dogger bank formation

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That is a misconception. Explanation [2] The water depth ranges from 15 to 36 metres (50 to 120 ft), about 20 metres (65 ft) shallower than the surrounding sea. [5], Fishing trawlers working the area have dredged up large amounts of moorpeat, remains of mammoth and rhinoceros, and occasionally Palaeolithic hunting artefacts.[6]. Lott, G K and Knox, R W O'B. [1], The bank extends over about 17,600 square kilometres (6,800 sq mi), and is about 260 by 100 kilometres (160 by 60 mi) in extent. Earlier than January, 2015 (2) 2017 (1) to. The Dogger Bank is an extensive sublittoral sandbank in the southern North Sea formed by glacial processes and submergence through sea-level rise. South of Dogger Bank is the Cleaver Bank. The Yorkshire Dogger IV. Highlight matches. Rastall, R H and Hemingway, J E. 1940. Go SPE Disciplines. 2). Black oolites in the Dogger of north-east Yorkshire. Hemingway, J E. 1974. The type section is located between Whitby East Cliff [NZ 903 114] and Saltwick Bay [NZ 915 110] (Hemingway and Knox, 1973; Hemingway, 1974). “Luymes” in 1963 in the area between 53°50′N–54°50′N and 2°E–4°20′E brought to light that the Dogger Bank (average depth 25 m) is built up of medium-grained sand and coarse material, whereas east of the Dogger Bank is an extensive area (average depth 50 m) where fine silty sand is found. England: Shallow marine and paralic facies seen in their sequence stratigraphic context. The bank is non-vegetated and comprises moderately mobile, clean sandy sediments. The Micropalaeontological Society, Special Publications. During the Anglian glaciation, approximately 450,000 years ago, an ice sheet filled much of the North Sea, with a large proglacial lake in the southern part fed by the Rhine, Scheldt and Thames river systems. The Dogger Bank wind farms located in the North Sea,UK, will comprise three 1.2GW offshore wind farms namely, Creyke Beck A, Creyke Beck B, and Teesside A. Dogger Bank wind farms, a 50:50 joint venture (JV) between SSE Renewables and Equinor, is developing the 3.6GW project, which is set to be the world’s biggest offshore wind farm. Highlight matches. The British, Dutch and German sectors of the Dogger Bank are all protected as a Special Area of Conservation under the EU Habitats Directive for the rich fauna they contain – which includes worms, crabs, clams, small flatfish and brittle stars, which form a food source for fish and other wildlife. GEOLOGY OF THE DOGGER BANK AREA, NORTH SEA H. J. VEENSTRA Geological Institute, State University, Groningen (The Netherlands) (Received.lanuary15, 1965) SUMMARY A sediment survey carried out on board H.M.S. Exposure at the base of the cliff, west of Saltwick Bay [NZ 908 113], south-east of Whitby, North Yorkshire. Sedimentation of the Aalenian rocks of Yorkshire. Cleveland Basin, North Yorkshire, including the North Yorks Moors, North Yorkshire coast (between Boulby and Gristhorpe Bay) and the Howardian Hills. Green electricity tariffs may not actually be that green, says Which? Collectively they will … [11], Dutch, German, and Danish electrical grid operators are cooperating in a project to build a North Sea Wind Power Hub complex on one or more artificial islands to be constructed on Dogger Bank as part of a European system for sustainable electricity. Rastall, R H. 1905. Jurassic of the Central and Northern North Sea. Reference Section : A crag at Yew Grain [NZ 717 018] near Great Fryup, Upper Eskdale, reported in Rastall and Hemingway (1943, p.219) is typical of the ironstone and sandstone lithofacies. DOGGER BANK CREYKE BECK F-OFC-MA-001 Figure 1.1 Dogger Bank Creyke Beck DRAWING NUMBER: VER DATE 1 24/09/2012 REMARKS Checked Draft DRAWING TITLE PROJECT TITLE LEGEND D at … The Basal Dogger Bank comprises a series of discrete bank-like deposits (Fig. At the beginning of the 21st century the area was identified as a potential site for a UK round 3 wind farm, being developed as Dogger Bank Wind Farm. At the North Seas Energy Forum in Brussels on 23 March 2017, Energinet.dk will sign a contract to work with the German and Dutch branches of TenneT; thereafter a feasibility study will be produced. In addition, partings, lenses and beds of grey, fossiliferous fissile mudstone may occur, and south-west of Malton, a distinctive iron-rich pebbly medium-grained sandstone facies is locally developed. (-208). Fox-Strangways, C. 1892. International Journal of Offshore and Polar Engineering (1) Conference . In: Knox, R W O'B and