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Rushup Edge
Rushup Edge is a ridge in the Derbyshire Peak District of England. The ridge's highest point is Lord's Seat at , while Mam Tor lies beyond its eastern end, at the western end of the Great Ridge. Lord's Seat is the site of a round barrow. Geology Rushup Edge is part of the ridge which extends east to Mam Tor, Hollins Cross, Back Tor and Lose Hill, separating the Edale and Hope valleys. The ridge is formed of Namurian (c320mya) age Mam Tor Beds (alternating sandstone and siltstone) and landslides on the north have formed colluvium. Protest In October 2014, mountain bikers, walkers, horse riders, climbers and conservationists held a protest against Derbyshire County Council maintenance work on the byway that runs along Rushup Edge. They were upset at the insensitive nature of the work, the cost, the environmental impact and the apparent lack of consultation with them before works began. Derbyshire County Council halted the work to speak with protesters in December 2014. See a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kinder Scout
Kinder Scout is a moorland plateau and national nature reserve in the Dark Peak of the Derbyshire Peak District in England. Part of the moor, at above sea level, is the highest point in the Peak District, in Derbyshire and the East Midlands; this summit is sometimes simply called the Peak. In excellent weather conditions, the city of Manchester and the Greater Manchester conurbation can be seen from the western edges, as well as Winter Hill near Bolton and the mountains of Snowdonia in North Wales. To the north, across the Snake Pass, lie the high moors of Bleaklow and Black Hill, which are of similar elevation. Kinder Scout featured on the BBC television programme ''Seven Natural Wonders'' (2005) as one of the wonders of the Midlands; however, it is considered by many to be in Northern England, lying between the cities of Manchester and Sheffield. In chronostratigraphy, the British sub-stage of the Carboniferous period, the ''Kinderscoutian'', derives its name from Kinder ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lose Hill
Lose Hill lies in the Derbyshire Peak District. It is the south-east corner of the parish of Edale and the end of the Great Ridge that runs from Rushup Edge to the west (over Mam Tor, Hollins Cross and Back Tor). Local access activist G. H. B. Ward was given an area of Lose Hill by the Sheffield and District Federation of the Ramblers Association in 1945, which was named Ward's Piece; he subsequently presented this to the National Trust. Suggested explanations for the name of Lose Hill include that it derives from the Old English ''hlose'', meaning pigsties, or that it may be a corruption of ‘loose’, as in ‘free land’. Another author (Murray) argues that Lose Hill should actually be called ''Laws Hill''. In relatively recent times, the two hills' names have prompted a fanciful tale concerning the outcome of an imagined 7th-century battle between the forces of Edwin of Northumbria and Cynegils of Wessex.> Edwin's forces occupied Win Hill, while Cynegils' men camped on ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains And Hills Of Derbyshire
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rushup
Rushop or RushupMarked as "Rushop" on the modern Ordnance Survey map and the house sign, but all the nearby features sharing this name (Rushup Farm, Rushup Edge etc.) use the "Rushup" spelling, as does the 1940s map. is a small North Derbyshire village. It is in the town of Chapel-en-le-Frith. Agriculture has until recently been the main occupation in the village. At present very few of the residents work in Rushop and several of the houses are second homes only occupied at weekends and holidays. There is archaeological and documentary evidence that there was a settlement at this site since before the Roman invasion of Britain. The settlement is alleged to have been a British village, under nominal Anglo Saxon rule after the fall of the area to Angles from Bernicia around 590, mainly due to the lack of Anglo Saxon placenames in the valley and the presence of names, such as Eccles, Inch and Pen-, which have origins in a Brythonic language of Britain Britain most often refers to: ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rushop
Rushop or RushupMarked as "Rushop" on the modern Ordnance Survey map and the house sign, but all the nearby features sharing this name (Rushup Farm, Rushup Edge etc.) use the "Rushup" spelling, as does the 1940s map. is a small North Derbyshire village. It is in the town of Chapel-en-le-Frith. Agriculture has until recently been the main occupation in the village. At present very few of the residents work in Rushop and several of the houses are second homes only occupied at weekends and holidays. There is archaeological and documentary evidence that there was a settlement at this site since before the Roman invasion of Britain. The settlement is alleged to have been a British village, under nominal Anglo Saxon rule after the fall of the area to Angles from Bernicia around 590, mainly due to the lack of Anglo Saxon placenames in the valley and the presence of names, such as Eccles, Inch and Pen-, which have origins in a Brythonic language of Britain Britain most often refers to: ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Colluvium
