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List Of Sites Of Special Scientific Interest In South Yorkshire
This is a list of Sites of Special Scientific Interest (SSSIs) in South Yorkshire, United Kingdom. , There are 35 sites designated within this Area of Search, of which 18 have been designated due to their biological interest, 14 due to its geological interest, and 3 for both biological and geological interest. In England the body responsible for designating SSSIs is Natural England, which chooses a site because of its fauna, flora, geological or physiographical features. Natural England took over the role of designating and managing SSSIs from English Nature in October 2006 when it was formed from the amalgamation of English Nature, parts of the Countryside Agency and the Rural Development Service. Natural England, like its predecessor, uses the 1974–1996 county system and as such the same approach is followed here, rather than, for example, merging all Yorkshire sites into a single list. Natural England produces citation sheets for each SSSI and are the main source of informat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
South Yorkshire Outline Map With UK
South is one of the cardinal directions or compass points. The direction is the opposite of north and is perpendicular to both east and west. Etymology The word ''south'' comes from Old English ''sūþ'', from earlier Proto-Germanic ''*sunþaz'' ("south"), possibly related to the same Proto-Indo-European root that the word ''sun'' derived from. Some languages describe south in the same way, from the fact that it is the direction of the sun at noon (in the Northern Hemisphere), like Latin meridies 'noon, south' (from medius 'middle' + dies 'day', cf English meridional), while others describe south as the right-hand side of the rising sun, like Biblical Hebrew תֵּימָן teiman 'south' from יָמִין yamin 'right', Aramaic תַּימנַא taymna from יָמִין yamin 'right' and Syriac ܬܰܝܡܢܳܐ taymna from ܝܰܡܝܺܢܳܐ yamina (hence the name of Yemen, the land to the south/right of the Levant). Navigation By convention, the ''bottom or down-facing side'' of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Plateau
In geology and physical geography, a plateau (; ; ), also called a high plain or a tableland, is an area of a highland consisting of flat terrain that is raised sharply above the surrounding area on at least one side. Often one or more sides have deep hills or escarpments. Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, and erosion by water and glaciers. Plateaus are classified according to their surrounding environment as intermontane, piedmont, or continental. A few plateaus may have a small flat top while others have wide ones. Formation Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, Plate tectonics movements and erosion by water and glaciers. Volcanic Volcanic plateaus are produced by volcanic activity. The Columbia Plateau in the north-western United States is an example. They may be formed by upwelling of volcanic magma or extrusion of lava. The un ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eastern Peak District Moors
The Peak District is an upland area in England at the southern end of the Pennines. Mostly in Derbyshire, 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 visitors – some 20 million live within an hour's ride. Inhabited from the Mesolithic era, it shows evidence of the Neolithic, Bronze and Iron Ages. Settled by the Romans and Anglo-Saxons, it remained largely agricultural; mining arose in the Middle Ages. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Denaby Ings
Denaby Ings are a nature reserve on the River Dearne, encompassing an area of 23 hectares north of Denaby Main, Doncaster, South Yorkshire, near the town of Mexborough. The Trans Pennine Trail passes here. The habitats include open water, water meadows, woodland scrub and hedgerows. Birdwatching Birdwatching, or birding, is the observing of birds, either as a recreational activity or as a form of citizen science. A birdwatcher may observe by using their naked eye, by using a visual enhancement device like binoculars or a telescope, by ... is a popular activity there. The area has been classed as a Site of Special Scientific Interest since 11 August 1983.{{cite web, url=https://designatedsites.naturalengland.org.uk/SiteDetail.aspx?SiteCode=S1004401&SiteName=denaby%20ings&countyCode=&responsiblePerson=&SeaArea=&IFCAArea=, title=Denaby Ings SSSI, publisher=Natural England, accessdate=30 July 2018 References Geography of Doncaster Nature reserves in South Yorkshire Sites of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carlton Main Brickworks
Carlton Main Brickworks () is a 15.5 hectare (38.4 acre) geological site of Special Scientific Interest in South Yorkshire. It opened alongside Grimethorpe colliery in the mid-1890s, and has been producing quality bricks for well over a century. The site was notified in 1989. See also * List of Sites of Special Scientific Interest in South Yorkshire References Carlton Main Brickworks''Natural England Natural England is a non-departmental public body in the United Kingdom sponsored by the Department for Environment, Food and Rural Affairs. It is responsible for ensuring that England's natural environment, including its land, flora and fauna, ...''. Retrieved on 2009-02-12 {{DEFAULTSORT:Carlton Main Brickworks Sites of Special Scientific Interest notified in 1989 Sites of Special Scientific Interest in South Yorkshire Brickworks in the United Kingdom Brierley ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canyards Hills
