Eskdale Anticline
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Eskdale Anticline
The Eskdale Anticline is a dip-slip Fault (geology)#Dip-slip faults, fault at Whitby in North Yorkshire, England. The anticline was thought to have stretched for approximately in a north–south direction underneath the mouth of the River Esk, North Yorkshire, River Esk in Whitby, with a depth of . However, modern geological studies have cast doubt on this, with a suggested displacement of only . Description The Eskdale Anticline was thought to have started north west of Scarborough, North Yorkshire, Scarborough and stretched for approximately along a north–south axis, and ending just off the coast of the River Esk mouth at Whitby in North Yorkshire. This results in a dip-slip fault of what was listed as a shift between the east and west cliffs at Whitby, where the West Cliff has sandstones covered by boulder drift, with a beach below of fine sand. The opposite side (the East Cliff), is composed of alum shale and has a rocky foreshore. The southern end of the anticline reach ...
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North Yorkshire
North Yorkshire is the largest ceremonial counties of England, ceremonial county (lieutenancy area) in England, covering an area of . Around 40% of the county is covered by National parks of the United Kingdom, 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 Office for National Statistics, 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 of England, unitary authorities. ...
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Whitby Mudstone
The Whitby Mudstone is a Toarcian (Early Jurassic; ''Falciferum''-''Bifrons'' in regional chronostratigraphy) geological formation in Yorkshire and Worcestershire, England.Whitby Mudstone
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The formation, part of the , is present in the and

List Of Geological Folds In Great Britain
This is a list of the named geological folds affecting the rocks of Great Britain and the Isle of Man. Terminology See the main article on folds for a fuller treatment of fold types and nomenclature but in brief, an anticline is an arch-like fold whereas a syncline is its converse; a downfold. Antiforms, anticlinoria, synforms and synclinoria are variations on these. A monocline (or, rarely, a monoform) is a step-like fold, one limb of which is roughly horizontal. Both domes and periclines are anticlines in which the strata fall away about equally in all directions. There are also a number of ' disturbances' named in parts of the country, notably in South Wales. These linear features are a combination of faults and folds - the relative importance of faulting and folding varying along the length of each disturbance. List of folds Key to table *Column 1 indicates the name of the fold. Some variant spellings are recorded between sources. *Column 2 indicates the county in wh ...
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Woodsmith Mine
Woodsmith Mine is a deep potash and polyhalite mine located near to the hamlet of Sneatonthorpe, Whitby in North Yorkshire, England. The venture was started by York Potash Ltd, which became a subsidiary of Sirius Minerals plc whose primary focus is the development of the polyhalite project. The project will mine the world's largest deposit of polyhalite – a naturally occurring mineral. Because the project would require mining to be undertaken in the North York Moors National Park, many objections were raised to the mine and the proposed conveyor that would be installed to transport the raw material offsite to a plant on Teesside away. The mine is expected to have a life of 100 years and has been labelled the biggest mining project in Britain for decades; its twin shafts will be the deepest commercial mineshafts in Britain. The project is expected to generate over £100 billion for the UK economy over a period of 50 years. Once it is functioning it will be the deepest min ...
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British Geological Survey
The British Geological Survey (BGS) is a partly publicly funded body which aims to advance geoscientific knowledge of the United Kingdom landmass and its continental shelf by means of systematic surveying, monitoring and research. The BGS headquarters are in Keyworth, Nottinghamshire, England. Its other centres are located in Edinburgh, Wallingford, Cardiff and London. The current motto of the BGS is: ''Gateway to the Earth''. History and previous names The Geological Survey was founded in 1835 by the Board of Ordnance as the Ordnance Geological Survey, under Henry De la Beche. This was the world's first national geological survey. It remained a branch of the Ordnance Survey for many years. In 1965, it was merged with the Geological Museum and Overseas Geological Surveys, under the name of Institute of Geological Sciences. On 1 January 1984, the institute was renamed the British Geological Survey (and often referred to as the BGS), a name still carried today. Competenc ...
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Percy Fry Kendall
Percy Fry Kendall, FRS (15 November 1856 – 19 March 1936), was an English geologist who was Professor of Geology at the University of Leeds from 1906 to 1922. Early life and education Kendall was the youngest of the eight children of Charles Kendall, a commercial traveller, and his wife Hannah Eltringham. He was born on 15 November 1856 in Mile End, London. He was educated at home and then studied Biology under Professor T H Huxley FRS and Geology under Professor J W Judd FRS at the Royal College of Science (now part of Imperial College London) in South Kensington, London. Academic career In 1885 Kendall became Bishop Berkeley Fellow at Owens College, Manchester, by then part of the federal Victoria University. In 1887 he was appointed an Assistant Lecturer in Geology there. In 1889 Kendall moved to Stockport Technical School as a part-time Lecturer in Natural Sciences. By 1891 Kendall was also lecturing part-time at the Yorkshire College in Leeds. The Yorkshire ...
