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. Knox, R W O B. Battle of Dogger Bank, naval engagement between British and German battle cruisers during World War I. Lithostratigraphical nomenclature of the Middle Jurassic strata of the Yorkshire Basin of north-east England. The boundary is less distinctive in the Peak Trough (Knox, 1984) (e.g. In central, north and west Cleveland there is a complex interdigitation between grey, weathering yellow-brown, berthierine (chamosite) ooidal ironstone (with siderite mudstone matrix) and pale grey limestone, medium-grained, bioclastic wackestone and packstone with peloids and ooids, generally bioturbated and locally cross-bedded. Battle of Dogger Bank, naval engagement between British and German battle cruisers during World War I. Highlight matches. The Blea Wyke Beds and the Dogger in north-east Yorkshire. Hemingway, J E and Knox, R W O'B. 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. [3] In September 2020, Greenpeace dropped several granite boulders from their ship Esperanza on the Dogger Bank area. British Geological Survey, Nottingham. Dogger Bank Creyke Beck A and B would be built 77 miles (125km) off the Yorkshire coast. "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 … Black, M. 1934. The result was a British victory, and the German navy delayed further significant action against the British fleet for more than a year. Richards, P C, Lott, G K, Johnson, H, Knox, R W O'B. 161-233 in Rayner, D H and Hemingway, J E (eds), The geology and mineral resources of Yorkshire. Rastall, R H. 1905. Green electricity tariffs may not actually be that green, says Which? Fox-Strangways, C. 1892. 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. Geological Magazine, Vol.86, 201-225, 265-278. 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. 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. Sedimentation of the Aalenian rocks of Yorkshire. Geological Magazine, Vol.76, 225-233 (273-281). Marine Geol., 3 (1965) 245-262 256 H.J. 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… 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). It is located in the southern North Sea, approximately 150km north east of the Humber Estuary, and was formed by glacial processes before being submerged through sea level rise. At the lower boundary, sand-filled burrows extend downwards from the Dogger Formation to the underlying mudstone. Earlier than January, 2015 (2) 2017 (1) to. 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. elongated, rounded or irregular ‘mound’ shapes) which may arise from horizontal or sloping plains of sandy sediment. Proceedings of the Yorkshire Geological Society, Vol. The Yorkshire Dogger II. The researchers’ paper explains “The broader landscape became increasingly fragmented by the formation of estuaries, inlets, and islands. The Jurassic Rocks of Britain, Vol.1. The upper boundary is unconformable or disconformable, sharp. Research Article A great wave: the Storegga tsunami and the end of Doggerland? The coastal region. A sediment survey carried out on board H.M.S. [9], In January 2010, a licence to develop a wind farm on Dogger Bank was granted to Forewind Ltd, a consortium of developers. The result was a British victory, and the German navy delayed further significant action against the British fleet for more than a year. (Ongar: PSS Group.). Lower and Middle Jurassic sediments of the Cleveland Basin N.E. 45, 99-108. Dogger Bank Formation. 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 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]. During the last ice age the bank was part of a large landmass connecting Europe and the British Isles, now known as Doggerland. The Dogger Bank is an isolated topographic relief located in the central part of the southern North Sea, extending into UK, German, Danish and Dutch waters (Figure 1). Field Excursion Guide, No.5; 13th International Sedimentological Congress, Nottingham, UK. About us; Report back; Contact; FAQ; News; Dutch; English 2). Any in Geologic Time (1) Journal. 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. Dogger Bank has been identified as an oceanic environment that exhibits high primary productivity throughout the year in the form of phytoplankton. Memoir of the British Geological Survey, Sheet 52 (England and Wales). Lott, G K and Knox, R W O'B. Powell, J H, Cooper, A H C and Benfield, A C. 1992. Go SPE Disciplines. and Riding, J B. The Yorkshire Dogger IV. The action undertaken by Greenpeace had support from some of those in the fishing trade. The bank is an important fishing area, with cod and herring being caught in large numbers. 1973. The oldest of these formations is the Dogger Bank Formation that comprises massive clays, sands and diamicts of glacial origin (Cotterill et al., 2017a), subdivided informally in this study into the Lower and Upper Dogger Bank sub-units. England: Shallow marine and paralic facies seen in their sequence stratigraphic context. 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). Topmenu. The Ravenscar Group: a coeval analogue for the Middle Jurassic reservoirs of the North Sea and offshore Mid-Norway. 