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Harboro' Rocks
Harboro' Rocks (or Harborough Rocks) is a dolomitic limestone hill near the village of Brassington in the Derbyshire Peak District. The summit is above sea level with views across to Carsington Water. Harboro' Cave is a natural cavern in the rocks where archaeologists have found evidence of human occupants since the Ice Age. Satirist author Daniel Defoe reported in his book ''Tour thro' the whole Island of Great Britain'' (published in 1726) that a poor family of seven was living in the cave. Defoe described how the father was a lead miner and was "lean as a skeleton, pale as a dead corps" but that they "seemed to live very pleasantly". The cave is a protected Scheduled Monument. There is a settlement site and chambered cairns nearby. The Golconda lead mine, on the north east side of the hill, was part of the Gell family's Griffe Grange mining liberty, which ran from the summit of Harboro' Rocks to Via Gellia. The mine dates back to the 1700s and the mine shaft is over deep. ...
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Brassington
Brassington is a village and civil parish in the Derbyshire Dales district of Derbyshire, 16 miles north west of Derby. The parish had a population of 573 at the 2011 census. The name, spelled ''Branzingtune'' in the Domesday Book, is thought to mean "Brand's people's place". Most of the houses in the village are built of local limestone, and most are 200 or 300 years old; there are 20th-century houses at the south end of the village. The oldest dated house, named Tudor House since the late 19th century, was built in 1615. It is located on Town Street () and was an inn until 1820, when it was bought by the parish and was used as a workhouse until 1848. There were 15 inmates at the 1841 census, but the number rose considerably in 1845, when the Brassington Poor Law Union was wound up and Brassington joined the new Ashbourne Union. The Brassington workhouse, augmented by the nearby George and Dragon pub, served the new union while a new workhouse was built in Ashbourne. The work ...
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Via Gellia
The A5012 road is a main road in the south of the English county of Derbyshire. Route Around in length, it connects two primary north–south routes; the A6 at Cromford and the A515 between Buxton and Ashbourne. It passes through Pikehall and Grangemill and alongside Ible. Via Gellia The eastern part (Grangemill to Cromford, set in a deep valley) is known as the Via Gellia – a steep-sided wooded dry valley and road. It is probably named after (or by) Philip Eyre Gell in a mock- Latin style; he was responsible for building the road through the valley, the name being a link to the Gell family's claim of Roman descent. They held lead-mining interests in and around Wirksworth. At its lower (eastern) end is the village of Cromford and its Georgian mill, built by inventor and entrepreneur Richard Arkwright. At the western end is the hamlet of Grangemill Grangemill is a village in the English county of Derbyshire. The hamlet
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Mountains And Hills Of The Peak District
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain an ...
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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 an ...
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Midshires Way
The Midshires Way is a long-distance footpath and bridleway that runs for from the Chiltern Hills from near Bledlow in Buckinghamshire, through the Midlands counties of Northamptonshire, Leicestershire, Nottinghamshire and Derbyshire, to Stockport, Greater Manchester. It also links several other long-distance walking routes or trackways including The Ridgeway, the Pennine Bridleway and the Trans Pennine Trail. The route was opened in 1994 as a collaboration between numerous Local Authorities and user groups. It is intended as a multi-user trail but there are places where the recommended route for walkers differs from the route for horse riders and cyclists. Buckinghamshire section The Midshires Way starts from Wain Hill (), between Bledlow and Chinnor. From there it runs near Princes Risborough north to Waddesdon and on to Winslow then in a northwest direction passing through the town of Milton Keynes. North of the town it passes to the west of Stoke Goldington before cr ...
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High Peak Trail
The High Peak Trail is a trail for walkers, cyclists and horse riders in the Peak District of England. Running from Dowlow , near Buxton, to High Peak Junction, Cromford , it follows the trackbed of the former Cromford and High Peak Railway, which was completed in 1831 to carry minerals and goods between the Cromford Canal wharf at High Peak Junction and the Peak Forest Canal at Whaley Bridge. Closure of the line occurred during the Beeching era, with the first section of the line closing in 1963 (i.e. the Middleton Incline) followed by full closure in 1967. In 1971 the Peak Park Planning Board and Derbyshire County Council bought the largest part of the trackbed and, in partnership with the Countryside Commission, adapted it for its current leisure use. The trail has a crushed limestone surface which makes it ideal for all users, including wheelchair use, assisted by level access onto the trail at various points along its route. The High Peak Trail is now a national ...
