Wheston

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.The walking along the flat valley floor is easy except for a couple of short rock-strewn sections. The Limestone Way long-distance footpath runs along the length of the gentle valley floor. The Peak District Boundary Walk trail passes the northern end of the valley. The Pennine Bridleway runs across the southern end and then parallel to the dale about 1km to the east (through the hamlet of Wheston). Where the Limestone Way crosses the A623 road (about 1 km north of Hay Dale), the route of the old Batham Gate Roman road runs east–west.Peter Dale's limestone cliffs are well-suited to rock climbing, with 25 graded routes on Main Crag.Access into Peter Dale from the south can be made from the hamlet of Wormhill along the Pennine Bridleway. From the north there is a footpath from the village of Peak Forest (on the A623 road) through Dam Dale and Hay Dale.

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.The dale is named after monks of Lenton Priory (a Benedictine monastery in Nottingham). During the 12th-century the priory was granted the income from a large area of north Derbyshire by William Peverel. 14th-century carved stones (of the low septum, or stone screen, dividing the chancel from the nave) are all that remains of the monks' grange.The valley is dry over the summer but has a winterbourne stream which runs into the River Wye at Miller's Dale. Monk's Dale is part of the Derbyshire Dales National Nature Reserve. Natural England manages the reserve which covers five separate dales of the White Peak (Lathkill Dale, Cressbrook Dale, Hay Dale, Long Dale and Monk's Dale). The reserve contains ash and elm woodland and shrubs including herb Paris, bird cherry and dogwood. Uncommon flowers in the shady dale include dark red helleborine. Native grasses include meadow oat, glaucous sedge, oat grass, cottongrass, knapweed and upright brome. Monk's Dale is also a designated Site of Special Scientific Interest (SSSI). It is especially important for the lichens on the shaded, limestone cliffs. There are two Grade II listed buildings at Miller's Dale at the southern end of the valley: The Anglers Rest pub from the 1700s and the Church of St Anne from 1879.The footpath along the length of the valley floor is challenging rough terrain for walkers. The Limestone Way long-distance footpath and Pennine Bridleway run along the same route on the plateau to the east of Monk's Dale. The Monsal Trail bridleway runs along the Wye Valley at the southern end of Monk's Dale.Access into the deep gorge is limited to the entry points at each end. Footpaths from the Wormhill village, from Peter Dale and from the Limestone Way converge at the northern end. At the southern foot of the dale, there is a large car park at Miller's Dale station on the Monsal Trail.

St Margaret's Church, Wormhill is a Grade II* listed parish church in the Church of England in Wormhill, Derbyshire.

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.Wormhill was mentioned in the Domesday book as belonging to Henry de Ferrers and containing 20 acres (81,000 m2) of meadow. The name is said by the English Place-Name Society to be derived from the Old English 'Wyrma's hyll'.There was a tradition of wolf hunting in Wormhill in the fourteenth century. It was said that a living was made by some and that an annual tribute of wolfheads was shown. It has been reported that the last wolf killed in England was at Wormhill Hall in the 15th century.From 1863 to 1967 the village was served by Millers Dale railway station, some 2 miles away, which was on the Midland Railway's extension of the Manchester, Buxton, Matlock and Midlands Junction Railway. The disused railway line is now the Monsal Trail bridleway. A footpath south of the village leads to the nearby River Wye in Chee Dale. The Peak District Boundary Walk runs past Wormhill on its way from Buxton to Peak Forest.It has memorials to James Brindley, pioneer builder of Britain's canals, who was born in 1716 in the hamlet of Tunstead within Wormhill parish. The well in Wormhill is dedicated to Brindley. As part of the annual well dressing festival the Brindley well is decorated each year and there is also a smaller well dressing in the churchyard of St Margaret's Church in the village. The lower part of a cross shaft and its stepped base stand in the churchyard. A sundial dated 1670 tops the broken shaft. Only the base of the church tower is medieval; the rest of the church was "almost rebuilt" in 1864, and a transept added in 1904–10.Near the church and Brindley's well can be found the old village stocks. At the north end of the village lies the hamlet of Hargate (now part of Wormhill), where the industrialist Robert Whitehead and notorious mill owner Ellis Needham once lived.

Wormhill Hall is a 17th-century grade II* listed country hall in Wormhill, Derbyshire.

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 (on the A623 road) 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.Hay Dale is part of the Derbyshire Dales National Nature Reserve. Natural England manages the reserve which covers five separate dales of the White Peak (Lathkill Dale, Cressbrook Dale, Hay Dale, Long Dale and Monk's Dale). The Carboniferous limestone rocks of the reserve 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. The reserve contains ash woodland, limestone grassland and many wildflowers including early purple orchid, cowslip, common rock rose and thyme. Butterflies are abundant and include the brown argus. The Limestone Way and the Peak District Boundary Walk long-distance footpaths run along the length of the gentle valley floor. The Pennine Bridleway crosses the northern end of the dale, dividing it from Dam Dale. Where the Limestone Way crosses the A623 road about 1 mile (1.6 km) north of Hay Dale, the route of the old Batham Gate Roman road runs east–west.Access into Hay Dale from the north is via a footpath from Peak Forest through Dam Dale. From the south, the dale can be reached from the village of Wormhill along the Pennine Bridleway and through Peter Dale. A minor road running west from Wheston marks the southern end of Hay Dale and the start of Peter Dale.

