscape, spa towns and Castleton's show caves.
West Yorkshire is a ceremonial county in the Yorkshire and the Humber region of England. It borders North Yorkshire to the north and east, South Yorkshire and Derbyshire to the south, Greater Manchester to the south-west, and Lancashire to the west. The city of Leeds is the largest settlement.
Airedale is a geographic area in Yorkshire, England, corresponding to the river valley or dale of the River Aire.
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 the north Midlands to North East England, near the Anglo-Scottish border. The Peak District is the southern end of the range, rising northwards from its foothills near the Trent Valley in northern Staffordshire, and further north into eastern Cheshire and southern Derbyshire. Beyond this are the 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 Forest of Bowland, also known as the Bowland Fells and formerly the Chase of Bowland, is an area of gritstone fells, deep valleys and peat moorland, mostly in north-east Lancashire, England, with a small part in North Yorkshire. It is a western outlier of the Pennines.
Moorland or moor is a type of habitat found in upland areas in temperate grasslands, savannas, and shrublands and montane grasslands and shrublands biomes, characterised by low-growing vegetation on acidic soils. Moorland, nowadays, generally means uncultivated hill land, but also includes low-lying wetlands. It is closely related to heath, although experts disagree on what precisely distinguishes these types of vegetation. Generally, moor refers to highland and high rainfall zones, whereas heath refers to lowland zones which are more likely to be the result of human activity. Moorland habitats mostly occur in tropical Africa, northern and western Europe, and neotropical South America. Most of the world's moorlands are diverse ecosystems. In the extensive moorlands of the tropics, biodiversity can be extremely high. Moorland also bears a relationship to tundra, appearing as the tundra and the natural tree zone. The boundary between tundra and moorland constantly shifts with climatic change.
Greenfield is a village in the civil parish of Saddleworth in the Metropolitan Borough of Oldham, in Greater Manchester, England. It is 4 miles (6.4 km) east of Oldham, and 13 miles (21 km) northeast of Manchester. It lies in a broad rural area at the southern edge of the South Pennines. To the east of the village Dovestone Reservoir, Chew Reservoir and Greenfield Reservoir lie in the Peak District National Park.
The Rossendale Valley is in the Rossendale area of Lancashire, England, between the West Pennine Moors and the main range of the Pennines. The area includes the steep-sided valleys of the River Irwell and its tributaries, which flow southwards into Greater Manchester. The rivers cut through the moorland of the Rossendale Hills, generally characterized by open unwooded land, despite the ancient designation of "forest".
Mickle Fell is a mountain in the Pennines, the range of hills and moors running down the middle of Northern England. It has a maximum elevation of 788 m (2,585 ft). It lies slightly off the main watershed of the Pennines, about 10 miles south of Cross Fell. After Cross Fell, Mickle Fell is the highest Marilyn within the North Pennines designated Area of Outstanding Natural Beauty (AONB).
The Pennine Bridleway is a National Trail in Northern England.
The West Pennine Moors is an area of the Pennines covering approximately 90 square miles (230 km2) of moorland and reservoirs in Lancashire and Greater Manchester, England. It is a Site of Special Scientific Interest.
Millstone Grit is the name given to any of a number of coarse-grained sandstones of Carboniferous age which occur in the British Isles. The name derives from its use in earlier times as a source of millstones for use principally in watermills. Geologists refer to the whole suite of rocks that encompass the individual limestone beds and the intervening mudstones as the Millstone Grit Group. The term Millstone Grit Series was formerly used to refer to the rocks now included within the Millstone Grit Group together with the underlying Edale Shale Group.
Standedge is a moorland escarpment in the Pennine Hills of northern England between Marsden, West Yorkshire and Diggle, Greater Manchester. Standedge has been a major moorland crossing point since Roman times and possibly earlier.
The South Pennine Moors are areas of moorland in the South Pennines in northern England. The designation is applied to two different but overlapping areas, a Site of Special Scientific Interest (SSSI) covering a number of areas in West Yorkshire, North Yorkshire, Lancashire and Greater Manchester, and a much larger Special Area of Conservation (SAC) covering parts of Derbyshire, South Yorkshire and West Yorkshire, and small areas of Cheshire, Staffordshire, Greater Manchester, Lancashire and North Yorkshire.
Boulsworth Hill is a large expanse of moorland, the highest point of the South Pennines of south-eastern Lancashire, England, separating the Borough of Pendle from Calderdale.
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.
Aire Gap is a pass through the Pennines in England formed by geologic faults and carved out by glaciers. The term is used to describe a geological division, a travel route, or a location that is an entry into the Aire river valley.
A National Character Area (NCA) is a natural subdivision of England based on a combination of landscape, biodiversity, geodiversity and economic activity. There are 159 National Character Areas and they follow natural, rather than administrative, boundaries. They are defined by Natural England, the UK government's advisors on the natural environment.
The geology of Lancashire in northwest England consists in the main of Carboniferous age rocks but with Triassic sandstones and mudstones at or near the surface of the lowlands bordering the Irish Sea though these are largely obscured by Quaternary deposits.
