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Flash (lake)
A flash is a body of water that forms where the land below it has subsided. Whilst these are mostly found in areas where mining has taken place, some can occur naturally. Collectively they are known as ''Flashes'' History Flash is recorded as being a dialectal word from Cheshire, which describes the water filled depressions caused by subsidence. Some have said that word was used as far back as the 17th century when describing small bodies of water across Cheshire, and was derived from a French word for puddle. Another writer states the "Flash or Plash, deriving from ''splash'', are small puddles left over after a thunderstorm". In William Gresley's book, "A Glossary of Terms Used in Coal-Mining", Gresley states that the word originated in the salt mining districts of Cheshire and defines it as: Flashes are common in former mining areas such as Cheshire, Lancashire and Yorkshire, where mining has had an effect on the landscape. In Cheshire especially, rock salt and brine extrac ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sprotbrough Flash - Geograph
Sprotbrough is a village in the City of Doncaster in South Yorkshire, England, west of the centre. With Cusworth to the north, it forms the civil parish of Sprotbrough and Cusworth. Sprotbrough village had a population of 3,321 at the 2011 census; this does not include the area of Newton to the east of the A1(M). The civil parish of Sprotbrough and Cusworth had a population of 12,134, which also includes Cusworth, Newton and part of Scawsby. The electoral ward of Sprotbrough, including numerous rural villages to the north and west, had a population of 11,143. History The place name 'Sprotbrough' is first attested in the Domesday Book of 1086, where it appears as ''Sproteburg''. The name is thought to mean 'Sprot's borough'. Much of the local land was owned by the Fitzwilliam family until the 15th century, when the Copley family emerged as major landowners. Sprotbrough Village harbours the Grade I listed St Mary's Church and The Old Rectory – the childhood home of Se ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pennington Flash Country Park
Pennington Flash Country Park is a country park located between Lowton and Leigh in Greater Manchester, England. History A flash is a water-filled hollow formed by subsidence. Pennington Flash is a lake created at the turn of the 20th century by coal mining subsidence, mainly from Bickershaw Colliery. Before the flash the area contained two farms, both of which were abandoned in the early 1900s due to flooding. During the 1960s and 1970s the idea to convert the flash for recreation was emerging and the country park was opened in 1981. Nature Pennington Flash Country Park is a nature reserve. Over 230 bird species have been recorded on site including black-faced bunting, nightingale, marsh harrier, spoonbill and Leach's storm-petrel. Additionally, a wide variety of butterflies, dragonflies and damselflies can be spotted in the area. Facilities Facilities include a small information centre, a nine-hole municipal golf course, a car park, a children's play area, toile ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glaze Brook
The Glaze Brook, or River Glaze, is a minor river in the River Mersey catchment area, England. From Hope Carr (just inside Leigh) to the River Mersey it forms the county boundary with Cheshire. It is about long and its main tributaries are the Astley, Bedford, Hey, Pennington, Shaw and Westleigh Brooks. Pennington Brook starts at the outflow of Pennington Flash close to Aspull Common. Pennington Flash is fed by Hey Brook, a continuation of Borsdane Brook, which runs southwards from Blackrod. Glaze Brook originates at the confluence of Pennington Brook and Moss Brook, approximately 120 m north of Hawkhurst Bridge. After picking up the waters of Bedford Brook, which runs southward from Leigh and the Black or Moss Brook coming west from Worsley via Chat Moss, the brook turns southward, ultimately draining into the River Mersey section of the Manchester Ship Canal near Cadishead. The Glaze Brook's catchment drains the flat lowland around Leigh which reaches a maximum altitude of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sprotbrough Flash