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Ironstone
Ironstone is a sedimentary rock, either deposited directly as a ferruginous sediment or created by chemical replacement, that contains a substantial proportion of an iron ore compound from which iron (Fe) can be smelted commercially. Not to be confused with native or telluric iron, which is very rare and found in metallic form, the term ''ironstone'' is customarily restricted to hard, coarsely banded, non-banded, and non-cherty sedimentary rocks of post-Precambrian age. The Precambrian deposits, which have a different origin, are generally known as banded iron formations. The iron minerals comprising ironstones can consist either of oxides, i.e. limonite, hematite, and magnetite; carbonates, i.e. siderite; silicates, i.e. chamosite; or some combination of these minerals.U.S. Bureau of Mines Staff (1996) ''Dictionary of Mining, Mineral, & Related Terms.'' Report SP-96-1, U.S. Department of Interior, U.S. Bureau of Mines, Washington, D.C.Neuendorf, K. K. E., J. P. Mehl Jr., and J. A. ...
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Sandsend
Sandsend is a small fishing village, near to Whitby in the Scarborough (borough), Scarborough district of North Yorkshire, England. It forms part of the Civil parishes of England, civil parish of Lythe. It is the birthplace of fishing magnate George Pyman. Originally two villages, Sandsend and East Row, the united Sandsend has a pub and restaurant. A large part of the western side of the village, in The Valley, is still owned by Mulgrave Estate. The Valley is one of the most expensive areas to buy property on the Yorkshire Coast. History Sandsend and the neighbouring village of East Row began as separate villages but were joined when extra cottages were built for workers in the alum industry. Sandsend was also buoyed by tourism from the Whitby, Redcar and Middlesbrough Union Railway, which ran through the village from 1855 to 1958. The local station was Sandsend railway station, which opened in 1883 and was closed in 1958. In popular culture In the 1947 British comedy dram ...
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North Sea
The North Sea lies between Great Britain, Norway, Denmark, Germany, the Netherlands and Belgium. An epeiric sea on the European continental shelf, it connects to the Atlantic Ocean through the English Channel in the south and the Norwegian Sea in the north. It is more than long and wide, covering . It hosts key north European shipping lanes and is a major fishery. The coast is a popular destination for recreation and tourism in bordering countries, and a rich source of energy resources, including wind and wave power. The North Sea has featured prominently in geopolitical and military affairs, particularly in Northern Europe, from the Middle Ages to the modern era. It was also important globally through the power northern Europeans projected worldwide during much of the Middle Ages and into the modern era. The North Sea was the centre of the Vikings' rise. The Hanseatic League, the Dutch Republic, and the British each sought to gain command of the North Sea and access t ...
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Andean Orogeny
The Andean orogeny ( es, Orogenia andina) is an ongoing process of orogeny that began in the Early Jurassic and is responsible for the rise of the Andes mountains. The orogeny is driven by a reactivation of a long-lived subduction system along the western margin of South America. On a continental scale the Cretaceous (90 Ma) and Oligocene (30 Ma) were periods of re-arrangements in the orogeny. Locally the details of the nature of the orogeny varies depending on the segment and the geological period considered. Overview Subduction orogeny has been occurring in what is now western South America since the break-up of the supercontinent Rodinia in the Neoproterozoic. The Paleozoic Pampean, Famatinian and Gondwanan orogenies are the immediate precursors to the later Andean orogeny.Charrier ''et al''. 2006, pp. 113–114. The first phases of Andean orogeny in the Jurassic and Early Cretaceous were characterized by extensional tectonics, rifting, the development of back-arc basins a ...
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Ruswarp
Ruswarp village lies within the Scarborough borough of North Yorkshire, England. It is around from Whitby, at the junction of the B1410 and B1416 roads, on the River Esk and the Esk Valley Line, with trains stopping at Ruswarp railway station. Originally it was called Risewarp (Old English hrīs wearp, ) meaning 'silted land overgrown with brushwood'. Northern Rail serves the station and Bus services connect the village to the surrounding area. The village is served by local shops including a butcher and a bakery, as well as a grocery store further down the street. There is a pub, the ''Bridge Inn'' and a parish church, the Church of St Bartholomew. Primary education is catered for by a local Church of England primary school. There was a Post Office opposite the butcher, but that closed down several years ago after losing the franchise, and is now converted into a private residence. Crossing the River Esk downstream is a railway viaduct, 120 feet high, built (using 5,2 ...
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Scarborough, North Yorkshire
Scarborough () is a seaside town in the Borough of Scarborough in North Yorkshire, England. Scarborough is located on the North Sea coastline. Historic counties of England, Historically in the North Riding of Yorkshire, the town lies between 10 and 230 feet (3–70 m) above sea level, from the harbour rising steeply north and west towards limestone cliffs. The older part of the town lies around the harbour and is protected by a rocky headland. With a population of 61,749, Scarborough is the largest seaside resort, holiday resort on the Yorkshire Coast and largest seaside town in North Yorkshire. The town has fishing and service industries, including a growing digital and creative economy, as well as being a tourist destination. Residents of the town are known as Scarborians. History Origins The town was reportedly founded around 966 AD as by Thorgils Skarthi, a Viking raider, though there is no archaeological evidence to support these claims, made during the 1960s, as p ...
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