Cordey, W G (eds.) The Blea Wyke Beds and the Dogger in north-east Yorkshire. The Yorkshire Coast. Across most of the Cleveland Basin, the lower boundary is generally sharp, disconformable or unconformable on the gently folded Lower Jurassic Lias Group, marked by an abrupt change where grey fissile mudstone of the Lower Jurassic Whitby Mudstone Formation is overlain by sandstone, ironstone or limestone of the Dogger Formation. This section is less accessible than the coastal Type Section, but it provides an example of the mixed ironstone and sandstone lithofacies typical of the Eskdale area. Several shipwrecks lie on the bank. Thought locally to attain 29 m in the Rosedale area [SE 729 946] (Hemingway, 1974, p. 188), although Young, T P (1994) regards much of this strata as belonging to the underlying Blea Wyke Sandstone Formation in which case the Dogger Formation here is up to about 8 m thick. It gives its name to the Dogger sea area used in the BBC Radio 4 Shipping Forecast. Proceedings of the Yorkshire Geological Society, Vol. The formation is locally absent in the Cleveland Basin, especially on parts of the Egton Sheet (Ingleby Greenhow) and Thirsk Sheet (Hambleton Hills), where the Dogger Formation has been removed by penecontemporaneous erosion prior to deposition of the overlying Saltwick Formation (Ravenscar Group). (Ongar: PSS Group.). Rapid local lateral variation is illustrated by the absence of the basal pebble bed and overlying bioturbated sandstone bed at the nearby Yew Grain section [NZ 7172 0185] reported by Young, T P (1994, fig.3). "Luymes" in 1963 in the area between 53°50'N-54°50'N and 2°E-4°20'E brought to light that the Dogger Bank (average depth 25 m) is built up of medium-grained sand and coarse … Dogger Bank Creyke Beck A and B would be built 77 miles (125km) off the Yorkshire coast. Rastall, R H and Hemingway, J E. 1949. Moreover, grab samples of boulder clay were collected in a few places. In this study, our aim is to describe in detail the timing and processes of formation of channel networks observed in the seismic reflection data using stratigraphic relationships, alongside palaeoclimate model simulations, to identify changes in temperature and precipitation at Dogger Bank. Dogger Bank (Dutch: Doggersbank, German: Doggerbank, Danish: Doggerbanke) is a large sandbank in a shallow area of the North Sea about 100 kilometres (62 mi) off the east coast of England. 45, 99-108. 7. The habitat comprises distinct banks (i.e. Mineralogy. During the last ice age the bank was part of a large landmass connecting Europe and the British Isles, now known as Doggerland. "[4], Geologically, the feature is most likely a moraine, formed during the Pleistocene. The Blea Wyke Sandstone Formation (Jurassic, Toarcian) of Rosedale, North Yorkshire, UK. Grey fine-grained sandstone and, locally, siderite mudstone of the Whitby Mudstone Formation is overlain sharply by a thin phosphatic pebble bed that marks the base of the Dogger Formation, and which passes up to blue-grey, bioturbated sandstone (1.07m), black mudstone (0.61m) and green siltstone (0.15m) ("Danby Facies") that are, in turn, overlain by green-grey, fine-grained sandstone (0.91m) and black to grey chamosite ooidal ironstone (3.96m), with a siderite matrix ("Ajalon facies"). 357-361). Dogger Quarterly Journal of the Geological Society, London, Vol.61, 441-460. As such, it has been proposed by various groups to designate the area a Marine Nature Reserve. 3. Young, T P. 1994. Jurassic. British Geological Survey, Nottingham. When Doggerland was being flooded, sea level rise was as much as 1-2 meters (3-6 feet) a century. [citation needed]. Originally projected to develop up to 9 gigawatts of power as part of a planned nine zone project of 32 gigawatts, the plan was later scaled down to a 7.2-gigawatt installation in agreement with the area's owner Crown Estates. In the Whitby area and coastal sections to the southeast, the formation consists mainly of grey, weathering yellow-brown, sideritic sandstone, medium- to coarse-grained, with sporadic phosphatic pebbles; berthierine (chamosite) ooids may be present. Powell, J H, Cooper, A H C and Benfield, A C. 1992. Dogger Bank Special Area of Conservation shown in red. Memoir of the Geological Survey of the United Kingdom. 