Taddington

Priestcliffe is a hamlet in Derbyshire, England. The hamlet falls within the civil parish of Taddington. It is about 1.2 km (or 0.75 miles) north of Taddington and within the boundaries of the Peak District National Park.

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.Five Wells is a Neolithic chambered tomb on Taddington Moor and it is a protected scheduled ancient monument. It was first excavated by the local archaeologist Thomas Bateman in 1846. He discovered the remains of at least twelve human skeletons in the stone-paved chambers. Taddington High Mere (on the edge of the moor south of Taddington village) is an ancient pond, formed during the Ice Age. It is a scarce water source on the White Peak limestone plateau. It was recorded in 1690 by John Orme as 'the great pond or meare called Taddington high Meare'. The ancient packhorse track Oriss Road passed the mere. In 2004 the mere was restored by volunteers from Taddington village with funding from the Countryside Agency.The Pennine Bridleway and the Midshires Way trails follow the same route north-south across the moor to the east of Chelmorten and Calton Hill. The Limestone Way long-distance footpath also runs north-south across the moor between Flagg and The Waterloo pub on the A6 road.

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.

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

Blackwell is a village in the Derbyshire Dales local government district of Derbyshire, England, on the A6 main road between Bakewell and Buxton.It is sometimes referred to as "Blackwell-in-the-Peak" to distinguish it from Blackwell near Alfreton. It lies on the River Wye on the edge of the carboniferous limestone of the White Peak. Nearby is Blackwell Hall in the grounds of which have been found neolithic remains, including a flint resharpening flake for tranchet axes. There are also the remnants of a Romano-British field system, dating from around the year 400. The name is said to derive from the Norman Blacheuuelle or King's land. Jedediah Strutt had a farm there. About a mile (1.6 km) to the north west is Blackwell Mill, with the remains of the Midland Railway line from Millers Dale.

Five Wells is a Neolithic chambered tomb between the villages of Chelmorton and Taddington on Taddington Moor in the Derbyshire Peak District in England. The tomb is a protected scheduled ancient monument. Three stones mark the main chamber, which has been dramatically reduced; a second less well-preserved chamber is to the west. The burial mound is over 20 metres (66 ft) in diameter and was first excavated by the local archaeologist Thomas Bateman in 1846. The chambers have paved floors. Bateman discovered the remains of at least twelve human skeletons. Subsequent excavations (by Llewellyn Jewitt, William Lukis and Micah Salt between 1862 and 1901) found further human remains, pottery and flint tools in the chambers and passages and a separate cist (stone coffin) within the mound.Access can be made on foot via a permitted path from Pillwell Gate to the west. Access along the permitted path can also be made from the Limestone Way long-distance footpath, which runs along Sough Lane 500 metres (550 yd) to the east.

Hubble is a short 10-metre (33 ft) bolted sport climb at the limestone crag of Raven Tor in Miller's Dale, in the Peak District in Derbyshire, England. When Hubble was first redpointed by English climber Ben Moon on 14 June 1990, it became the first-ever climb in the world to have a consensus climbing grade of 8c+ (5.14c); and the highest grade in the English system at E9 7b.

Flagg (Old Norse A sod of peat) is a small Peak District village and civil parish, set in the Derbyshire Dales, halfway between the small market town of Bakewell and the spa town of Buxton, in the area known as the White Peak. The population of the civil parish as taken at the 2011 Census was 192.Flagg is predominantly a farming village. As well as farms, houses and cottages, Flagg has an Elizabethan manor house, Flagg Hall, which is not open to the public. There is a caravan/campsite within its grounds. The former Unitarian church, built in 1838, is now a private dwelling. A Methodist chapel is also situated in the village. It was completed in 1839. Next to the chapel is the former village school, now a nursery school. 1000 feet above sea level, Flagg is recorded in the Domesday Book as "Flagun", and is believed to have originally been a Viking settlement engaged primarily in lead mining, the evidence of which can still be seen today with many spoil heaps and disused mine shafts in the area. In the mid-19th century, well dressings were held during "Wakes Week", which was always begun on the first Sunday after June 24. There were two wells, one opposite to Ivy House Farm, and the other opposite to Edge Close Farm. Flagg is known for the point-to-point races held annually on Easter Tuesday by the High Peak Hunt. On one occasion, King Edward VIII, the then Prince of Wales, rode at the races. The village is also popular with hikers and campers, having numerous walks within or close to its boundaries, and several campsites catering for tents, caravans, and motorhomes.

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.

Brushfield is a hamlet and civil parish in the Derbyshire Dales district of Derbyshire, England, in the Peak District National Park. It is about 8 miles east of Buxton. According to the 2001 census it had a population of 13. In 2007 it had just three houses. Several holiday lets are run by two separate families. One of these cottages is called the 'Old School House', a small one-bed house of stone. There are three scheduled monuments in the parish: bowl barrows at Brushfield Hough and Putwell Hill and High Field hlæw, a rare pre-Christian burial monument dating from around 600AD.

Calton Hill is a Site of Special Scientific Interest in Derbyshire, England, showing Olivine Diorite magma chamber.It is the site of an extinct volcano and the quarrying that has now been abandoned means that it is possible to observe the geological structures caused by the repeated eruptions. The eruptions were small and were then underwater as Derbyshire was covered by a sea in the Carboniferous period (around 330 million years ago).The nearest place is Blackwell and the nearest town is Buxton to the west.

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.