Chee Dale | |
---|---|
Geography | |
Location | Derbyshire, England |
Coordinates | 53°15′09″N1°49′18″W / 53.2526°N 1.8218°W |
Rivers | River Wye, Derbyshire |
Chee Dale is a steep-sided gorge on the River Wye near Buxton, Derbyshire, in the Peak District of England.
The Wye valley continues upstream towards Buxton as Wye Dale, while downstream are Miller's Dale village and valley. [1]
Chee Dale has a protected nature reserve (close to the village of Wormhill), which is overseen by the Derbyshire Wildlife Trust. The reserve contains ash, yew and rock whitebeam woodland on the cliff sides and abundant wild flowers including cowslips, early purple orchids, rock rose and the rare Jacob's ladder. Dippers are often seen darting low above the river and bobbing on rocks in the river. Other birds nesting in the valley include blackcap, chiffchaff and willow warbler. [2] Chee Dale is part of the Wye Valley Site of Special Scientific Interest (SSSI), running for 15 kilometres (9.3 mi) east of Buxton. [3]
The Monsal Trail bridleway runs for 8.5 miles (13.7 km) from Topley Pike Junction (at the head of Chee Dale) to Rowsley near Bakewell, along the disused Manchester, Buxton, Matlock and Midlands Junction Railway line. It passes through Upper Chee Dale and then enters Chee Tor Tunnels 1 and 2 through to Miller's Dale. [4]
There is also a riverside footpath along the length of Chee Dale with several wooden footbridges over the river. Sets of stepping stones allow walkers to pass the foot of the cliffs. [5]
The crags of carboniferous limestone in Upper Chee Dale and of Chee Tor cliff in Lower Chee Dale have extensive rock climbing routes. [6] These include the overhanging Cornice and Chee Tor. Chee Tor has the Chee Tor Girdle route, a 167-metre (548 ft) horizontal traverse 20 metres (66 ft) above the cliff base, first climbed in 1964 by Chris Jackson and J. Atkinson. [7]
At the head of Chee Dale, Great Rocks Dale enters from the north, at the former railway stations of Blackwell Mill and Chee Dale Halt. [8] Great Rocks Dale is a dry valley and is the site of Tunstead Quarry, one of the largest limestone quarries in the UK. [9]
The Pennine Bridleway crosses the River Wye over a footbridge at Blackwell Mill.
Access into the deep gorge is limited, though it can be reached from Miller's Dale car park. At the west end of Chee Dale is Topley Pike layby, with limited parking by the A6 road. There is also a short steep footpath from Wormhill. [1]
The Upper Goyt Valley is the southern section of the valley of the River Goyt in North West 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.
Blackwell Mill is a location in Derbyshire, England; it lies near to, but not part of, the village of Blackwell near Buxton. It stands at the meeting point of several valleys: Great Rocks Dale, Chee Dale and Ashford Dale. A railway station was sited here by the Midland Railway; it operated for 92 years.
Monsal Dale is a valley in Derbyshire, England, in the White Peak limestone area of the Peak District National Park. It is a Site of Special Scientific Interest (SSSI), a Special Area of Conservation (SAC) (1) and part of a Europe-wide network called Natura 2000.
Millers Dale is a valley on the River Wye in Derbyshire, England, where there is also a hamlet of the same name.
Millers Dale railway station was in Millers Dale, near Tideswell, in Derbyshire, England. It was opened in 1863 by the Midland Railway on its line from Rowsley, extending the Manchester, Buxton, Matlock and Midlands Junction Railway. It closed in 1967 and the site is now used as a car park for the Monsal Trail, which follows the trackbed.
Tunstead is a village in Derbyshire, England, situated above Great Rocks Dale north of Buxton. It should not be confused with Tunstead Milton, which is roughly five miles to the north west. It is in the civil parish of Wormhill.
The Monsal Trail is a cycling, horse riding and walking trail in the Derbyshire Peak District. It was constructed from a section of the former Manchester, Buxton, Matlock and Midland Junction Railway, which was built by the Midland Railway in 1863 to link Manchester with London and closed in 1968. The Monsal Trail is about 8.5 miles (13.7 km) long and opened in 1981. It starts at the Topley Pike junction in Wye Dale, 3 miles (4.8 km) east of Buxton, and runs to Coombs Viaduct, 1 mile (1.6 km) south-east of Bakewell. It follows the valley of the River Wye. The trail passes through Blackwell Mill, Chee Dale, Millers Dale, Cressbrook, Monsal Dale, Great Longstone, Hassop and Bakewell. The trail has numerous landmarks including Headstone Viaduct, Cressbrook Mill, Litton Mill and Hassop railway station, and passes through six tunnels.
Wormhill is a village and civil parish in the High Peak district of Derbyshire, England, situated east by north of Buxton. The population of the civil parish including Peak Dale was 1,020 at the 2011 Census.
Great Rocks Dale is a dry valley in the Derbyshire Peak District, known for its extensive quarrying.
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.
The White Peak Loop is a 60-mile (97 km) route for walking, cycling and horse riding in the Peak District of England. The trail combines sections of the High Peak Trail and the Monsal Trail with linking sections through the towns of Buxton, Bakewell and Matlock. The White Peak Loop is being developed by Derbyshire County Council and as of 2022 some sections are not yet complete.
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.
Hay Dale is a short dry valley near Buxton, Derbyshire, in the Peak District of England. It is part of a longer valley that runs for approximately 4 miles (6.4 km) north–south from Peak Forest to the River Wye at Millers Dale. This valley has several names along its length: from the northern end running downhill these are Dam Dale, Hay Dale, Peter Dale and Monk's Dale. There is a farmland plateau on either side.
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.
The Derbyshire Dome is a geological formation across mid-Derbyshire in England.
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.