|
West Heath, Cheshire
West Heath is a suburb to the west of Congleton, in Cheshire, England. It is the site of Astbury Mere Country Park. The West Heath area has three schools, with one of Congleton's two secondary schools, Congleton High School being located there. Geography and environment Congleton lies at a zone of transition between the Cheshire Plain and Peak District ( Pennines, Pennine) Mountains. West Heath lies on the Cheshire plain and consists of rolling farmland, suburbs and small woodlands. The flora of the area is typical of the Cheshire Plain, but is well wooded and with small areas of Heath (habitat), heathlands still surviving in isolated pockets, mainly around Astbury Mere and out towards Somerford. History West Heath was formerly an area of large heathland and woodland. It had an opencast sand quarry, now a lake known as Astbury Mere. Many of the houses and layout were built after the 1960s to the present, although older buildings pocket the area. Astbury Mere Astbury Mere is a l ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Congleton
Congleton is a town and civil parish in the unitary authority of Cheshire East in Cheshire, England. The town is by the River Dane, south of Manchester and north of Stoke on Trent. At the 2011 Census, it had a population of 26,482. Toponymy The town's name is of unknown origin. The first recorded reference to it was in 1282, when it was spelt ''Congelton''. The element ''Congle'' might relate to the old Norse ''kang'' meaning a bend, followed by the Old English element ''tun'' meaning settlement. History The first settlements in the Congleton area were Neolithic. Stone Age and Bronze Age artefacts have been found in the town. Congleton was once thought to have been a Roman settlement, although there is no archaeological or documentary evidence to support this. Congleton became a market town after Vikings destroyed nearby Davenport. Godwin, Earl of Wessex held the town in the Saxon period. The town is mentioned in the Domesday Book, where it is listed as ''Cogeltone: ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cheshire
Cheshire ( ) is a ceremonial and historic county in North West England, bordered by Wales to the west, Merseyside and Greater Manchester to the north, Derbyshire to the east, and Staffordshire and Shropshire to the south. Cheshire's county town is the cathedral city of Chester, while its largest town by population is Warrington. Other towns in the county include Alsager, Congleton, Crewe, Ellesmere Port, Frodsham, Knutsford, Macclesfield, Middlewich, Nantwich, Neston, Northwich, Poynton, Runcorn, Sandbach, Widnes, Wilmslow, and Winsford. Cheshire is split into the administrative districts of Cheshire West and Chester, Cheshire East, Halton, and Warrington. The county covers and has a population of around 1.1 million as of 2021. It is mostly rural, with a number of towns and villages supporting the agricultural and chemical industries; it is primarily known for producing chemicals, Cheshire cheese, salt, and silk. It has also had an impact on popular culture, producin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Astbury Mere
Astbury Mere is a lake and open area in West Heath, a suburb of Congleton, Cheshire, England, in an area formerly quarried for silica sand. Part of the area is accredited by Natural England as a country park, Astbury Mere Country Park. The country park has an area of and the lake covers . The park is owned by Astbury Mere Trust, and the lake and its banks by Stoke-on-Trent Angling Society. History Extraction of silica sand occurred at the Congleton West Heath quarry from around the 1930s until 1984. The sand was used for making glass and for precision casting of metal. After the closure of the quarry, the site was divided into housing (Ennerdale Drive estate) and open space. A trust was established in 1989 to manage the open land. The park first opened to the public in 1991. In 2002, the Stoke-on-Trent Angling Society acquired the lake. By 2008 the Astbury Mere Trust had acquired the majority of the land. The park was accredited by Natural England as a country park in 2012. L ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Congleton High School
Congleton High School (CHS) is an 11–18 mixed secondary school and sixth form with academy status in Congleton, Cheshire, England. It has a specialism in engineering. History The school was formed after the reduction of the area's three schools to two larger schools (the previous schools being Dane Valley High School, Heathfield High School and Westlands High School). In 2022 Congleton High School applied for planning permission to expand, the planned expansion will add new classroom faculties and provide and a new dinning area for staff and students among other additions. See also *Eaton Bank Academy Eaton Bank Academy (formerly Eaton Bank School) is a co-educational secondary school with academy status located in the town of Congleton in Cheshire, England England is a country that is part of the United Kingdom. It shares land ... References External links * Academies in the Borough of Cheshire East Secondary schools in the Borough ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cheshire Plain
The Cheshire Plain is a relatively flat expanse of lowland within the county of Cheshire in North West England but extending south into Shropshire. It extends from the Mersey Valley in the north to the Shropshire Hills in the south, bounded by the hills of North Wales to the west and the foothills of the Pennines to the north-east. The Wirral Peninsula lies to the north-west whilst the plain merges with the South Lancashire Plain in the embayment occupied by Manchester to the north. In detail, the plain comprises two areas with distinct characters, the one to the west of the Mid Cheshire Ridge and the other, larger part, to its east. The plain is the surface expression of the Cheshire Basin, a deep sedimentary basin that extends north into Lancashire and south into Shropshire. It assumed its current form as the ice-sheets of the last glacial period melted away between 20,000 and 15,000 years ago leaving behind a thick cover of glacial till and extensive tracts of glacio-flu ... [...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] |
Pennines
