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Rogerley Quarry
Rogerley Quarry is a Site of Special Scientific Interest in the Wear Valley district of west County Durham, England. It lies on the edge of the valley of the River Wear, alongside the A689 road, about 1 km upriver from the village of Frosterley. The site is a disused quarry and has been designated as of national importance in the Geological Conservation Review as a key site for sedimentological studies. The quarry exhibits a long section of basal Namurian sandstones which derive from riverine sedimentation Sedimentation is the deposition of sediments. It takes place when particles in suspension settle out of the fluid in which they are entrained and come to rest against a barrier. This is due to their motion through the fluid in response to the .... The quarry face intersects the ancient river channel at right angles, allowing the lateral changes in deposition across the channel to be clearly seen. References Sites of Special Scientific Interest in County Dur ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stanhope, County Durham
Stanhope is a market town and civil parish in the County Durham district, in the ceremonial county of Durham, England. It lies on the River Wear between Eastgate and Frosterley, in the north-east of Weardale. The main A689 road over the Pennines is crossed by the B6278 between Barnard Castle and Shotley Bridge. In 2001 Stanhope had a population of 1,633, in 2019 an estimate of 1,627, and a figure of 1,602 in the 2011 census for the ONS built-up-area which includes Crawleyside. In 2011 the parish population was 4,581. Civil parish The civil parish includes the settlements of Cornriggs, Cowshill, Daddry Shield, Eastgate, Frosterley, Ireshopeburn, Lanehead, St John's Chapel, Wearhead and Westgate, all on the A689 road, and also Bollihope, Bridge End, Brotherlee, Copthill, Crawleyside, East Blackdene, Hill End, Lintzgarth, New House, Rookhope and West Blackdene. Other places it includes are Killhope, Shittlehope, Unthank and White Kirkley. This gives it the lar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Site Of Special Scientific Interest
A Site of Special Scientific Interest (SSSI) in Great Britain or an Area of Special Scientific Interest (ASSI) in the Isle of Man and Northern Ireland is a conservation designation denoting a protected area in the United Kingdom and Isle of Man. SSSI/ASSIs are the basic building block of site-based nature conservation legislation and most other legal nature/geological conservation designations in the United Kingdom are based upon them, including national nature reserves, Ramsar sites, Special Protection Areas, and Special Areas of Conservation. The acronym "SSSI" is often pronounced "triple-S I". Selection and conservation Sites notified for their biological interest are known as Biological SSSIs (or ASSIs), and those notified for geological or physiographic interest are Geological SSSIs (or ASSIs). Sites may be divided into management units, with some areas including units that are noted for both biological and geological interest. Biological Biological SSSI/ASSIs may ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wear Valley
Wear Valley was, from 1974 to 2009, a local government district in County Durham, England. Its council and district capital was Crook. The district covered much of the Weardale area. In the west it was parished and rural, whereas in the east it was more urban. Crook and Willington are unparished. The district was formed on 1 April 1974, under the Local Government Act 1972, by the merger of the Bishop Auckland, Crook and Willington and Tow Law urban districts, along with Weardale Rural District. The district was abolished as part of the 2009 structural changes to local government in England, becoming part of the Durham County Council Durham County Council is a local authority administering all significant local government functions in the unitary authority area of County Durham in North East England. The council area covers part of the ceremonial county of County Durham, e ... unitary authority. Wear Valley had a population of around 65,000 in 2001. Electoral divis ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
County Durham
County Durham ( ), officially simply Durham,UK General Acts 1997 c. 23Lieutenancies Act 1997 Schedule 1(3). From legislation.gov.uk, retrieved 6 April 2022. is a ceremonial county in North East England.North East Assembly â€About North East England. Retrieved 30 November 2007. The ceremonial county spawned from the historic County Palatine of Durham in 1853. In 1996, the county gained part of the abolished ceremonial county of Cleveland.Lieutenancies Act 1997 . Retrieved 27 October 2014. The county town is the of |
England
England is a country that is part of the United Kingdom. It shares land borders with Wales to its west and Scotland to its north. The Irish Sea lies northwest and the Celtic Sea to the southwest. It is separated from continental Europe by the North Sea to the east and the English Channel to the south. The country covers five-eighths of the island of Great Britain, which lies in the North Atlantic, and includes over 100 smaller islands, such as the Isles of Scilly and the Isle of Wight. The area now called England was first inhabited by modern humans during the Upper Paleolithic period, but takes its name from the Angles, a Germanic tribe deriving its name from the Anglia peninsula, who settled during the 5th and 6th centuries. England became a unified state in the 10th century and has had a significant cultural and legal impact on the wider world since the Age of Discovery, which began during the 15th century. The English language, the Anglican Church, and Engli ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Wear