Sprotbrough Flash is a nature reserve south of Sprotbrough near Doncaster, South Yorkshire, on the north bank of the River Don. It is named after its main feature, a long, water-filled depression parallel to the river. The reserve is managed by the Yorkshire Wildlife Trust. It overlaps with Sprotbrough Gorge, a Site of Special Scientific Interest. The size of the protected area is 28 hectares (0.28 square kilometers). The Trans Pennine Trail passes through the area. History Two hundred and eighty million years ago, during the Permian period, dolomite (magnesium limestone) formed here. This has been mined since the mid-19th century. Mining has since stopped and wildlife has returned to this area. The original quarry can still be seen opposite the River Don, adjacent to the Sprotbrough Flash lake. Worthy of note, the woolly rhinoceros lived in this area in the Pleistocene. Bones from this creature have been discovered here. The long lake from which the name of the reserve ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandbach Flashes
Sandbach Flashes () are a group of 14 wetlands west of Sandbach in Cheshire, England. The flashes were designated as a Site of Special Scientific Interest in 1963, with a total area of 1.53 km2. There are a number of individual flashes including Bottom's Flash, Crabmill Flash, Elton Hall Flash, Fodens Flash, Groby's Flash, Ilse Pool, Moston Flashes, Pump House Flash, Railway Flash, Red Lane Tip and Pool, and Watch Lane Flash. Part of the site is managed by the Sandbach Flashes Joint Management Committee. Description of site Sandbach Flashes consists of a number of pools formed as a result of subsidence due to the solution of underlying salt deposits. The water varies from freshwater, chemically similar to other Cheshire meres, to highly saline. Most of the flashes are surrounded by semi-improved or improved grassland. Fodens Flash is partly surrounded by wet woodland. Biodiversity Inland saline habitats such as those present at Sandbach Flashes are extremely ra ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North Yorkshire
North Yorkshire is the largest ceremonial county (lieutenancy area) in England, covering an area of . Around 40% of the county is covered by national parks, including most of the Yorkshire Dales and the North York Moors. It is one of four counties in England to hold the name Yorkshire; the three other counties are the East Riding of Yorkshire, South Yorkshire and West Yorkshire. North Yorkshire may also refer to a non-metropolitan county, which covers most of the ceremonial county's area () and population (a mid-2016 estimate by the ONS of 602,300), and is administered by North Yorkshire County Council. The non-metropolitan county does not include four areas of the ceremonial county: the City of York, Middlesbrough, Redcar and Cleveland and the southern part of the Borough of Stockton-on-Tees, which are all administered by unitary authorities. The non-metropolitan county and the City of York are within the Yorkshire and the Humber region. Middlesbrough, Redcar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hellifield
Hellifield is a village and civil parish in the Craven district of North Yorkshire, England (). Historically part of the West Riding of Yorkshire, the village was once an important railway junction on the Settle-Carlisle Railway between the Midland Railway and the Lancashire and Yorkshire Railway, but Hellifield railway station is now a shadow of its former glory. It is situated on the A65, between Skipton and Settle. Hellifield had a population of 1,060 residents at the 2001 census, increasing to 1,426 at the 2011 census. History In the Domesday Book of 1086, Hellifield is mentioned as Helgeflet; meaning 'Holy Marsh or Stream', translated from Anglo-Saxon, the village also could have been dedicated to the Anglo-Saxon Goddess ' Hel'. There is also the possibility that the name derives from the Norse 'The Farm of Helgi'. The village name changed over the years; in the 12th century, Hellifield was referred to as "Nether Hellifield" and in the 17th and 18th centuries the v ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Rother, South Yorkshire
The River Rother, a waterway in the northern midlands of England, gives its name to the town of Rotherham and to the Rother Valley parliamentary constituency. It rises near Clay Cross in Derbyshire and flows in a generally northwards direction through the centre of Chesterfield, where it feeds the Chesterfield Canal, and on through the Rother Valley Country Park and several districts of Sheffield before joining the River Don at Rotherham in Yorkshire. Historically, it powered mills, mainly corn or flour mills, but most had ceased to operate by the early 20th century, and few of the mill buildings survive. From the 1880s, the water quality deteriorated rapidly, as a result of coal mining and its associated communities. The river became unable to sustain life, and by 1974, was the most polluted of the rivers within the River Don catchment. The pollutants came from coking plants, from inefficient sewage treatment plants, and from the manufacture of chemicals. Major investm ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Catcliffe
