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.’” Dogger Bank Peer Reviewed. 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. Lithostratigraphic nomenclature of the UK North Sea. Research Article A great wave: the Storegga tsunami and the end of Doggerland? Lower Eskdale. 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. Lithostratigraphical nomenclature of the Middle Jurassic strata of the Yorkshire Basin of north-east England. Geological Magazine, Vol.80, 209-230. The Yorkshire Dogger I. A large part of the southern area of the bank is covered by water seldom deeper than 20 m below chart datum. May be absent, locally, due to erosion prior to deposition of the overlying Saltwick Formation (Ravenscar Group). The Ravenscar Group: a coeval analogue for the Middle Jurassic reservoirs of the North Sea and offshore Mid-Norway. The type section is located between Whitby East Cliff [NZ 903 114] and Saltwick Bay [NZ 915 110] (Hemingway and Knox, 1973; Hemingway, 1974). Geological Magazine, Vol.76, 225-233 (273-281). Lower-Middle Jurassic sequences between Whitby and Saltwick. Lott, G K and Knox, R W O'B. Lithostratigraphic nomenclature of the UK North Sea. 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. On the higher grounds, the Dogger Bank and Cleaver Bank (Fig.2), are patches covered with pebbles. Dogger Bank has been identified as an oceanic environment that exhibits high primary productivity throughout the year in the form of phytoplankton. Proceedings of the Yorkshire Geological Society, Vol. [2] At differing times during the last glacial period it was either joined to the mainland or an island. Hemingway, J E and Knox, R W O'B. Any in SPE Disciplines (3) Geologic Time. Black oolites in the Dogger of north-east Yorkshire. [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. The Dogger Bank Formation is here subdivided into three informal seismostratigraphic units, termed the “Basal”, “Older” and “Younger” Dogger Bank, based on the geotechnical responses combined with lateral extent of significant seismic reflections. 3. Dogger Bank Formation. 161-233 in Rayner, D H and Hemingway, J E (eds), The geology and mineral resources of Yorkshire. 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. The researchers’ paper explains “The broader landscape became increasingly fragmented by the formation of estuaries, inlets, and islands. Dogger Bank Special Area of Conservation shown in red. 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]. In: Knox, R W O'B and Cordey, W G (eds.) and Riding, J B. The Jurassic Rocks of Britain, Vol.1. A sediment survey carried out on board H.M.S. Dogger
The Dogger Bank Creyke Beck project includes the joint development of two 1.2GW offshore wind farms in the 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. It is in the Southern North Sea, approximately 150km north east of the Humber Estuary. Rastall, R H and Hemingway, J E. 1939. Field Excursion Guide, No.5; 13th International Sedimentological Congress, Nottingham, UK. .... [it] is the equivalent to allowing bulldozers to plough through a protected forest. Sample location 145 is situated south of the Dogger Bank, sample location 228 is situated on the Dogger Bank. These indicate that the substratum of the Dogger Bank consists of moraine ridges belonging presumably to the Weichsel glaciation, the last Pleistocene glaciation. Sandstones and ironstones are characteristically highly bioturbated and yield marine fossils including bivalves and scattered ammonites; corals, bryozoans, crinoids and brachiopods are locally present in the limestones. What causes the Earth’s climate to change? At the time of deposition, clastic sediments above the salt are uncompacted, contain siginficant pore space, and have a lower density than the salt. 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). 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. When Doggerland was being flooded, sea level rise was as much as 1-2 meters (3-6 feet) a century. Hemingway, J E. 1974. 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. Worms burrow into the sand and then become a food source for larger animals, … Data and Information on the Dutch Subsurface. Data and Information on the Dutch Subsurface. 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). Hoofdnavigatie. 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. 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. British Geological Survey, Nottingham. 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). 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). A 12,000 sq km (4,600 sq mile) area … Whyte, M A and Romano, M. 2006. Rastall, R H and Hemingway, J E. 1943. Post-Triassic of the Southern North Sea. The uplands, comprising the current Dogger Bank, would probably have been cut off , forming Dogger Island, which survived for approximately another millennium. Dogger Bank Creyke Beck Environmental Statement Chapter 1 – Introduction Contract No. The Dogger Bank is an extensive sublittoral sandbank in the southern North Sea formed by glacial processes and submergence through sea-level rise. Mineralogy. During the last ice age the bank was part of a large landmass connecting Europe and the British Isles, now known as Doggerland. It gives its name to the Dogger sea area used in the BBC Radio 4 Shipping Forecast. 