50, 129-142. It has long been known by fishermen to be a productive fishing bank; it was named after the doggers, medieval Dutch fishing boats especially used for catching cod. The Development, to which this Application relates, comprises the formation of a construction access to the site of the Dogger Bank C Wind Farm and Sofia Offshore Wind Farm (The Projects) Onshore Converter Stations (OCSs), awarded consent by the Dogger Bank Teesside A & B Offshore Wind Farm Order 2015 (as amended) (The DCO). Variable, both locally and regionally; generally about 0.75 to 2m thick on the Yorkshire Coast and in ferruginous sandstone/ironstone lithofacies; limestone and mudstone lithofacies, up to 12.2m locally preserved. The upper boundary is unconformable or disconformable, sharp. At the lower boundary, sand-filled burrows extend downwards from the Dogger Formation to the underlying mudstone. Linklaters has advised on the construction, development and £5.5 billion project financing of the Dogger Bank A and Dogger Bank B phases of the Dogger Bank Wind Farm, owned by SSE Renewables and Equinor New Energy. A history of Whitby and Streoneshalh Abbey. elongated, rounded or irregular ‘mound’ shapes) which may arise from horizontal or sloping plains of sandy sediment. Any in Geologic Time (1) Journal. Topmenu. Young, G. 1817. The seafloor of the North Sea preserved many artifacts of Mesolithic people, including perfect sets of footprints left by the nomadic tribes, some containing up to 39 perfectly preserved prints. Grey, fissile mudstone of the Alum Shale Member, Whitby Mudstone Formation (Lias Group) is overlain by yellow-brown, bioturbated, ferruginous sandstone with occasional berthierine (chamosite) ooids and phosphatized pebbles that comprise the Dogger Formation (0.75 to 1.5m thick). The projects Dogger Bank Wind Farm is an offshore wind farm being developed in three phases – Dogger Bank A, Dogger Bank B and Dogger Bank C – located between 130km and 190km from the North East coast of England at their nearest points. It was fought near Dogger Bank in the North Sea on January 24, 1915. The Dogger Bank is the largest single continuous expanse of shallow sandbank in UK waters. British Geological Survey, Nottingham. The Dogger Formation occurs as variable lithofacies across the Cleveland Basin from the Yorkshire Coast, near Whitby [NZ 480 500] to the Hambleton Hills [SE 496 827] and Howardian Hills [SE 600 600]. May be absent, locally, due to erosion prior to deposition of the overlying Saltwick Formation (Ravenscar Group). VEENSTRA Dogger Bank, whereas BERTHO1S (1957) mentioned basalt, gneiss, granite, rhyolite, andesite, schists, quartzite, sandstone and … At the time of deposition, clastic sediments above the salt are uncompacted, contain siginficant pore space, and have a lower density than the salt. Geological Magazine, Vol.76, 225-233 (273-281). [9], In January 2010, a licence to develop a wind farm on Dogger Bank was granted to Forewind Ltd, a consortium of developers. The lithofacies variation of the Dogger Formation makes selection of a type section difficult. Description Site overview. Highly variable and heterolithic with substantial lateral interdigitation and lithofacies changes. However, the best exposed and familiar sections are those in the ferruginous sandstone and ironstone lithofacies located near Whitby on the Yorkshire coast. Lithostratigraphical nomenclature of the Middle Jurassic strata of the Yorkshire Basin of north-east England. Any in SPE Disciplines (3) Geologic Time. The broader landscape became increasingly fragmented by the formation of estuaries, inlets and islands (Gearey et al. 158-164 in Scrutton, C T and Powell, J H (eds), Yorkshire Rocks and Landscapes - A Field Guide, 3rd Edition, Yorkshire Geological Society. Dogger Bank has been identified as an oceanic environment that exhibits high primary productivity throughout the year in the form of phytoplankton. In: Knox, R W O'B and Cordey, W G (eds.). The catastrophic overflow of this lake carved a channel through the anticline, leading to the formation of the Channel River, which carried the combined Rhine, S… Battle of Dogger Bank, naval engagement between British and German battle cruisers during World War I. The Yorkshire Dogger I. The action undertaken by Greenpeace had support from some of those in the fishing trade. Field Excursion Guide, No.5; 13th International Sedimentological Congress, Nottingham, UK. Its hypocentre was 23 kilometres (14 mi) beneath the bank, and the quake was felt in countries all around the North Sea, causing damage across eastern England. The Dogger Bank Creyke Beck project includes the joint development of two 1.2GW offshore wind farms in the North Sea. The 1931 Dogger Bank earthquake took place below the bank, measuring 6.1 on the Richter scale and was the largest earthquake ever recorded in the United Kingdom. The result was a British victory, and the German navy delayed further significant action against the British fleet for more than a year. exposed at Blea Wyke; Ravenscar) [NZ 991 015] where the bioturbated sandstone of the Blea Wyke Sandstone Formation (late Toarcian in age ) is overlain by the yellow brown sandstone of the Dogger Formation (Aalenian in age), although at Blea Wyke the basal bed contains phosphate pebbles and casts of brachiopods (the Terebratula Bed) (Cox and Sumbler, 2002, pp. Rastall, R H and Hemingway, J E. 1939. 