List Of Sites Of Special Scientific Interest In Oxfordshire
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List Of Sites Of Special Scientific Interest In Oxfordshire
Oxfordshire in South East England has an area of 2,605 square kilometres and a population of 648,700. In England, the body responsible for designating Sites of Special Scientific Interest (SSSIs) is Natural England, which is responsible for protecting England's natural environment. Notification as an SSSI gives legal protection to the best sites for wildlife and geology. As of 2020, there are 111 SSSIs in Oxfordshire, 78 of which have been designated for biological interest, 27 for geological interest, and 6 for both biological and geological interest. Key Interest *B = site of biological interest *G = site of geological interest Public access *FP = access to footpaths through the site only *No = no public access to site *PP = public access to part of site *Yes = public access to all or most of the site Other designations and wildlife trust management *BBOWT = Berkshire, Buckinghamshire and Oxfordshire Wildlife Trust *GCR = Geological Conservation Review site *LNR = Loca ...
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Oxfordshire
Oxfordshire is a ceremonial and non-metropolitan county in the north west of South East England. It is a mainly rural county, with its largest settlement being the city of Oxford. The county is a centre of research and development, primarily due to the work of the University of Oxford and several notable science parks. These include the Harwell Science and Innovation Campus and Milton Park, both situated around the towns of Didcot and Abingdon-on-Thames. It is a landlocked county, bordered by six counties: Berkshire to the south, Buckinghamshire to the east, Wiltshire to the south west, Gloucestershire to the west, Warwickshire to the north west, and Northamptonshire to the north east. Oxfordshire is locally governed by Oxfordshire County Council, together with local councils of its five non-metropolitan districts: City of Oxford, Cherwell, South Oxfordshire, Vale of White Horse, and West Oxfordshire. Present-day Oxfordshire spanning the area south of the Thames was h ...
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Appleton, Oxfordshire
Appleton is a village in the civil parish of Appleton-with-Eaton, about northwest of Abingdon. Historically in Berkshire, the 1974 boundary changes transferred it to Oxfordshire for administrative purposes. The 2011 Census recorded Appleton-with-Eaton's parish population as 915. Manor In the 9th century Abingdon Abbey held the manor of Appleton. In 871 the Danes sacked the abbey and thereby obtained Appleton, but it is assumed that Appleton was recovered by Alfred the Great. Appleton's toponym means simply "an orchard". In the 10th century it was ''Æppeltune'' or ''Appeltun'', from then until the 17th century it evolved as ''Apletone'', ''Apletune'' and ''Appelton'', and in 1316 it was recorded as ''Aspelton''. In the 10th century the village had the alternative name of ''Earmundeslæh'', ''Earmundesleah'', ''Earmundeslee'' or ''Earmundeslei'', referring to King Edmund I, who in 942 granted it to Athelstan, one of his thegns, who may have restored it to Abingdon Abbey. ...
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Middle Jurassic
The Middle Jurassic is the second epoch of the Jurassic Period. It lasted from about 174.1 to 163.5 million years ago. Fossils of land-dwelling animals, such as dinosaurs, from the Middle Jurassic are relatively rare, but geological formations containing land animal fossils include the Forest Marble Formation in England, the Kilmaluag Formation in Scotland,British Geological Survey. 2011Stratigraphic framework for the Middle Jurassic strata of Great Britain and the adjoining continental shelf: research report RR/11/06 British Geological Survey, Keyworth, Nottingham. the Daohugou Beds in China, the Itat Formation in Russia, and the Isalo III Formation of western Madagascar. Paleogeography During the Middle Jurassic Epoch, Pangaea began to separate into Laurasia and Gondwana, and the Atlantic Ocean formed. Eastern Laurasia was tectonically active as the Cimmerian plate continued to collide with Laurasia's southern coast, completely closing the Paleo-Tethys Ocean. A subduction zone ...
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Bathonian
In the geologic timescale the Bathonian is an age and stage of the Middle Jurassic. It lasted from approximately 168.3 Ma to around 166.1 Ma (million years ago). The Bathonian Age succeeds the Bajocian Age and precedes the Callovian Age. Stratigraphic definitions The Bathonian Stage takes its name from Bath, a spa town in England built on Jurassic limestone (the Latinized form of the town name is ''Bathonium''). The name was introduced in scientific literature by Belgian geologist d'Omalius d'Halloy in 1843. The original type locality was located near Bath. The French palaeontologist Alcide d'Orbigny was in 1852 the first to define the exact length of the stage. The base of the Bathonian is at the first appearance of ammonite species '' Parkinsonia (Gonolkites) convergens'' in the stratigraphic column. The global reference profile for the base of the Bathonian (a GSSP) was ratified as Ravin du Bès, Bas-Auran area, Alpes de Haute Provence, France in 2009. The top of the Bat ...
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BBOWT
The Berkshire, Buckinghamshire and Oxfordshire Wildlife Trust (BBOWT), is a The Wildlife Trusts partnership, wildlife trust covering the counties of Berkshire, Buckinghamshire and Oxfordshire in England. The trust was formerly called the Berkshire, Buckinghamshire and Oxfordshire Naturalists' Trust (BBONT). __TOC__ Sites Berkshire Buckinghamshire Oxfordshire Notes References External links Berkshire, Buckinghamshire and Oxfordshire Wildlife Trust website
{{DEFAULTSORT:Berkshire, Buckinghamshire And Oxfordshire Wildlife Trust Berkshire, Buckinghamshire and Oxfordshire Wildlife Trust, Wildlife Trusts of England ...
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Ardley, Oxfordshire
Ardley is a village and civil parish in Oxfordshire, England, about northwest of Bicester. The parish includes the village of Fewcott, which is now contiguous with Ardley. The 2011 Census recorded the population of Ardley parish as 751. Geography and natural history The two villages of Ardley and Fewcott are on either side of a stream that rises at Fritwell, flows south to Ardley, then turns east through Stoke Lyne to Fringford. There it joins Crowell Brook, which continues east into Buckinghamshire and ultimately becomes part of the Great Ouse. The limestone quarry at Ardley has yielded a significant find of dinosaur tracks (ichnites), discovered in 1997 and thought to have been left by Megalosaurus and possibly Cetiosaurus. Some of these are on display in the dinosaur garden at the Oxfordshire Museum in Woodstock, Oxfordshire. There is a site of special scientific interest in the village with a colony of the great crested newts and an outcrop of Jurassic limestone. Cas ...
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Railway Cutting, Close To Ardley Nature Reserve - Geograph
Rail transport (also known as train transport) is a means of transport that transfers passengers and goods on wheeled vehicles running on rails, which are incorporated in tracks. In contrast to road transport, where the vehicles run on a prepared flat surface, rail vehicles (rolling stock) are directionally guided by the tracks on which they run. Tracks usually consist of steel rails, installed on sleepers (ties) set in ballast, on which the rolling stock, usually fitted with metal wheels, moves. Other variations are also possible, such as "slab track", in which the rails are fastened to a concrete foundation resting on a prepared subsurface. Rolling stock in a rail transport system generally encounters lower frictional resistance than rubber-tyred road vehicles, so passenger and freight cars (carriages and wagons) can be coupled into longer trains. The operation is carried out by a railway company, providing transport between train stations or freight customer faciliti ...
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