Catcliffe is a village and civil parish on the north-west bank of the River Rother in South Yorkshire, England. The population of the civil parish at the 2011 census was 2,108. It is in the Metropolitan Borough of Rotherham, approximately south of the town of Rotherham and east of Sheffield City Centre. History Catcliffe is mentioned in the ''Domesday book'', its name is presumed to mean either ''the cliff where the cats live'', or ''steep river bank''. In 1740 William Fenney established a glassworks here. The site was chosen, among other reasons, for being away from Fenney's glassworks in Bolsterstone, formerly owned by his mother-in-law—the terms of her will prevented him from setting up a glassworks within 10 miles of the town. One of the cones of this glassworks still exists and is the oldest surviving structure of its type in Western Europe. It is a Grade I listed building and a Scheduled Ancient Monument. On 25 June 2007 the village was evacuated because of fears ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Aire
The River Aire is a major river in Yorkshire, England, in length. The ''Handbook for Leeds and Airedale'' (1890) notes that the distance from Malham to Howden is direct, but the river's meanderings extend that to . Between Malham Tarn and Airmyn, the river drops . Part of the river below Leeds is canalised, and is known as the Aire and Calder Navigation. Course The Aire starts at Malham Tarn and becomes a subterranean stream at 'Water Sinks' about one mile (1.6 km) before the top of Malham Cove, it then flows underground to Aire Head, just below Malham, in North Yorkshire, and then flows through Gargrave and Skipton. After Cononley, the river enters West Yorkshire where it passes through the former industrial areas of Keighley, Bingley, Saltaire and Shipley. It then passes through Leeds and on to Swillington and Woodlesford. At Castleford is the confluence of the Aire and Calder; just downstream of the confluence was the ford where the ancient British r ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fairburn Ings
Fairburn Ings Nature Reserve is a protected area in West Yorkshire, England, noted for its avian biodiversity. The reserve has recorded around 280 bird species, remarkable for an inland site in the United Kingdom. This is explained by the site being on migration routes as well as the diversity of habitats. History It was designated a local nature reserve in 1957 under the National Parks and Access to the Countryside Act (1949). Since the late 1970s it has been managed by the Royal Society for the Protection of Birds on behalf of the local naturalists who set it up. Geography The reserve is in the Lower Aire Valley, south and west of Fairburn, near Castleford. It includes the whole of Fairburn & Newton Ings SSSI. It is also a Statutory Bird Sanctuary (one of only 10 in England) with a focus mainly on wildfowl and waders, although many other birds can be seen. The word ''ings'' (singular ''ing'') is of Old Norse origin and means "damp or marshy land that floods", a reference ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Don, Yorkshire
The River Don (also called River Dun in some stretches) is a river in South Yorkshire and the East Riding of Yorkshire, England. It rises in the Pennines, west of Dunford Bridge, and flows for eastwards, through the Don Valley, via Penistone, Sheffield, Rotherham, Mexborough, Conisbrough, Doncaster and Stainforth. It originally joined the Trent, but was re-engineered by Cornelius Vermuyden as the ''Dutch River'' in the 1620s, and now joins the River Ouse at Goole. Don Valley is a UK parliamentary constituency near the Doncaster stretch of the river. Etymology The probable origin of the name was Brittonic ''Dānā'', from a root ''dān-'', meaning "water" or "river". The name Dôn (or Danu), a Celtic mother goddess, has the same origin. The river gave its name to the Don River, one of the principal rivers of Toronto, Canada. Geography The Don can be divided into sections by the different types of structures built to restrict its passage. The upper reaches, and th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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