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Peter Dale (Derbyshire)
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Derbyshire
Derbyshire ( ) is a ceremonial county in the East Midlands, England. It includes much of the Peak District National Park, the southern end of the Pennine range of hills and part of the National Forest. It borders Greater Manchester to the north-west, West Yorkshire to the north, South Yorkshire to the north-east, Nottinghamshire to the east, Leicestershire to the south-east, Staffordshire to the west and south-west and Cheshire to the west. Kinder Scout, at , is the highest point and Trent Meadows, where the River Trent leaves Derbyshire, the lowest at . The north–south River Derwent is the longest river at . In 2003, the Ordnance Survey named Church Flatts Farm at Coton in the Elms, near Swadlincote, as Britain's furthest point from the sea. Derby is a unitary authority area, but remains part of the ceremonial county. The county was a lot larger than its present coverage, it once extended to the boundaries of the City of Sheffield district in South Yorkshire where it cov ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ice Age
An ice age is a long period of reduction in the temperature of Earth's surface and atmosphere, resulting in the presence or expansion of continental and polar ice sheets and alpine glaciers. Earth's climate alternates between ice ages and greenhouse periods, during which there are no glaciers on the planet. Earth is currently in the Quaternary glaciation. Individual pulses of cold climate within an ice age are termed ''glacial periods'' (or, alternatively, ''glacials, glaciations, glacial stages, stadials, stades'', or colloquially, ''ice ages''), and intermittent warm periods within an ice age are called '' interglacials'' or ''interstadials''. In glaciology, ''ice age'' implies the presence of extensive ice sheets in both northern and southern hemispheres. By this definition, Earth is currently in an interglacial period—the Holocene. The amount of anthropogenic greenhouse gases emitted into Earth's oceans and atmosphere is predicted to prevent the next glacial period for th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Valleys Of The Peak District
A valley is an elongated low area often running between hills or mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In areas of limestone bedrock, dry valleys may also result from drainage now taking place underground rather than at the surface. Rift valleys arise principally from earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms that may be global in use or else applied only locally. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Roman Roads
Roman roads ( la, viae Romanae ; singular: ; meaning "Roman way") were physical infrastructure vital to the maintenance and development of the Roman state, and were built from about 300 BC through the expansion and consolidation of the Roman Republic and the Roman Empire. They provided efficient means for the overland movement of armies, officials, civilians, inland carriage of official communications, and trade goods. Roman roads were of several kinds, ranging from small local roads to broad, long-distance highways built to connect cities, major towns and military bases. These major roads were often stone-paved and metaled, cambered for drainage, and were flanked by footpaths, bridleways and drainage ditches. They were laid along accurately surveyed courses, and some were cut through hills, or conducted over rivers and ravines on bridgework. Sections could be supported over marshy ground on rafted or piled foundations.Corbishley, Mike: "The Roman World", page 50. Warwick Press, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Batham Gate
Batham Gate is the medieval name for a Roman road in Derbyshire, England, which ran south-west from Templebrough on the River Don, South Yorkshire, River Don in South Yorkshire to Brough-on-Noe (Latin ''Navio Roman Fort, Navio'') and the spa town of Buxton (Latin ''Aquae Arnemetiae'') in Derbyshire. ''Gate'' means "road" in northern English dialects; the name therefore means "road to the bath town". The route of the road from Templebrough to the Roman signal station Navio is disputed. Joseph Hunter (antiquarian), Hunter suggested the Long Causeway at Redmires Reservoirs, Redmires as the route and it was shown as such on Ordnance Survey maps, but this is now known to be a medieval packhorse Salt road, saltway. Roman road historian Ivan Donald Margary said that the Long Causeway had a slightly different route in Roman times. In his book ''Roman Roads In Britain'' he said that evidence is now available that shows that after the Redmires Reservoir the Roman road did not follow the m ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wheston
Wheston is a village and civil parish in the Derbyshire Peak District. Notable features include Wheston Hall and the Wheston Cross. The cross, which survives intact, is more than high. It probably dates from the 14th century and marked the way from Tideswell to Buxton along the Forest Road. Images of the Madonna and Child and the Crucifixion Crucifixion is a method of capital punishment in which the victim is tied or nailed to a large wooden cross or beam and left to hang until eventual death from exhaustion and asphyxiation. It was used as a punishment by the Persians, Carthagi ... are carved into it. The cross is both a scheduled monument and a Grade II* listed building. The village was formerly known as ''Whestone''. References External links {{authority control Towns and villages of the Peak District Villages in Derbyshire Derbyshire Dales ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pennine Bridleway
