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Grin Low
Grin Low is a hill overlooking Buxton in Derbyshire, in the Peak District. The summit is above sea level. Grin Low was the main location for the early Buxton lime industry. It was an extensive area of limestone quarrying and was licensed for lime burning from 1662 by the 1st Duke Of Devonshire. Demand for lime grew dramatically during the Industrial Revolution. There are widespread remains of over 100 large 'pudding' lime kilns, built of earth and rock, which date from the 17th–19th centuries. The land is also covered in spoil heaps of waste material. Coal came from local collieries at Axe Edge and Goyts Moss. In 1820 the 6th Duke of Devonshire commissioned the 'Grin Plantation' (now the wooded Buxton Country Park) to shield the scarred lime-burning landscape from visitors to the spa town of Buxton. The Cromford and High Peak Railway opened in 1831 and passed by Grin Low. The railway allowed the lime to be transported to canals and generated expansion of quarrying in Buxton. ...
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Buxton Lime Industry
The Buxton lime industry has been important for the development of the town of Buxton in Derbyshire, England, and it has shaped the landscape around the town. Geology The White Peak area of the Peak District is named after the limestone plateau landscape of the 'Derbyshire Dome'. This limestone outcrop is surrounded by a horseshoe-shaped formation of younger sandstones ( gritstones) and shales. Buxton is at the western edge of the limestone region. The layers of carboniferous limestone were deposited in a warm shallow sea in the Brigantian stage of the Carboniferous period (around 330 million years ago). These deposits were compressed into rocks which over time were uplifted and folded into a dome. Erosion of the younger sandstones exposed the limestone strata. The limestone in the Bee Low and Woo Dale limestone formations around Buxton is of unusually high quality, with less than 3% dolomite and less than 1% chert. History Limestone has been quarried as building stone in ...
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Buxton
Buxton is a spa town in the Borough of High Peak, Derbyshire, England. It is England's highest market town, sited at some above sea level."Buxton – in pictures"
, BBC Radio Derby, March 2008, accessed 3 June 2013.
also claims this, but lacks a regular market. It lies close to to the west and to the south, on the edge of the



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 ...
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River Wye, Derbyshire
The River Wye is a limestone river in the Peak District of Derbyshire, England. It is 22 miles long (widely but incorrectly attributed as 15 miles/24 km, which refers to the section within the National Park), and is one of the major tributaries of the River Derwent, which flows into the River Trent, and ultimately into the Humber and the North Sea. The river rises just west of Buxton, on Axe Edge Moor. Part of the flow passes underground through Poole's Cavern before rising at Wye Head, and flowing through the Pavilion Gardens in Buxton. It then flows east through the dales of the Wye Valley, along a route roughly followed by the A6 road. It enters the Peak District, flows just south of Tideswell, then through Ashford in the Water and Bakewell, and south of Haddon Hall, before meeting the River Derwent at Rowsley. The main tributary of the river is the River Lathkill, which enters approximately one mile from its mouth. The River Wye is one of Derbyshire's best-known ...
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Mary, Queen Of Scots
Mary, Queen of Scots (8 December 1542 – 8 February 1587), also known as Mary Stuart or Mary I of Scotland, was Queen of Scotland from 14 December 1542 until her forced abdication in 1567. The only surviving legitimate child of James V of Scotland, Mary was six days old when her father died and she inherited the throne. During her childhood, Scotland was governed by regents, first by the heir to the throne, James Hamilton, Earl of Arran, and then by her mother, Mary of Guise. In 1548, she was betrothed to Francis, the Dauphin of France, and was sent to be brought up in France, where she would be safe from invading English forces during the Rough Wooing. Mary married Francis in 1558, becoming queen consort of France from his accession in 1559 until his death in December 1560. Widowed, Mary returned to Scotland in August 1561. Following the Scottish Reformation, the tense religious and political climate that Mary encountered on her return to Scotland was further agitated by pro ...
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Seven Wonders Of The Peak
The Seven Wonders of the Peak were described in the 17th century by the philosopher Thomas Hobbes in his book ''De Mirabilibus Pecci: Being The Wonders of the Peak in Darby-shire, Commonly called The Devil's Arse of Peak.'' The wonders refer to places to visit in the Peak District of Derbyshire in England. Thomas Hobbes worked for the Dukes of Devonshire at Chatsworth House, as tutor and secretary. After touring the High Peak in 1626, Hobbes published his 84-page Latin poem ''De Mirabilibus Pecci'' in 1636. It was published with an English translation in 1676. He recounted:"Of the High Peak are seven wonders writ. Two fonts, two caves. One pallace, mount and pit."These wonders are: Mary Queen of Scots is known to have visited three of the wonders. By command of Queen Elizabeth I, she was held prisoner at Chatsworth House several times between 1569 and 1584 (her rooms are still called the Queen of Scots Apartments). Mary was granted permission by the Queen to ‘take the cure ...