Colluvium (also colluvial material or colluvial soil) is a general name for loose, unconsolidated sediments that have been deposited at the base of hillslopes by either rainwash, sheetwash, slow continuous downslope creep, or a variable combination of these processes. Colluvium is typically composed of a heterogeneous range of rock types and sediments ranging from silt to Rock (geology), rock fragments of various sizes. This term is also used to specifically refer to sediment deposited at the base of a hillslope by unconcentrated surface runoff or sheet erosion. Location Colluviation refers to the buildup of colluvium at the base of a hillslope.Jackson, JA, J Mehl, and K. Neuendorf (2005) ''Glossary of Geology'' American Geological Institute, Alexandria, Virginia. 800 pp. Goodie, AS (2003) ''Colluvium'' in A. S. Goodie, ed., pp. 173, Encyclopedia of Geomorphology Volume 1, A–I. Routledge, New York, New York. 1200 pp. Colluvium is typically loosely consolidated angular materi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Siltstone
Siltstone, also known as aleurolite, is a clastic sedimentary rock that is composed mostly of silt. It is a form of mudrock with a low clay mineral content, which can be distinguished from shale by its lack of fissility.Blatt ''et al.'' 1980, pp.381-382 Although its permeability and porosity is relatively low, siltstone is sometimes a tight gas reservoir rock, an unconventional reservoir for natural gas that requires hydraulic fracturing for economic gas production. Siltstone was prized in ancient Egypt for manufacturing statuary and cosmetic palettes. The siltstone quarried at Wadi Hammamat was a hard, fine-grained siltstone that resisted flaking and was almost ideal for such uses. Description There is not complete agreement on the definition of siltstone. One definition is that siltstone is mudrock ( clastic sedimentary rock containing at least 50% clay and silt) in which at least 2/3 of the clay and silt fraction is composed of silt-sized particles. Silt is defined a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Namurian
The Namurian is a stage in the regional stratigraphy of northwest Europe with an age between roughly 326 and 313 Ma (million years ago). It is a subdivision of the Carboniferous system or period and the regional Silesian series. The Namurian is named for the Belgian city and province of Namur where strata of this age occur (part of the Belgian Coal Measures). The Millstone Grit Group in the lithostratigraphy of northern England and parts of Wales is also of Namurian age. The Namurian age lasted from 326 to 313 million years ago. It is preceded by the Visean stage/age (which corresponds to the upper Carboniferous Limestone of Great Britain) and succeeded by the Westphalian stage/age (which corresponds to the lower and middle Coal Measures of Great Britain). In the official geologic timescale of the International Commission on Stratigraphy (ICS), the Namurian straddles the boundary between the Mississippian epoch (359-318 Ma) and the Pennsylvanian epoch (318-299 Ma). The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Edale
Edale is a village and civil parish in the Peak District, Derbyshire, England, whose population was 353 at the 2011 Census. Edale, with an area of , is in the Borough of High Peak. Edale is best known to walkers as the start, or southern end, of the Pennine Way and, to less ambitious walkers, as a starting point for evening or day walks. The village is accessible by generally hourly railway services from Sheffield and Manchester. There are two pubs serving real ale and food. History As spelt, the name is first recorded in 1732. Earlier recorded versions of the name are ''Aidele'' (1086), ''Heydale'' (1251), ''Eydale'' (1275), ''Eydal'' (1285) and ''Edall'' (1550). Historically, Edale was the name of the valley of the River Noe. From the Norman Conquest of England it was in the royal Forest of High Peak and at its centre is the Edale Cross, which marked the boundary of the three wards at the Forest, Campana, Hopedale and Longdendale. Settlement in the valley consists of severa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hollins Cross
Hollins Cross lies between Mam Tor and Lose Hill on the Great Ridge that separates Castleton and Edale in Derbyshire, England. Hollins Cross is the lowest point on the ridge and is therefore a popular route taken by walkers wishing either to cross from one side to the other, or to start a walk along the ridge. It was also the traditional route from Castleton to Edale. Coffins from Edale were taken over Hollins Cross to Hope church until a church was constructed in Edale, leading to the nickname of the "coffin road" for this route.Neville T. Sharpe, ''Crosses of the Peak District'' (Landmark Collectors Library, 2002) There are three well-used paths on both sides of the ridge leading to Hollins Cross. The path west of Hollins Cross is a gentle climb on a paved path of around one kilometre to the summit of Mam Tor. The path east is slightly more taxing with the initial climb up Back Tor being unpaved and badly eroded. Beyond Back Tor the path continues on to Lose Hill on a pave ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dewey (hill)
The mountains and hills of the British Isles are categorised into various lists based on different combinations of elevation, prominence, and other criteria such as isolation. These lists are used for peak bagging, whereby hillwalkers attempt to reach all the summits on a given list, the oldest being the 282 Munros in Scotland, created in 1891. A height above 2,000 ft, or more latterly 610 m, is considered necessary to be classified as a mountain – as opposed to a hill – in the British Isles. With the exception of Munros, all the lists require a prominence above . A prominence of between (e.g. some Nuttalls and Vandeleur-Lynams), does not meet the International Climbing and Mountaineering Federation (UIAA) definition of an "independent peak", which is a threshold over . Most lists consider a prominence between as a "top" (e.g. many Hewitts and Simms). Marilyns, meanwhile, have a prominence above , with no additional height threshold. They range from small hills to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saunders_Quarry-1.jpg "Click for more on -> Sandstone")