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Countryside And Rights Of Way Act 2000
The Countryside and Rights of Way Act 2000 (c. 37), known informally as the CRoW Act or "Right to Roam" Act is a United Kingdom Act of Parliament affecting England and Wales which came into force on 30 November 2000. Right to roam The Act implements the so-called "right to roam" (also known as ''jus spatiandi'') long sought by the Ramblers' Association and its predecessors, on certain upland and uncultivated areas of England and Wales. This element of the act was implemented in stages as conclusive maps of different regions were produced. The act refers to areas of 'mountain, moor, heath and down' in addition to registered common land; not all uncultivated land is covered. Rights of way A staged review of public rights of way, including limited rights to create new public footpaths where needed, is being conducted under the Act. Again, this is being conducted in a staged manner, which can produce anomalies – of the two administrative areas of the County of Gloucestershi ...
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Megalithic Architectural Elements
This article describes several characteristic architectural elements typical of European megalithic ( Stone Age) structures. Forecourt In archaeology, a forecourt is the name given to the area in front of certain types of chamber tomb. Forecourts were probably the venue for ritual practices connected with the burial and commemoration of the dead in the past societies that built these types of tombs. In European megalithic architecture, forecourts are curved in plan with the entrance to the tomb at the apex of the open semicircle enclosure that the forecourt creates. The sides were built up by either large upright stones or walls of smaller stones laid atop one another. Some also had paved floors and some had blocking stones erected in front of them to seal the tomb such as at West Kennet Long Barrow. Their shape, which suggests an attempt to focus attention on the tomb itself may mean that they were used ceremonially as a kind of open air auditorium during ceremonies. Excavation ...
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Romano-British Culture
The Romano-British culture arose in Britain under the Roman Empire following the Roman conquest in AD 43 and the creation of the province of Britannia. It arose as a fusion of the imported Roman culture with that of the indigenous Britons, a people of Celtic language and custom. Scholars such as Christopher Snyder believe that during the 5th and 6th centuries – approximately from 410 when the Roman legions withdrew, to 597 when St Augustine of Canterbury arrived – southern Britain preserved an active sub-Roman culture that survived the attacks from the Anglo-Saxons and even used a vernacular Latin when writing. Arrival of the Romans Roman troops, mainly from nearby provinces, invaded in AD 43, in what is now part of England, during the reign of Emperor Claudius. Over the next few years the province of Britannia was formed, eventually including the whole of what later became England and Wales and parts of Scotland.Kinder, H. & Hilgemann W. ''The Penguin Atlas of Wor ...
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Arête
An arête ( ) is a narrow ridge of rock which separates two valleys. It is typically formed when two glaciers erode parallel U-shaped valleys. Arêtes can also form when two glacial cirques erode headwards towards one another, although frequently this results in a saddle-shaped pass, called a col. The edge is then sharpened by freeze-thaw weathering, and the slope on either side of the arête steepened through mass wasting events and the erosion of exposed, unstable rock. The word ''arête'' () is actually French for "edge" or "ridge"; similar features in the Alps are often described with the German equivalent term ''Grat''. Where three or more cirques meet, a pyramidal peak is created. Cleaver A ''cleaver'' is a type of arête that separates a unified flow of glacial ice from its uphill side into two glaciers flanking, and flowing parallel to, the ridge. ''Cleaver'' gets its name from the way it resembles a meat cleaver slicing meat into two parts. A cleaver may be t ...
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White Peak
The White Peak, also known as the Low Peak, is a limestone plateau that forms the central and southern part of the Peak District in England. It is mostly between and above sea-level and is enclosed by the higher altitude Dark Peak (also known as the High Peak) to the west, north and east. Area Broadly speaking, the White Peak covers the Derbyshire and Staffordshire parts of the Peak District from the Hope Valley southwards to the Weaver Hills near the Churnet Valley. As defined by Natural England, the White Peak national character area covers and includes the area approximately bounded by Ashbourne, Buxton, Castleton, Matlock and Wirksworth. Geology and soils The geology of the White Peak has its origins in the Carboniferous Period, when the area was under a shallow sea that was fringed by reefs, leading to thick deposits of shelly calcareous material. Over millions of years the area rose up and subsided several times, leading to muddy, sandy and peaty deposit ...
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Baryte
Baryte, barite or barytes ( or ) is a mineral consisting of barium sulfate ( Ba S O4). Baryte is generally white or colorless, and is the main source of the element barium. The ''baryte group'' consists of baryte, celestine (strontium sulfate), anglesite (lead sulfate), and anhydrite (calcium sulfate). Baryte and celestine form a solid solution (Ba,Sr)SO4. Names and history The radiating form, sometimes referred to as ''Bologna Stone'', attained some notoriety among alchemists for specimens found in the 17th century near Bologna by Vincenzo Casciarolo. These became phosphorescent upon being calcined. Carl Scheele determined that baryte contained a new element in 1774, but could not isolate barium, only barium oxide. Johan Gottlieb Gahn also isolated barium oxide two years later in similar studies. Barium was first isolated by electrolysis of molten barium salts in 1808 by Sir Humphry Davy in England. The American Petroleum Institute specification API 13/ ISO 135 ...
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