The River Wear (, ) in North East England rises in the Pennines and flows eastwards, mostly through County Durham to the North Sea in the City of Sunderland. At long, it is one of the region's longest rivers, wends in a steep valley through the cathedral city of Durham and gives its name to Weardale in its upper reach and Wearside by its mouth. Etymology The origin behind the hydronym ''Wear'' is uncertain but is generally understood to be Celtic. The ''River Vedra'' on the Roman Map of Britain may very well be the River Wear. The name may be derived from Brittonic ''*wejr'' (<''*wẹ:drÄ''), which meant "a bend" (c.f ''-gwair-''). An alternative but very problematic etymology might involve ''*wẹ:d-r-'', from a lengthened form of the |
A689 Road
The A689 is a road in northern England that runs east from the A595, to the west of Carlisle in Cumbria, to Hartlepool in County Durham. The road begins west of Carlisle, just outside the city at the A595. The initial stretch was recently constructed as part of the Carlisle Northern Development Route, a road bypassing Carlisle from west to north. Crossing the River Eden and the West Coast Main Line, the road intersects with Junction 44 of the M6 at Greymoorhill. From Junction 44 of the M6, the A689 runs roughly south-east to a roundabout, with the B6264. From here, the A689 heads east, and crosses the River Irthing at Ruleholme, then it meets the A69 at a roundabout junction. The A689 joins the route of the A69 around part of the Brampton bypass. Near the village of Milton, the A689 turns right, and continues through Milton and Hallbankgate before crossing the border into the county of Northumberland. The route continues roughly south-east, and re-enters the county o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Frosterley
Frosterley is a village in County Durham, in England. It is situated in Weardale, on the River Wear close to its confluence with Bollihope Burn; between Wolsingham and Stanhope, County Durham, Stanhope; 18 miles west of Durham, England, Durham City and 26 miles southwest of Newcastle-upon-Tyne. In the United Kingdom Census 2001, 2001 census Frosterley had a population of 705. Frosterley is on the Weardale Railway. Heritage trains currently run to Stanhope, County Durham, Stanhope, Wolsingham and Witton-le-Wear History The area has been inhabited since Mesolithic times: Mesolithic flints and Neolithic stones axes have been found in the vicinity. A bronze spearhead was found in a local quarry dating to the late Bronze Age circa 1000 BC. The village itself has Middle Ages, medieval origins, and although the original houses have long been replaced, the village still retains its medieval pattern. On the north of the village are the remains of Saint Botolph, St Botolph’s Chapel. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geological Conservation Review
The Geological Conservation Review (GCR) is produced by the UK's Joint Nature Conservation Committee and is designed to identify those sites of national and international importance needed to show all the key scientific elements of the geological and geomorphological features of Britain. These sites display sediments, rocks, minerals, fossils, and features of the landscape that make a special contribution to an understanding and appreciation of Earth science and the geological history of Britain, which stretches back more than three billion years. The intention of the project, which was devised in 1974 by George Black and William Wimbledon working for the Governmental advisory agency, the Nature Conservancy Council (NCC), was activated in 1977. It aimed to provide the scientific rationale and information base for the conservation of geological SSSIs (Sites of Special Scientific Interest, protected under British law (latterly the Wildlife and Countryside Act 1981, as amended 1995). ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Namurian
The Namurian is a stage in the regional stratigraphy of northwest Europe with an age between roughly 326 and 313 Ma (million years ago). It is a subdivision of the Carboniferous system or period and the regional Silesian series. The Namurian is named for the Belgian city and province of Namur where strata of this age occur (part of the Belgian Coal Measures). The Millstone Grit Group in the lithostratigraphy of northern England and parts of Wales is also of Namurian age. The Namurian age lasted from 326 to 313 million years ago. It is preceded by the Visean stage/age (which corresponds to the upper Carboniferous Limestone of Great Britain) and succeeded by the Westphalian stage/age (which corresponds to the lower and middle Coal Measures of Great Britain). In the official geologic timescale of the International Commission on Stratigraphy (ICS), the Namurian straddles the boundary between the Mississippian epoch (359-318 Ma) and the Pennsylvanian epoch (318-299 Ma). The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Riverine
A river is a natural flowing watercourse, usually freshwater, flowing towards an ocean, sea, lake or another river. In some cases, a river flows into the ground and becomes dry at the end of its course without reaching another body of water. Small rivers can be referred to using names such as creek, brook, rivulet, and rill. There are no official definitions for the generic term river as applied to geographic features, although in some countries or communities a stream is defined by its size. Many names for small rivers are specific to geographic location; examples are "run" in some parts of the United States, "burn" in Scotland and northeast England, and "beck" in northern England. Sometimes a river is defined as being larger than a creek, but not always: the language is vague. Rivers are part of the water cycle. Water generally collects in a river from precipitation through a drainage basin from surface runoff and other sources such as groundwater recharge, springs, a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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