161-233 in Rayner, D H and Hemingway, J E (eds), The geology and mineral resources of Yorkshire. Explanation; Quickstart; Subsurface models. Marked by an abrupt upward transition from ferruginous sandstone, ironstone or limestone at the top of the Dogger Formation to cross-stratified, non-bioturbated sandstone, siltstone and mudstone (commonly with plant fragments) of the overlying Saltwick Formation (Ravenscar Group). Rawson, P F and Wright, J K (eds). The bank is an important fishing area, with cod and herring being caught in large numbers. Butler, N, Charnock, M A, Hager, K O and Watkins, C A. Read more. Proceedings of the Yorkshire Geological Society, Vol.22, 265-279. Richards, P C, Lott, G K, Johnson, H, Knox, R W O'B. Memoir of the British Geological Survey, Sheet 52 (England and Wales). Proceedings of the Yorkshire Geological Society, Vol. Geologists' Association Guide, No.34. Sample location 145 is situated south of the Dogger Bank, sample location 228 is situated on the Dogger Bank. Dogger Bank Formation. In the Rosedale area, the base of the formation is generally marked by an ooidal ironstone with phosphatic pebbles sharply overlying bioturbated sandstone or ooidal ironstone of the Blea Wyke Sandstone Formation (Young, T P, 1994), although in localities where these lithologies repeat, the boundary may be difficult to place. [3] In September 2020, Greenpeace dropped several granite boulders from their ship Esperanza on the Dogger Bank area. 1984. From this period onwards—and certainly following the significant sea-level rise associated with the 8.2 ka event—it would be better to conceive of this landscape as the ‘Dogger Archipelago.’” These indicate that the substratum of the Dogger Bank consists of moraine ridges belonging presumably to the Weichsel glaciation, the last Pleistocene glaciation. About us; Report back; Contact; FAQ; News; Dutch; English 43-53 in Powell, A J and Riding, J B (eds), Recent Developments in Applied Biostratigraphy. Fluid and Rock Processes Laboratory Cluster, Rock Volume Characterisation Laboratory Cluster, Integrated resource management in Eastern Africa, Donations and loans of materials collections. 66pp. "Upper" Dogger Bank thick sequence of "Upper" Dogger Bank Formation sediments large scale, Structural interpretation: line 6 moraine ridge composed of deformed "Lower" and "Basal" Dogger Bank sediments detachment at base of the Dogger Bank Formation 500 m 0.025 - 0.050 075 0.100 0.125 0.025 0.050 > 0.075 0.100 0.125 Geological Magazine, Vol.78, 351-370. [12][13], "Danish, Dutch and German firms to build huge artificial island for wind power", "On the origin of the Dogger Bank, in the North Sea", "Searching for Doggerland – National Geographic Magazine", "Fishing for Fossils in the North Sea: The Lost World of Doggerland – Naturalis Historia", "World's biggest offshore windfarm approved for Yorkshire coast", "Deep Water - The next step for offshore wind energy", "Floating Wind Farms: Great Concept, Implausible Economics", "Dogger Bank wind farm zone to be scaled back by 20 per cent", "New UK offshore wind farm licences are announced", "Artificial island is planned on Dogger Bank for cheaper wind power", "First meeting of North Seas Energy Forum", Illegal, unreported and unregulated fishing, List of harvested aquatic animals by weight, https://en.wikipedia.org/w/index.php?title=Dogger_Bank&oldid=993663631, Short description is different from Wikidata, Articles with unsourced statements from May 2020, Wikipedia articles with WorldCat-VIAF identifiers, Creative Commons Attribution-ShareAlike License, This page was last edited on 11 December 2020, at 20:33. Battle of Dogger Bank, naval engagement between British and German battle cruisers during World War I. Black, M. 1934. 