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Lathkill Aqueduct
The River Lathkill is a river in the Peak District National Park in Derbyshire, England. First recorded in 1280, the name "Lathkill" possibly has Scandinavian roots, the old Norse ''hlada-kill'' translating as "narrow valley with a barn". Course In times of high rainfall the source of the river is Lathkill Head Cave (), but in normal conditions the river rises from springs slightly further down the Lathkill Dale valley, close to the village of Monyash, west of Bakewell, and flows generally eastward past the village of Over Haddon and through the village of Alport (where it is joined by the River Bradford) until it meets the River Wye near Rowsley. Roughly six and a half miles from source to outfall, it is the only river in the district that flows over limestone for its entire length. The medieval Conksbury Bridge () now carries the road from Bakewell to Youlgreave. History The dale has a history of lead mining, and among the trees on the north side of the valley are t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tufa
Tufa is a variety of limestone formed when carbonate minerals precipitate out of water in unheated rivers or lakes. Geothermally heated hot springs sometimes produce similar (but less porous) carbonate deposits, which are known as travertine. Tufa is sometimes referred to as (meteogene) travertine. It should not be confused with hot spring (thermogene) travertine. Tufa, which is calcareous, should also not be confused with tuff, a porous volcanic rock with a similar etymology that is sometimes also called "tufa". Classification and features Modern and fossil tufa deposits abound with wetland plants; as such, many tufa deposits are characterised by their large macrobiological component, and are highly porous. Tufa forms either in fluvial channels or in lacustrine environments. Ford and Pedley (1996) provide a review of tufa systems worldwide. Fluvial deposits Deposits can be classified by their depositional environment (or otherwise by vegetation or petrographically). Pedle ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lathkill Aqueduct
The River Lathkill is a river in the Peak District National Park in Derbyshire, England. First recorded in 1280, the name "Lathkill" possibly has Scandinavian roots, the old Norse ''hlada-kill'' translating as "narrow valley with a barn". Course In times of high rainfall the source of the river is Lathkill Head Cave (), but in normal conditions the river rises from springs slightly further down the Lathkill Dale valley, close to the village of Monyash, west of Bakewell, and flows generally eastward past the village of Over Haddon and through the village of Alport (where it is joined by the River Bradford) until it meets the River Wye near Rowsley. Roughly six and a half miles from source to outfall, it is the only river in the district that flows over limestone for its entire length. The medieval Conksbury Bridge () now carries the road from Bakewell to Youlgreave. History The dale has a history of lead mining, and among the trees on the north side of the valley are t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Derbyshire Dales NNR
The Derbyshire Dales National Nature Reserve is a series of unconnected limestone dales in the Peak District National Park. It is managed by Natural England and has a permanent staff of wardens who carry out conservation works and ensure the dales are usable for recreation. The dales are: *Lathkill Dale () *Cressbrook Dale () *Monk's Dale () * Long Dale () *Hay Dale ({{coord, 53.2890, -1.8203, scale:30000_region:GB, display=inline, name=Hay Dale) They are all in the White Peak national character area, of which dales are an integral part. The dales are a mixture of grassland, woodland and scrub; some also have streams (generally winterbournes). They are a haven for biodiversity and many Sites of Special Scientific Interest (SSSI) lie partly or wholly within the reserve boundaries. There are a number of Biodiversity Action Plan species and habitats present. Dippers are common along the River Lathkill, and ravens and buzzards are regularly seen around the dale. The Monyash end of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Compleat Angler
''The Compleat Angler'' (the spelling is sometimes modernised to ''The Complete Angler'', though this spelling also occurs in first editions) is a book by Izaak Walton. It was first published in 1653 by Richard Marriot in London. Walton continued to add to it for a quarter of a century. It is a celebration of the art and spirit of fishing in prose and verse. It was illustrated by Arthur Rackham in 1931. Background Walton was born in Stafford and moved to London when he was in his teens in order to learn a trade. ''The Compleat Angler'' reflects the author's connections with these two locations, especially on the River Dove, Central England that forms the border between Staffordshire and Derbyshire in the Peak District. The book was dedicated to John Offley of Madeley, Staffordshire, and there are references in it to fishing in the English Midlands. However, the work begins with Londoners making a fishing trip up the Lea Valley in Hertfordshire, starting at Tottenham. Walton w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Charles Cotton
Charles Cotton (28 April 1630 – 16 February 1687) was an English poet and writer, best known for translating the work of Michel de Montaigne from the French, for his contributions to ''The Compleat Angler'', and for the influential ''The Compleat Gamester'' attributed to him. Early life He was born in Alstonefield, Staffordshire, at Beresford Hall, near the Derbyshire Peak District. His father, Charles Cotton the Elder, was a friend of Ben Jonson, John Selden, Sir Henry Wotton and Izaak Walton. The son was apparently not sent to university, but was tutored by Ralph Rawson, one of the fellows ejected from Brasenose College, Oxford, in 1648. Cotton travelled in France and perhaps in Italy, and at the age of twenty-eight he succeeded to an estate greatly encumbered by lawsuits during his father's lifetime. Like many Royalist gentlemen after the English Civil War the rest of his life was spent chiefly in quiet country pursuits, in Cotton's case in the Peak District and North Staf ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aqueduct (water Supply)
