|
Longstone Edge
Longstone Edge is a limestone ridge in the Peak District National Park, in Derbyshire, England. Longstone Edge is immediately north of the village of Great Longstone, which is in turn about north of the town of Bakewell. It runs from east to west for about , from the village of Calver to the River Wye at Monsal Dale and is about wide. It rises to about and commands far-reaching views over the Peak District. Quarrying The Edge has been, and is, intensively quarried for galena, fluorspar and barytes, and more controversially, 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 whe .... Since Longstone Edge is a noted beauty spot within the Peak District National Park, there is strong local pressure for the quarrying to stop altogether. Some of this quarrying is strictly con ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Derbyshire Dales
Derbyshire Dales ( ) is a local government district in Derbyshire, England. The population at the 2011 Census was 71,116. Much of it is in the Peak District, although most of its population lies along the River Derwent. The borough borders the districts of High Peak, Amber Valley, North East Derbyshire and South Derbyshire in Derbyshire, Staffordshire Moorlands and East Staffordshire in Staffordshire and Sheffield in South Yorkshire. The district also lies within the Sheffield City Region, and the district council is a non-constituent partner member of the Sheffield City Region Combined Authority. A significant amount of the working population is employed in Sheffield and Chesterfield. The district offices are at Matlock Town Hall in Matlock. It was formed on 1 April 1974, originally under the name of West Derbyshire. The district adopted its current name on 1 January 1987. The district was a merger of Ashbourne, Bakewell, Matlock and Wirksworth urban districts alon ... [...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] |
Peak District
The Peak District is an upland area in England at the southern end of the Pennines. Mostly in 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 nor ..., it extends into Cheshire, Greater Manchester, Staffordshire, West Yorkshire and South Yorkshire. It includes the Dark Peak, where moorland is found and the geology is dominated by gritstone, and the White Peak, a limestone area with valleys and gorges. The Dark Peak forms an arc on the north, east and west sides; the White Peak covers central and southern tracts. The historic Peak District extends beyond the National Park, which excludes major towns, quarries and industrial areas. It became the first of the national parks of England and Wales in 1951. Nearby Manchester, Stoke-on-Trent, Derby and Sheffield send millions of v ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Great Longstone
Great Longstone with Little Longstone is one of two villages in the local government district of Derbyshire Dales in Derbyshire, England. The population (including Hassop and Rowland, but not Little Longstone) as taken at the 2011 Census was 843. History A place called ''Longsdune'' was mentioned in the Domesday Book as belonging to Henry de FerrersHenry was given a large number of manors in Derbyshire including Doveridge, Spondon, Pilsbury and Breadsall. and being worth thirty shillings; this is considered to be Great Longstone. The church of St Giles in Great Longstone dates from the 13th century. A medieval cross stands in the churchyard, and the head of a cross is built into the wall of the vestry.Neville T. Sharpe, ''Crosses of the Peak District'' (Landmark Collectors Library, 2002) The manor house, Longstone Hall, has its origins in the following century, but was rebuilt in the mid-18th century. That century was one of prosperity, with lead-mining and shoemaking. Th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bakewell
Bakewell is a market town and civil parish in the Derbyshire Dales district of Derbyshire, England, known also for its local Bakewell pudding. It lies on the River Wye, about 13 miles (21 km) south-west of Sheffield. In the 2011 census, the population of the civil parish appeared as 3,949. It was estimated at 3,695 in 2019. The town is close to the tourist attractions of Chatsworth House and Haddon Hall. History Although there is evidence of earlier settlement in the area, Bakewell itself was probably founded in Anglo-Saxon times in the Anglian kingdom of Mercia. The name Bakewell means a spring or stream of a woman named Badeca or Beadeca, so deriving from a personal name with the Old English suffix ''wella''. In 949 it was called Badecanwelle and in the 1086 Domesday Book ''Badequelle''. The Domesday book listing stated that King Edward held land here; the settlement had a church and a mill. These are the outlying estates or berewicks of the manor: Haddon addon or Ov ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Calver
Calver (Old English ''Calf Slope'') is a village and civil parish in Derbyshire, England. The population of the civil parish at the 2011 census was 710. Overview Calver is a small village situated in the Derwent Valley, Derbyshire. The village is bordered by the River Derwent and intersected by the A623 trunk road, responsible for carrying traffic between Manchester to the west, Sheffield to the north and Chesterfield to the east. Stoke Hall is nearby. Today, the village's buildings are predominantly residential, but some local enterprises, including a craft centre, garden centre, petrol station and shop, garage, and two pubs remain. It is also home to Cliff College, which was founded in 1883. There are two camp sites in Calver and many walkers visit the area. Historic mills The village is the site of an historic cotton mill opened in 1778 by John Gardom of Bakewell and John Pares of Leicester in place of a corn mill at leased from Thomas Eyre of Hassop. By 1785 the mill ha ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Monsal Dale
Monsal Dale is a valley in Derbyshire, England, in the White Peak limestone area of the Peak District National Park. It is a Site of Special Scientific Interest (SSSI), a Special Area of Conservation (SAC) (1) and part of a Europe-wide network called Natura 2000. Headstone viaduct The Headstone Viaduct was built by the Midland Railway over the River Wye. The bridge, which stands near the Headstone Tunnel, is long. It had five span arches, some high at the centre. Initially, some slippage occurred, and remedial work was carried out in 1907–08. Whilst considered elegant today, with Grade II listed status being assigned to it in 1970, when it was built in 1863 it was seen as destroying the beauty of the dale. John Ruskin, considered to be Britain's leading cultural critic, harshly criticised the building of the railway: A proposal that never came to fruition was for another viaduct for the Lancashire, Derbyshire and East Coast Railway to cross both the valley and th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Galena
Galena, also called lead glance, is the natural mineral form of lead(II) sulfide (PbS). It is the most important ore of lead and an important source of silver. Galena is one of the most abundant and widely distributed sulfide minerals. It crystallizes in the cubic crystal system often showing octahedral forms. It is often associated with the minerals sphalerite, calcite and fluorite. Occurrence Galena is the main ore of lead, used since ancient times, since lead can be smelted from galena in an ordinary wood fire. Galena typically is found in hydrothermal veins in association with sphalerite, marcasite, chalcopyrite, cerussite, anglesite, dolomite, calcite, quartz, barite, and fluorite. It is also found in association with sphalerite in low-temperature lead-zinc deposits within limestone beds. Minor amounts are found in contact metamorphic zones, in pegmatites, and disseminated in sedimentary rock. In some deposits the galena contains up to 0.5% silver, a byproduct that ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fluorspar
Fluorite (also called fluorspar) is the mineral form of calcium fluoride, CaF2. It belongs to the halide minerals. It crystallizes in isometric cubic habit, although octahedral and more complex isometric forms are not uncommon. The Mohs scale of mineral hardness, based on scratch hardness comparison, defines value 4 as fluorite. Pure fluorite is colourless and transparent, both in visible and ultraviolet light, but impurities usually make it a colorful mineral and the stone has ornamental and lapidary uses. Industrially, fluorite is used as a flux for smelting, and in the production of certain glasses and enamels. The purest grades of fluorite are a source of fluoride for hydrofluoric acid manufacture, which is the intermediate source of most fluorine-containing fine chemicals. Optically clear transparent fluorite lenses have low dispersion, so lenses made from it exhibit less chromatic aberration, making them valuable in microscopes and telescopes. Fluorite optics are also ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Barytes
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 13500, which governs ... [...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] |