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). Worms burrow into the sand and then become a food source for larger animals, … 357-361). Probably named after a synonym for the German Bight, the southeastern bight of the North Sea bounded by the Netherlands and Germany to the south, and Denmark and Germany to the east. 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. On the higher grounds, the Dogger Bank and Cleaver Bank (Fig.2), are patches covered with pebbles. Proceedings of the Yorkshire Geological Society, Vol.39, 527-535. Geological Magazine, Vol.78, 351-370. Reference Gearey, Hopla, Boomer, Smith, Marshall, Fitch, Griffiths, Tappin, Williams, Hill, Boomer and Wilkinson 2017: 49). South of Dogger Bank is the Cleaver Bank. Rastall, R H and Hemingway, J E. 1949. 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. .... [it] is the equivalent to allowing bulldozers to plough through a protected forest. Geological Magazine, Vol.80, 209-230. Rastall, R H and Hemingway, J E. 1943. Dogger Bank Special Area of Conservation shown in red. Young, T P. 1994. In: Knox, R W O'B and Cordey, W G (eds.) The Micropalaeontological Society, Special Publications. [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. [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. Memoir of the Geological Survey of the United Kingdom. Mineralogy. Several shipwrecks lie on the bank. 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 … Rawson, P F and Wright, J K (eds). Hoofdnavigatie. Jurassic of the Central and Northern North Sea. The Dogger Bank was selected for offshore wind farms because it is far away from shore, avoiding complaints about the visual impact of wind turbines, yet the water is shallow enough for traditional fixed foundation wind turbine designs. Highly variable and heterolithic with substantial lateral interdigitation and lithofacies changes. It was fought near Dogger Bank in the North Sea on January 24, 1915. Quarterly Journal of the Geological Society, London, Vol.61, 441-460. 3. The Yorkshire Dogger I. Explanation 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]. 1984. These indicate that the substratum of the Dogger Bank consists of moraine ridges belonging presumably to the Weichsel glaciation, the last Pleistocene glaciation. 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. Highlight matches. The Yorkshire Coast. In: Knox, R W O'B and Cordey, W G (eds.). 2nd Edition, 117pp. 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. (-208). 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. Proceedings of the Yorkshire Geological Society, Vol.22, 265-279. The Dogger Bank Wind Farm will be the largest offshore wind farm in the world, once all three phases are complete in 2026. Many explainations of salt domes suggest that the lower density of salt, compared to the density of overlying rock units, is the driving force of salt dome formation. The upper boundary is marked by the sharp change from ferruginous, bioturbated sandstone of the Dogger Formation to grey, fine- to medium-grained, locally cross-bedded sandstone with plant fragments of the overlying Saltwick Formation (Ravenscar Group). A 12,000 sq km (4,600 sq mile) area … The broader landscape became increasingly fragmented by the formation of estuaries, inlets and islands (Gearey et al. The Dogger Bank is an extensive sublittoral sandbank in the southern North Sea formed by glacial processes and submergence through sea-level rise. The lithofacies variation of the Dogger Formation makes selection of a type section difficult. 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 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. 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. [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. 1990. The Basal Dogger Bank comprises a series of discrete bank-like deposits (Fig. What causes the Earth’s climate to change? [2] The water depth ranges from 15 to 36 metres (50 to 120 ft), about 20 metres (65 ft) shallower than the surrounding sea. Where both formations are dominated by mudstone, the boundary may be somewhat cryptic – that of the Dogger Formation is dark grey, less silty and of a distinctly marine aspect, that of the Saltwick Formation is paler grey, silty and with black plant debris. The base of the overlying Saltwick Formation is marked by black, carbonaceous clay, passing up to yellow sandstone. 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 habitat comprises distinct banks (i.e. 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]. James Walker1, Vincent Gaffney1,*, Simon Fitch1, Merle Muru1,2, Andrew Fraser1, Martin Bates3 & Richard Bates4 1 School of Archaeological and Forensic Science, University of Bradford, UK 2 Department of Geography, Institute of Ecology and Earth Sciences, University of Tartu, Estonia 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. Offshore Document Number: F-OFC-CH-001 ... caused or arisin g from reliance upon in formation provid ed herein. 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. Supertrawler had been seen off the Yorkshire coast overlying Saltwick Formation ( Ravenscar Group ) the largest wind farm the... 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