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Roman Empire
The Roman Empire ( la, Imperium Romanum ; grc-gre, Βασιλεία τῶν Ῥωμαίων, Basileía tôn Rhōmaíōn) was the post-Republican period of ancient Rome. As a polity, it included large territorial holdings around the Mediterranean Sea in Europe, North Africa, and Western Asia, and was ruled by emperors. From the accession of Caesar Augustus as the first Roman emperor to the military anarchy of the 3rd century, it was a Principate with Italia as the metropole of its provinces and the city of Rome as its sole capital. The Empire was later ruled by multiple emperors who shared control over the Western Roman Empire and the Eastern Roman Empire. The city of Rome remained the nominal capital of both parts until AD 476 when the imperial insignia were sent to Constantinople following the capture of the Western capital of Ravenna by the Germanic barbarians. The adoption of Christianity as the state church of the Roman Empire in AD 380 and the fall of the Western ...
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Bronze Age
The Bronze Age is a historic period, lasting approximately from 3300 BC to 1200 BC, characterized by the use of bronze, the presence of writing in some areas, and other early features of urban civilization. The Bronze Age is the second principal period of the three-age system proposed in 1836 by Christian Jürgensen Thomsen for classifying and studying ancient societies and history. An ancient civilization is deemed to be part of the Bronze Age because it either produced bronze by smelting its own copper and alloying it with tin, arsenic, or other metals, or traded other items for bronze from production areas elsewhere. Bronze is harder and more durable than the other metals available at the time, allowing Bronze Age civilizations to gain a technological advantage. While terrestrial iron is naturally abundant, the higher temperature required for smelting, , in addition to the greater difficulty of working with the metal, placed it out of reach of common use until the end o ...
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Stone Age
The Stone Age was a broad prehistoric period during which stone was widely used to make tools with an edge, a point, or a percussion surface. The period lasted for roughly 3.4 million years, and ended between 4,000 BC and 2,000 BC, with the advent of metalworking. Though some simple metalworking of malleable metals, particularly the use of gold and copper for purposes of ornamentation, was known in the Stone Age, it is the melting and smelting of copper that marks the end of the Stone Age. In Western Asia, this occurred by about 3,000 BC, when bronze became widespread. The term Bronze Age is used to describe the period that followed the Stone Age, as well as to describe cultures that had developed techniques and technologies for working copper alloys (bronze: originally copper and arsenic, later copper and tin) into tools, supplanting stone in many uses. Stone Age artifacts that have been discovered include tools used by modern humans, by their predecessor species in the ...
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Stalagmite
A stalagmite (, ; from the Greek , from , "dropping, trickling") is a type of rock formation that rises from the floor of a cave due to the accumulation of material deposited on the floor from ceiling drippings. Stalagmites are typically composed of calcium carbonate, but may consist of lava, mud, peat, pitch, sand, sinter, and amberat (crystallized urine of pack rats). The corresponding formation hanging down from the ceiling of a cave is a stalactite. Mnemonics have been developed for which word refers to which type of formation; one is that ''stalactite'' has a C for "ceiling", and ''stalagmite'' has a G for "ground", another is that, as with ants in the pants, the mites go up and the tights (tites) come down. Formation and type Limestone stalagmites The most common stalagmites are speleothems, which usually form in limestone caves. Stalagmite formation occurs only under certain pH conditions within the cavern. They form through deposition of calcium carbonate ...
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Stalactite
A stalactite (, ; from the Greek 'stalaktos' ('dripping') via ''stalassein'' ('to drip') is a mineral formation that hangs from the ceiling of caves, hot springs, or man-made structures such as bridges and mines. Any material that is soluble and that can be deposited as a colloid, or is in suspension, or is capable of being melted, may form a stalactite. Stalactites may be composed of lava, minerals, mud, peat, pitch, sand, sinter, and amberat (crystallized urine of pack rats). A stalactite is not necessarily a speleothem, though speleothems are the most common form of stalactite because of the abundance of limestone caves. The corresponding formation on the floor of the cave is known as a stalagmite. Mnemonics have been developed for which word refers to which type of formation; one is that ''stalactite'' has a C for "ceiling", and ''stalagmite'' has a G for "ground". Another example is that ''stalactites'' "hang on ''T''ight" and ''stalagmites'' "''M''ight grow up" ...
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Poole's Cavern
Poole's Cavern or Poole's Hole is a two-million-year-old natural limestone cave on the edge of Buxton in the Peak District, in the county of Derbyshire, England. Poole's Cavern forms part of the Wye system, and has been designated a Site of Special Scientific Interest. Human history The name derives from an outlaw, Poole, who reputedly used the cave as a lair and a base to rob travellers in the fifteenth century. Archeological explorations in 1981 and 1983 have suggested that the cave was occupied from the Bronze Age. Some of the finds have been interpreted as suggesting that one of the chambers was used for religious purposes by Romano-Britons; an alternative explanation is that the cave was a metal-workers' workshop. Officially opened as a show cave in 1853 by the 6th Duke of Devonshire, the cave was already a tourist attraction, being listed as one of the Seven Wonders of the Peak by Thomas Hobbes in 1636 and in Charles Cotton's poetic essay on the same subject in 1681. Earl ...
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