Poole's Cavern or Poole's Hole is a two-million-year-old natural limestone cave on the edge of Buxton in the Peak District, in the county of Derbyshire, England.
Poole's Cavern forms part of the Wye system, and has been designated a Site of Special Scientific Interest.
The River Wye is a limestone river in the Peak District of Derbyshire, England. It is 23.9 miles (38.5 km) long, although it is widely quoted as being 15 miles (24 km) long, which refers to the section within the National Park. It is one of the major tributaries of the River Derwent, which flows into the River Trent, and ultimately into the Humber and the North Sea.
The river rises just west of Buxton, on Axe Edge Moor, and the flow is augmented by water which passes underground through Poole's Cavern before rising at Wye Head. The two sources join as they cross the Pavilion Gardens in Buxton. The river then flows east through the dales of the Wye Valley, along a route roughly followed by the A6 road. It enters the Peak District, flows just south of Tideswell, then through Ashford in the Water and Bakewell, passing to the south of Haddon Hall, before meeting the River Derwent at Rowsley. The main tributary of the river is the River Lathkill, which enters approximately one mile from its mouth.
Buxton is a spa town in the Borough of High Peak, Derbyshire, in the East Midlands region of England. It is England's highest market town, sited at some 1,000 feet (300 m) above sea level. It lies close to Cheshire to the west and Staffordshire to the south, on the edge of the Peak District National Park. In 1974, the municipal borough merged with other nearby boroughs, including Glossop, to form the local government district and borough of High Peak.
The town population was 22,115 at the 2011 Census. Sights include Poole's Cavern, a limestone cavern; St Ann's Well, fed by a geothermal spring bottled by Buxton Mineral Water Company; and many historic buildings, including John Carr's restored Buxton Crescent, Henry Currey's Buxton Baths and Frank Matcham's Buxton Opera House. The Devonshire Campus of the University of Derby occupies historic premises. Buxton is twinned with Oignies in France and Bad Nauheim in Germany.
View the full Wikipedia page for BuxtonWye Head is an area in Derbyshire, England. It is in the civil parish of Burbage, on the outskirts of Buxton. It is so named because of a major rising of the River Wye, which carries much of the water from Poole's Cavern.
View the full Wikipedia page for Wye HeadThe 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.
The A6 road from Buxton to Bakewell follows the Wye Valley for most of its path. The Manchester, Buxton, Matlock and Midland Junction Railway used to run through the valley. It was built to link Manchester through the Peak District to London and operated from the 1860s to 1968.
View the full Wikipedia page for Wye Valley, Derbyshire