The Pennine Bridleway is a National Trail in Northern England. It runs roughly parallel with the Pennine Way but provides access for horse riders and cyclists as well as walkers. The trail is around long, extending from Derbyshire to Cumbria. It includes the Mary Towneley Loop and the Settle Loop. In its southern part, it follows the High Peak Trail along the trackbed of the former Cromford and High Peak Railway. History In 1986 Mary Towneley rode on horseback from Corbridge, Northumberland, to Ashbourne, Derbyshire, to launch the idea of a Pennine Bridleway. This was followed by a feasibility study and route investigation from 1987 to 1990. Finally in 1995 approval was granted for the Pennine Bridleway National Trail from Carsington Water, Derbyshire, to Kirkby Stephen, Cumbria. In 1999 Sport England awarded and donated £1,841,876 towards the route from Derbyshire to North Yorkshire and 3 feeder routes from Keighley, Bolton and Penistone. The Pennine Bridleway proje ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Peak District Boundary Walk
The Peak District Boundary Walk is a circular 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 (a branch of the Campaign to Protect Rural England) and was launched on 17 June 2017. The Friends of the Peak District's founders, Gerald and Ethel Haythornthwaite, proposed the boundary of the Peak District National Park, which was subsequently established as the United Kingdom's first National Park in 1951. The route is waymarked with green markers and uses existing footpaths, tracks, quiet lanes, disused railway lines and a canal towpath. The start and finish is at the King's Head pub on Buxton Market Place, where a plaque has been installed by the Peak & Northern Footpaths Society (PNFS). The terrain covers open moorlands of the South Pennines, the limestone scenery of the Derbyshire Dales, woodlands, reservoirs and rural farming ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone Way
The Limestone Way is a waymarked long-distance footpath in Derbyshire, England. It runs for 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 (which became Derbyshire Dales District Council in 1987). It originally ran to Matlock, but was extended to its current, longer route in 1992 to join up with the Staffordshire Way. The route From Castleton, the route runs up Cave Dale, past the village of Peak Forest, down Hay Dale (shared with the Peak District Boundary Walk) and along Peter Dale. It then runs parallel to Monk's Dale and through the village of Millers Dale (passing under the viaduct which carries the Monsal Trail and crossing the River Wye). It then crosses the A6 near the Waterloo Inn ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carboniferous Limestone
Carboniferous Limestone is a collective term for the succession of limestones occurring widely throughout Great Britain and Ireland that were deposited during the Dinantian Epoch of the Carboniferous Period. These rocks formed between 363 and 325 million years ago. Within England and Wales, the entire limestone succession, which includes subordinate mudstones and some thin sandstones, is known as the Carboniferous Limestone Supergroup. Depositional basins Within Great Britain the suite of rocks known traditionally as the Carboniferous Limestone Series was deposited as marine sediments in three distinct ‘provinces’ separated by contemporary landmasses. One of these landmasses was the Wales-London-Brabant Massif, an east–west aligned belt of land stretching through central Wales and the English Midlands to East Anglia and on into Belgium. The limestones deposited to its south form a distinct South Wales-Mendip province which extends from Pembrokeshire in the west through ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
England
England is a country that is part of the United Kingdom. It shares land borders with Wales to its west and Scotland to its north. The Irish Sea lies northwest and the Celtic Sea to the southwest. It is separated from continental Europe by the North Sea to the east and the English Channel to the south. The country covers five-eighths of the island of Great Britain, which lies in the North Atlantic, and includes over 100 smaller islands, such as the Isles of Scilly and the Isle of Wight. The area now called England was first inhabited by modern humans during the Upper Paleolithic period, but takes its name from the Angles, a Germanic tribe deriving its name from the Anglia peninsula, who settled during the 5th and 6th centuries. England became a unified state in the 10th century and has had a significant cultural and legal impact on the wider world since the Age of Discovery, which began during the 15th century. The English language, the Anglican Church, and Engli ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Natural England
Natural England is a non-departmental public body in the United Kingdom sponsored by the Department for Environment, Food and Rural Affairs. It is responsible for ensuring that England's natural environment, including its land, flora and fauna, freshwater and marine environments, geology and soils, are protected and improved. It also has a responsibility to help people enjoy, understand and access the natural environment. Natural England focuses its activities and resources on four strategic outcomes: * a healthy natural environment * enjoyment of the natural environment * sustainable use of the natural environment * a secure environmental future Roles and responsibilities As a non-departmental public body (NDPB), Natural England is independent of government. However, the Secretary of State for Environment, Food & Rural Affairs has the legal power to issue guidance to Natural England on various matters, a constraint that was not placed on its predecessor NDPBs. Its powers inc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
