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 Pennine Way is a National Trail in England, with a small section in Scotland. The trail stretches for 268 miles (431 km) from Edale, in the northern Derbyshire Peak District, north through the Yorkshire Dales and Northumberland National Park and ends at Kirk Yetholm, just inside the Scottish border. The path runs along the Pennine hills, sometimes described as the "backbone of England". Although not the United Kingdom's longest National Trail, it is according to The Ramblers, "one of Britain's best known and toughest".
The White Peak, also known as the Low Peak, is a limestone plateau that forms the central and southern part of the Peak District in England. It is mostly between 270 metres (900 ft) and 430 metres (1,400 ft) above sea-level and is enclosed by the higher altitude Dark Peak to the west, north and east.
The High Peak Trail is a 17-mile (27 km) trail for walkers, cyclists and horse riders in the Peak District of England. Running from Dowlow (53.2059°N 1.8349°W), near Buxton, to High Peak Junction, Cromford (53.1004°N 1.5354°W), it follows the trackbed of the former Cromford and High Peak Railway, which was completed in 1831 to carry minerals and goods between the Cromford Canal wharf at High Peak Junction and the Peak Forest Canal at Whaley Bridge.
The Tissington Trail is a bridleway, footpath and cycleway in Derbyshire, England, along part of the trackbed of the former railway line connecting Ashbourne to Buxton. It takes its name from the village of Tissington, which it skirts. Opened in 1971, and now a part of the National Cycle Network, it stretches for 13 miles (21 km) from Parsley Hay (53.1706°N 1.7828°W) in the north to Ashbourne (53.0196°N 1.7397°W) in the south.
Peak Forest is a small village and civil parish on the main road the (A623) from Chapel-en-le-Frith to Chesterfield in Derbyshire. The population of the civil parish at the 2011 census was 335.
The Pennine Bridleway is a National Trail in Northern England.
The Limestone Way is a waymarked long-distance footpath in Derbyshire, England. It runs for 46 miles (74 km) through the White Peak of the Peak District National Park, from Castleton south to Rocester over the county boundary into Staffordshire. The trail is named for the limestone scenery along its route. It was devised by Brian Spencer of Matlock Rotary Club and developed and opened in 1986 by the West Derbyshire District Council. It originally ran to Matlock, but was extended to its current, longer route in 1992 to join up with the Staffordshire Way.
The Sabrina Way is a waymarked long-distance footpath and bridleway in England.
The Peak District Boundary Walk is a circular 190-mile (310 km) walking trail, starting and finishing at Buxton and broadly following the boundary of the Peak District, Britain's first national park. The route was developed by the Friends of the Peak District and was launched on 17 June 2017.
Chee Dale is a steep-sided gorge on the River Wye near Buxton, Derbyshire, in the Peak District of England.
Deep Dale is a short steep-sided gorge near Buxton, Derbyshire, in the Peak District of England. It is distinct from another Deep Dale, near Sheldon, 4 miles (6.4 km) to the east.
Monk's Dale is a short steep-sided dry gorge near Buxton, Derbyshire, in the Peak District of England. The dale is cut into a plateau of farmland and lies to the east of the village of Wormhill. The head of the valley leads into Peter Dale to the north. Miller's Dale is at the foot of the valley to the south.
Cressbrook Dale is a dry carboniferous limestone gorge near Bakewell, Derbyshire, in the Peak District of England. The dale is cut into a plateau of farmland and lies to the south east of the village of Litton. Cressbrook village is at the foot of the valley to the south.
Peter Dale is a short dry crag-sided valley near Buxton, Derbyshire, in the Peak District of England. There is a farmland plateau on either side. The northern end of the valley leads into Hay Dale at Dale Head and the foot of the valley leads into Monk's Dale. Hay Dale and Monk's Dale are both part of the Derbyshire Dales National Nature Reserve managed by Natural England. The Carboniferous limestone rocks of all these dales were formed 350 million years ago from the shells and sediments of a tropical sea. The landscape was then sculpted by the ice sheets from the last Ice Age 20,000 years ago.
Tideswell Dale is a short dry limestone valley near Tideswell village, Derbyshire, in the Peak District of England. There is a farmland plateau on either side. The foot of the valley leads into Miller's Dale on the River Wye, which the valley's Brook Head stream runs into.
Middleton Dale is a steep-sided, carboniferous limestone valley in the Derbyshire Peak District of England. The village of Stoney Middleton lies at the eastern foot of the dale and the village of Eyam lies about 600 metres (660 yd) to the north, through the side valley of Eyam Dale. The dale is cut into the surrounding gritstone uplands of Middleton Moor and Eyam Moor. Dale Brook stream runs down the dale into Stoke Brook and on into the River Derwent 1.5 kilometres (1 mi) beyond Stoney Middleton. The Delf is a secluded, wooded side gorge with a stream between Eyam and Middleton Dale. Opposite The Delf, water gushes from Hawkenedge Well and flows into Dale Brook.
The Wye Valley is the limestone valley of the River Wye in the White Peak of Derbyshire, England. The source of the River Wye is west of Buxton on Axe Edge Moor. One main channel runs underground through Poole's Cavern. The river flows though Buxton Pavilion Gardens and then along a culvert under the town centre. After leaving the flat area of central Buxton, the Wye Valley becomes distinct as a gorge running east for 10 miles (16 km) before the valley broadens at Ashford-in-the Water.
Long Dale is a carboniferous limestone valley near the village of Elton, Derbyshire, in the Peak District of England. The dale is cut into the plateau of Gratton Moor and Smerrill Moor and lies to the north of the hamlet of Pikehall, which is the venue of the annual Y Not Festival. Midway down the valley it turns sharply left and is known as Gratton Dale. Most of the valley is dry but Rowlow Brook flows down the lower part of Gratton Dale towards Dale End and onwards to become the River Bradford at Youlgreave.
Taddington Moor is a limestone hill between the villages of Taddington, Flagg and Chelmorton in the Derbyshire Peak District. The moor is an upland farming landscape. The summit at Sough Top is 438 metres (1,437 ft) above sea level.