Canyards Hills () is a 64.1 hectare (158.4 acre) biological and geological site of Special Scientific Interest in South Yorkshire. The site was notified in 1990. This site possesses the most impressive examples in England and Wales of 'ridge-and-trough' or 'tumbled ground.' Beneath a 10 m high cliff, the north-facing valley side above Broomhead Reservoir and the hamlet of Wigtwizzle is a chaotic mass of sub-parallel ridges, separated by intervening narrow areas of marshy ground. The site is formed in Upper Carboniferous Millstone Grit and shows the most extreme form and best example of 'tumbled ground', with innumerable small Millstone Grit blocks (controlled by jointing) taking up a large landslip. See also *List of Sites of Special Scientific Interest in South Yorkshire References Canyards Hills''Natural England Natural England is a non-departmental public body in the United Kingdom sponsored by the Department for Environment, Food and Rural Affairs. It is responsible f ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cadeby Quarry
Cadeby is a village and civil parish in the Metropolitan Borough of Doncaster in South Yorkshire, England. The population at the census of 2011 was 203. It is about five miles west of Doncaster, and four miles east of Mexborough. History The manor of Cadeby was held in medieval times by the Norman baronial Fitzwilliam family, and later by their descendants, the Copley baronets. Later, it was inherited by barrister Thomas Levett, a native of High Melton, who sold to his brother, York barrister John Levett, who in turn sold it to Edmund Hastings, Esq., of Plumtree, Nottinghamshire. Cadeby Quarry Close to the village is Cadeby Quarry, a site of special scientific interest, which was notified in 1977 for its geological interest. The site covers 240 acres (97 hectares) of the old quarry. '' |
Bradgate Brickworks
Bradgate Brickworks () is a 0.9 hectare (2.2 acre) geological site of Special Scientific Interest in South Yorkshire. The site was notified in 1988. In November 2001 a report by Rotherham Borough Council Rotherham Metropolitan Borough Council is the local authority of the Metropolitan Borough of Rotherham in South Yorkshire, England. It is a metropolitan district council, one of four in South Yorkshire and one of 36 in the metropolitan countie ... noted concern that overgrown vegetation at the site presented a risk to the geological features of the quarry face and proposed the acquisition and management of the site by the Council. See also * List of Sites of Special Scientific Interest in South Yorkshire References {{DEFAULTSORT:Bradgate Brickworks Sites of Special Scientific Interest notified in 1988 Sites of Special Scientific Interest in South Yorkshire Brickworks in the United Kingdom ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bilham Sand Pits
Bilham Sand Pits () is a 0.2 hectare (0.1 acre) geological site of Special Scientific Interest in South Yorkshire. The site was notified in 1987. See also * List of Sites of Special Scientific Interest in South Yorkshire References Bilham Sand Pits''Natural England Natural England is a non-departmental public body in the United Kingdom sponsored by the Department for Environment, Food and Rural Affairs. It is responsible for ensuring that England's natural environment, including its land, flora and fauna, ...''. Retrieved on 2009-02-12 {{DEFAULTSORT:Bilham Sand Pits Sites of Special Scientific Interest notified in 1987 Sites of Special Scientific Interest in South Yorkshire South Yorkshire ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ashfield Brick Pits
Ashfield Brick Pits () is a 0.6 hectare (1.4 acre) geological site of Special Scientific Interest south of Conisbrough in South Yorkshire. The site was notified in 1955. See also * List of Sites of Special Scientific Interest in South Yorkshire References Ashfield Brick Pits''Natural England Natural England is a non-departmental public body in the United Kingdom sponsored by the Department for Environment, Food and Rural Affairs. It is responsible for ensuring that England's natural environment, including its land, flora and fauna, ...''. Retrieved on 2009-02-12 {{DEFAULTSORT:Ashfield Brick Pits Sites of Special Scientific Interest notified in 1955 Sites of Special Scientific Interest in South Yorkshire ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anston Stones Wood
Anston Stones Wood () is a 33.7 hectare (88.3 acre) biological site of Special Scientific Interest in South Yorkshire. The site was notified in 1955. The site contains the second best example of limestone 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 (se ... in South Yorkshire. It is also a Local Nature Reserve. See also * List of Sites of Special Scientific Interest in South Yorkshire References {{DEFAULTSORT:Anston Stones Wood Sites of Special Scientific Interest notified in 1955 Sites of Special Scientific Interest in South Yorkshire Local Nature Reserves in South Yorkshire ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Peatland
A mire, peatland, or quagmire is a wetland area dominated by living peat-forming plants. Mires arise because of incomplete decomposition of organic matter, usually litter from vegetation, due to water-logging and subsequent anoxia. All types of mires share the common characteristic of being saturated with water, at least seasonally with actively forming peat, while having their own ecosystem. Like coral reefs, mires are unusual landforms that derive mostly from biological rather than physical processes, and can take on characteristic shapes and surface patterning. A quagmire is a floating (quaking) mire, bog, or any peatland being in a stage of hydrosere or hydrarch (hydroseral) succession, resulting in pond-filling yields underfoot. Ombrotrophic types of quagmire may be called quaking bog (quivering bog). Minerotrophic types can be named with the term quagfen. There are four types of mire: bog, fen, marsh and swamp. A bog is a mire that, due to its location relative to the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