An aqueduct is a watercourse constructed to carry water from a source to a distribution point far away. In modern engineering, the term ''aqueduct'' is used for any system of pipes, ditches, canals, tunnels, and other structures used for this purpose. The term ''aqueduct'' also often refers specifically to a bridge carrying an artificial watercourse. Aqueducts were used in ancient Greece, ancient Egypt, and ancient Rome. The simplest aqueducts are small ditches cut into the earth. Much larger channels may be used in modern aqueducts. Aqueducts sometimes run for some or all of their path through tunnels constructed underground. Modern aqueducts may also use pipelines. Historically, agricultural societies have constructed aqueducts to irrigate crops and supply large cities with drinking water. Etymology The word ''aqueduct'' is derived from the Latin words (''water'') and (''led'' or ''guided''). Ancient aqueducts Although particularly associated with the Romans, aqueducts we ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mining
Mining is the extraction of valuable minerals or other geological materials from the Earth, usually from an ore body, lode, vein, seam, reef, or placer deposit. The exploitation of these deposits for raw material is based on the economic viability of investing in the equipment, labor, and energy required to extract, refine and transport the materials found at the mine to manufacturers who can use the material. Ores recovered by mining include metals, coal, oil shale, gemstones, limestone, chalk, dimension stone, rock salt, potash, gravel, and clay. Mining is required to obtain most materials that cannot be grown through agricultural processes, or feasibly created artificially in a laboratory or factory. Mining in a wider sense includes extraction of any non-renewable resource such as petroleum, natural gas, or even water. Modern mining processes involve prospecting for ore bodies, analysis of the profit potential of a proposed mine, extraction of the desired materials, an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lead
Lead is a chemical element with the symbol Pb (from the Latin ) and atomic number 82. It is a heavy metal that is denser than most common materials. Lead is soft and malleable, and also has a relatively low melting point. When freshly cut, lead is a shiny gray with a hint of blue. It tarnishes to a dull gray color when exposed to air. Lead has the highest atomic number of any stable element and three of its isotopes are endpoints of major nuclear decay chains of heavier elements. Lead is toxic, even in small amounts, especially to children. Lead is a relatively unreactive post-transition metal. Its weak metallic character is illustrated by its amphoteric nature; lead and lead oxides react with acids and bases, and it tends to form covalent bonds. Compounds of lead are usually found in the +2 oxidation state rather than the +4 state common with lighter members of the carbon group. Exceptions are mostly limited to organolead compounds. Like the lighter members of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Youlgreave
Youlgreave or Youlgrave is a village and civil parish in the Peak District of Derbyshire, England, on the River Bradford south of Bakewell. The name possibly derives from "yellow grove", the ore mined locally being yellow in colour. The population in 1991 was 1,256; it is one of the largest villages in the Peak District National Park. The village has three public houses (the George Hotel, Farmyard Inn and Bull's Head Hotel), and a British Legion club. Geography The village is on the B5056 and the parish has an area of . Youlgrave is at an altitude of located on the southwestern edge of a Carboniferous plateau. It stands on the hillside above the confluence of Lathkill Dale and Bradford Dale. To the east, the geology is shale-like rather than limestone. The area is home to many mineral veins such as fluorspar, galena (lead ore) and calamine (zinc ore). Three long-distance paths, the Alternative Pennine Way, the Limestone Way and the White Peak Way, pass through the village, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Conksbury
Conksbury is the site of a deserted medieval settlement between Over Haddon and Youlgreave in Derbyshire, England. History The village was recorded in the Domesday Book of 1086 AD as ''Cranchesberie'' in the hundred of Blackwell'','' in the county of ''Derbyscire.'' The settlement was one of seven ''berewicks'' (surrounding estates) within the royal manor of Bakewell. It was listed as part of the lands owned by William the Conqueror, with the following details documented for Bakewell (including Burton; Conksbury; Holme; Monyash; ether and OverHaddon; One Ash and Rowsley): * Households: 35 villagers. 16 smallholders. 2 priests. 1 men-at-arms. * Farming: 18 ploughlands. 7 lord's plough teams. 11 men's plough teams. * Meadow 80 acres. Woodland 1 by 1 leagues. 1 mill, value 10 shillings and 7 pence. 1 church. 3 church lands. * Tenant-in-chief in 1086: King William * Lord in 1066: King Edward William the Conqueror subsequently granted the manor of Bakewell to the Norman knight ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alport
Alport is a hamlet in the White Peak area of Derbyshire, England. It lies east of Youlgreave, at the confluence of the River Bradford and the River Lathkill. The oldest house in the hamlet is Monks Hall. There also used to be a pub, which was demolished thanks the construction of a main road, which leads to the A6 and towards Buxton. A Grade-II listed stone bridge crosses the River near the centre of the hamlet, close to the 18th century mill. There are lead mines in the area, and at the Alport mine, an early steam-powered Nutating disc engine was installed. In chronostratigraphy, the British sub-stage of the Carboniferous period, the 'Alportian' derives its name from study of a core from a borehole drilled at Alport. The name ''Alport'' means "Old town", possibly with market trading connotations. The hamlet lies on the line of the Derbyshire Portway, an ancient trading route. Governance Alport is within the civil parish of Youlgreave which, in turn, is part of the Derbyshi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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