The Pennines (), also known as the Pennine Chain or Pennine Hills, are a range of uplands running between three regions of Northern England: North West England on the west, North East England and Yorkshire and the Humber on the east. Commonly described as the "backbone of England", the range stretches northwards from the Peak District at the southern end, through the South Pennines, Yorkshire Dales and North Pennines to the Tyne Gap, which separates the range from the Border Moors and Cheviot Hills across the Anglo-Scottish border, although some definitions include them. South of the Aire Gap is a western spur into east Lancashire, comprising the Rossendale Fells, West Pennine Moors and the Bowland Fells in North Lancashire. The Howgill Fells and Orton Fells in Cumbria are sometimes considered to be Pennine spurs to the west of the range. The Pennines are an important water catchment area with numerous reservoirs in the head streams of the river valleys. The North Pennin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Heath (habitat)
A heath () is a shrubland habitat found mainly on free-draining infertile, acidic soils and characterised by open, low-growing woody vegetation. Moorland is generally related to high-ground heaths with—especially in Great Britain—a cooler and damper climate. Heaths are widespread worldwide but are fast disappearing and considered a rare habitat in Europe. They form extensive and highly diverse communities across Australia in humid and sub-humid areas where fire regimes with recurring burning are required for the maintenance of the heathlands.Specht, R.L. 'Heathlands' in 'Australian Vegetation' R.H. Groves ed. Cambridge University Press 1988 Even more diverse though less widespread heath communities occur in Southern Africa. Extensive heath communities can also be found in the Texas chaparral, New Caledonia, central Chile, and along the shores of the Mediterranean Sea. In addition to these extensive heath areas, the vegetation type is also found in scattered locations ac ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Heathland
A heath () is a shrubland habitat found mainly on free-draining infertile, acidic soils and characterised by open, low-growing woody vegetation. Moorland is generally related to high-ground heaths with—especially in Great Britain—a cooler and damper climate. Heaths are widespread worldwide but are fast disappearing and considered a rare habitat in Europe. They form extensive and highly diverse communities across Australia in humid and sub-humid areas where fire regimes with recurring burning are required for the maintenance of the heathlands.Specht, R.L. 'Heathlands' in 'Australian Vegetation' R.H. Groves ed. Cambridge University Press 1988 Even more diverse though less widespread heath communities occur in Southern Africa. Extensive heath communities can also be found in the Texas chaparral, New Caledonia, central Chile, and along the shores of the Mediterranean Sea. In addition to these extensive heath areas, the vegetation type is also found in scattered locations acro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Woodland
A woodland () is, in the broad sense, land covered with trees, or in a narrow sense, synonymous with wood (or in the U.S., the ''plurale tantum'' woods), a low-density forest forming open habitats with plenty of sunlight and limited shade (see differences between British, American, and Australian English explained below). Woodlands may support an understory of shrubs and herbaceous plants including grasses. Woodland may form a transition to shrubland under drier conditions or during early stages of primary or secondary succession. Higher-density areas of trees with a largely closed canopy that provides extensive and nearly continuous shade are often referred to as forests. Extensive efforts by conservationist groups have been made to preserve woodlands from urbanization and agriculture. For example, the woodlands of Northwest Indiana have been preserved as part of the Indiana Dunes. Definitions United Kingdom ''Woodland'' is used in British woodland management to mean tre ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quarry
A quarry is a type of open-pit mine in which dimension stone, rock, construction aggregate, riprap, sand, gravel, or slate is excavated from the ground. The operation of quarries is regulated in some jurisdictions to reduce their environmental impact. The word ''quarry'' can also include the underground quarrying for stone, such as Bath stone. Types of rock Types of rock extracted from quarries include: *Chalk *China clay *Cinder *Clay *Coal * Construction aggregate (sand and gravel) * Coquina * Diabase *Gabbro *Granite * Gritstone *Gypsum *Limestone *Marble *Ores *Phosphate rock *Quartz *Sandstone * Slate *Travertine Stone quarry Stone quarry is an outdated term for mining construction rocks (limestone, marble, granite, sandstone, etc.). There are open types (called quarries, or open-pit mines) and closed types ( mines and caves). For thousands of years, only hand tools had been used in quarries. In the 18th century, the use of drilling and blasting operatio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake
A lake is an area filled with water, localized in a basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are not part of the ocean, although, like the much larger oceans, they do form part of the Earth's water cycle. Lakes are distinct from lagoons, which are generally coastal parts of the ocean. Lakes are typically larger and deeper than ponds, which also lie on land, though there are no official or scientific definitions. Lakes can be contrasted with rivers or streams, which usually flow in a channel on land. Most lakes are fed and drained by rivers and streams. Natural lakes are generally found in mountainous areas, rift zones, and areas with ongoing glaciation. Other lakes are found in endorheic basins or along the courses of mature rivers, where a river channel has widened into a basin. Some parts of the world have many lakes formed by the chaotic drainage patterns left over from the la ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
_in_1902.png "Click for more on -> Congleton")
.jpeg/1200px-Amrum_(187753235).jpeg "Click for more on -> Heath (habitat)")