Millers Dale railway station was situated in Millers Dale, near Tideswell, in the Peak District.

Hargate Wall is a hamlet in Derbyshire, England, situated northeast of Buxton and now part of Wormhill. The name Hargate Wall derives from Old English Herdwyk-waella, meaning "herd farm by the spring", so the first settlement was probably around AD 700–950. The hamlet now consists of several cottages, farms and property called Hayward Farm and Hargate Hall (completed and lived in by Robert Whitehead). On the edge of Hargate Wall is a Neolithic barrow known as Wind Low (53.2733°N 1.8299°W / 53.2733; -1.8299 (Wind Low)). Excavations have revealed the remains of a Neolithic chieftain and his family, a female member of a Celtic tribe and a Celtic necklace which is now in the Weston Park Museum in Sheffield.

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 Carboniferous limestone rocks of 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. The disused basalt quarry on the east side of Tideswell Dale is now a nature reserve. Stone was quarried from a sill of dolerite rock, which was the result of lava rising through the strata of the surrounding limestone 'Debyshire Dome'. Tideswell Dale is part of the designated Wye Valley Site of Special Scientific Interest (SSSI) between Buxton and Bakewell, which also covers Cunning Dale, Woo Dale, Wye Dale, Chee Dale, Monsal Dale and Taddington Wood. These dales contain ancient ash and wych elm woodland. The many herbs and wild flowers include lady's bedstraw, bird's-foot trefoil, bloody cranesbill, devil's-bit scabious, saw-wort, ox-eye daisy, cowslip and common spotted-orchid. The upper valley sides are heathland habitat for bilberry and heather. The dale is also home to small heath and common blue butterflies.Ravenstor at the foot of Tideswell Dale is a huge outcrop of overhanging rock. It is a challenging rock climbing location with over 200 graded routes, up to 50m long and including Mutation, graded 9a making it the hardest route in the Peak District. There are also several limestone buttresses in Tideswell Dale itself with established rock climbing pitches.Access into Tideswell Dale is easy from the B6049 road which runs down the valley from Tideswell in the north to Miller's Dale, about 1 km west of the south end of the dale. Tideswell Dale car park is on the B6049 from where the footpath follows an avenue of mature beech trees. A footpath runs from the Monsal Trail, over the footbridge at Litton Mill up through the dale to Tideswell. There is also a parking area near Litton Mill.

Millers Dale (Ordnance Survey: Miller's Dale) is a valley on the River Wye in Derbyshire, England, where there is also a hamlet of the same name. It is a popular beauty spot in the Peak District of England, much of the area being preserved as a Site of Special Scientific Interest. Nearby are Ravenstor and Chee Dale, both popular with rock-climbers. Just to the north of the dale lie the village of Wormhill and the lesser-known valleys of Peter Dale and Monk's Dale, the latter being listed as a Site of Special Scientific Interest and a nature reserve. A local landmark is the viaduct, first built by the Midland Railway in 1866. Increasing traffic meant that a second viaduct parallel to the first was built in 1905, increasing the number of tracks to four. Millers Dale station was at the junction where passengers for Buxton joined or left the trains between London and Manchester. The station closed in 1967 and the line closed in the following year. Large sections of the trackbed now form part of the Monsal Trail, a cycle and walking trail.Northwards from Millers Dale the line entered the two Chee Tor tunnels (401 and 94 yards), separated by a 50-foot-high (15 m) bridge over the River Wye, then along a ledge cut into the rock face, before entering Rusher Cutting tunnel (121 yards), crossing the Wye again by another viaduct. The line here was immensely difficult and expensive to construct, skirting, as it did, the base of the 300-foot (91 m) high ciff of Chee Tor. Chee number 1 was, until May 2011, sealed off for safety reasons, but it is now possible to walk through all three tunnels. Further on was the triangular junction for Buxton via Blackwell Mill, before continuing to Peak Forest. The area is of great interest to geologists, particularly where the strata have been exposed by quarries and railway cuttings. In Station Quarry two layers of limestone can be seen, separated by a bed of shale. At one point there is a dip in the lower layer, possibly from a watercourse, millions of years ago. This is filled with the shale and a large limestone boulder can be seen within it. Elsewhere in the area there are signs of lava flows from long-ago volcanic activity.

Tideswell is a village, civil parish, and ward in the Peak District of Derbyshire, England. It lies 6 miles (9.7 km) east of Buxton on the B6049, in a wide valley on a limestone plateau, at an altitude of 1,000 feet (300 m) above sea level, and is within the District of Derbyshire Dales. The population (including Wheston) was 1,820 in 2001, increasing slightly to 1,827 at the 2011 Census, making it the second-largest settlement within the National Park, after Bakewell. Tideswell Dale is a short limestone valley leading south from the village to the River Wye valley.

The church of St John the Baptist in Tideswell is a Church of England parish church.