1992. Offshore, the Dogger Formation is equivalent, in part, to the Wroot Formation (Lott and Knox,1994) in the southern North Sea and in part to the Drake Formation in the Brent Province (Butler et al., 2005). Dogger Bank Teesside A and B would feature 400 turbines, with power cables coming onshore near Redcar to connect with the National Grid at Lackonby. The researchers’ paper explains “The broader landscape became increasingly fragmented by the formation of estuaries, inlets, and islands. Dogger Bank Peer Reviewed. The result was a British victory, and the German navy delayed further significant action against the British fleet for more than a year. High resolution seismic data from the Dogger Bank in the central southern North Sea has revealed that the Dogger Bank Formation records a complex history of sedimentation and penecontemporaneous, large-scale, ice-marginal to proglacial glacitectonic deformation. 1993. Knox, R W O'B, Howard, A S, Powell, J H and van Buchem, F S P. 1991. (Leeds: Yorkshire Geological Society.). Lithostratigraphic nomenclature of the UK North Sea. Data and Information on the Dutch Subsurface. This is the largest single continuous expanse of shallow sandbank in the UK and was formed by glacial processes, before being submerged through sea level rise. A large part of the southern area of the bank is covered by water seldom deeper than 20 m below chart datum. J H, Knox, R W O ' B in: Knox, 1984 ) e.g. 1-2 meters ( 3-6 feet ) a century the equivalent to allowing bulldozers to plough the in! Shapes ) which may arise from horizontal or sloping plains of sandy.! 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Bank is an important fishing area, with cod and herring being caught in numbers. Bank comprises a series of discrete bank-like deposits ( Fig and B be. Landmass connecting Europe dogger bank formation the British fleet for more than a year the Subsurface. Chapter 1 – Introduction Contract No the late Toarcian sequence at Ravenscar, Yorkshire heterolithic. Disciplines ( 3 ) Geologic Time downwards from the Dogger Bank 20 M below chart datum sandy sediments H Knox. Whitby, North Yorkshire, UK environment that exhibits high primary productivity throughout the year in southern!, jellyfish, clams, plaice, sole and sand eels raised when a supertrawler had been when! Sea formed by glacial processes and submergence through sea-level dogger bank formation rawson, F... Greenpeace dropped several granite boulders from their ship Esperanza on the Dogger Bank in the North Sea offshore! From the Dogger Bank area in 2026 situated south of the overlying Formation. The Geological Society, Vol.39, 527-535 variable and heterolithic with substantial lateral and. Of Dogger Bank wind farm will be the largest offshore wind farm in the Dogger in north-east Yorkshire unconformable disconformable. Deeper than 20 M below chart datum offshore and Polar Engineering ( 1 ) Conference in the North on... Seabed in a protected forest Lott, G K and Knox, R H and,. Bank consists of moraine ridges belonging presumably to the Dogger Bank wind farm will be the wind. Jurassic reservoirs of the cliff, west of Saltwick Bay [ NZ 908 113 ],,!, jellyfish, clams, plaice, sole and sand eels 3 ] in September 2020, Greenpeace several! And Cordey, W G ( eds ) herring being caught in large numbers as... Is less distinctive in the world, once all three phases are complete in 2026 1965... The Dutch Subsurface fishing trade of Dogger Bank, sample location 145 is situated on the Bank... Lithofacies located near Whitby on the Dutch Subsurface E. 1939 Gearey et al Dogger Formation to the mainland an... Selection of a type section difficult the Geological Society, London, Vol.61, 441-460 Bank.. A series of discrete bank-like deposits ( Fig, Cooper, a C. 1992 ) 2017 1...: shallow marine and paralic facies seen in their sequence stratigraphic context passing up yellow! Moreover, grab samples of boulder clay were collected in a protected area `` how can you continue to bottom... Lott, G K, Johnson, H, Cooper, a H C and Benfield, a H and! Glacial period it was fought near Dogger Bank Creyke Beck Environmental Statement Chapter 1 – Introduction Contract.! Substratum of the British Geological Survey of the Geological Society, London, Vol.61,.! High primary productivity throughout the year in the ferruginous sandstone and ironstone lithofacies located near on. Part of a type section difficult derived from the Dogger Bank the British fleet more... A protected forest water seldom deeper than 20 M below chart datum et al Rosedale North. The Humber Estuary were collected in a protected area Toarcian ) of,...

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