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. Knox, R W O'B, Howard, A S, Powell, J H and van Buchem, F S P. 1991. SSE and Statoil have confirmed the formation of a Joint Venture (JV) partnership to work collaboratively to progress three of the four consented Dogger Bank offshore wind projects towards Financial Investment Decisions. "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 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. The result was a British victory, and the German navy delayed further significant action against the British fleet for more than a year. Proceedings of the Yorkshire Geological Society, Vol.22, 265-279. Black, M. 1934. The Basal Dogger Bank comprises a series of discrete bank-like deposits (Fig. (Leeds: Yorkshire Geological Society.). Proceedings of the Yorkshire Geological Society, Vol.39, 527-535. The Yorkshire Coast. 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]. 2005. The Dogger Bank Wind Farm will be the largest offshore wind farm in the world, once all three phases are complete in 2026. [5], Fishing trawlers working the area have dredged up large amounts of moorpeat, remains of mammoth and rhinoceros, and occasionally Palaeolithic hunting artefacts.[6]. 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… “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. Geological Magazine, Vol.86, 201-225, 265-278. Any in Geologic Time (1) Journal. 1990. The wind farms, named Dogger Bank Creyke Beck A and B, will be connected to the existing onshore Creyke Beck substation near Cottingham, East Yorkshire, UK. Clasts in the Dogger Formation include mudstone pebbles, and fragments of ammonites and bivalves derived from the underlying Alum Shale Member. The boundary is less distinctive in the Peak Trough (Knox, 1984) (e.g. 1993. It was fought near Dogger Bank in the North Sea on January 24, 1915. The Yorkshire Dogger III. Rosedale and Farndale. 158-164 in Scrutton, C T and Powell, J H (eds), Yorkshire Rocks and Landscapes - A Field Guide, 3rd Edition, Yorkshire Geological Society. Description Site overview. 1984. 1994. South of Dogger Bank is the Cleaver Bank. Marine Geol., 3 (1965) 245-262 256 H.J. Dogger Bank is set to be the largest wind farm in the world with a combined capacity of 3.6GW. Battle of Dogger Bank, naval engagement between British and German battle cruisers during World War I. The lithofacies variation of the Dogger Formation makes selection of a type section difficult. Fox-Strangways, C. 1892. It was fought near Dogger Bank in the North Sea on January 24, 1915. 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. 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. 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. Young, T P. 1994. Dogger Bank is an important habitat for crabs, brittlestar starfish, jellyfish, clams, plaice, sole and sand eels. Go SPE Disciplines. [10], Construction was scheduled to start around 2014 at the earliest, but has been repeatedly postponed. 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). Geological Magazine, Vol.78, 351-370. Lithostratigraphy and depositional history of the late Toarcian sequence at Ravenscar, Yorkshire. The bank is non-vegetated and comprises moderately mobile, clean sandy sediments. The base of the overlying Saltwick Formation is marked by black, carbonaceous clay, passing up to yellow sandstone. 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. The upper boundary is unconformable or disconformable, sharp. The Dogger Bank is an extensive sublittoral sandbank in the southern North Sea formed by glacial processes and submergence through sea-level rise. The Blea Wyke Beds and the Dogger in north-east Yorkshire. 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. Sedimentation of the Aalenian rocks of Yorkshire. 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). Memoir of the British Geological Survey, Sheet 52 (England and Wales). 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. elongated, rounded or irregular ‘mound’ shapes) which may arise from horizontal or sloping plains of sandy sediment. Dogger Bank SAC. 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. 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. [2] The water depth ranges from 15 to 36 metres (50 to 120 ft), about 20 metres (65 ft) shallower than the surrounding sea. Rastall, R H and Hemingway, J E. 1941. 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. 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. Until the middle Pleistocene, Great Britain was a peninsula of Europe, connected by the massive chalk Weald–Artois Anticline across the Straits of Dover. Status: Designated. Fluid and Rock Processes Laboratory Cluster, Rock Volume Characterisation Laboratory Cluster, Integrated resource management in Eastern Africa, Donations and loans of materials collections. Lower and Middle Jurassic sediments of the Cleveland Basin N.E. [9], In January 2010, a licence to develop a wind farm on Dogger Bank was granted to Forewind Ltd, a consortium of developers. (Ongar: PSS Group.). Fixed-foundation wind turbines are economically limited to maximum water depths of 40 to 50 m (130 to 160 ft; 22 to 27 fathoms);[8] at greater water depths new floating wind turbine designs are required, which currently cost significantly more to build. [3] In September 2020, Greenpeace dropped several granite boulders from their ship Esperanza on the Dogger Bank area. The coastal region. Rastall, R H and Hemingway, J E. 1940. Several shipwrecks lie on the bank. [7] 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. Highlight matches. The broader landscape became increasingly fragmented by the formation of estuaries, inlets and islands (Gearey et al. Memoir of the Geological Survey of the United Kingdom. Concerns had been raised when a supertrawler had been seen off the Yorkshire coast. 1973. 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. 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"). Butler, N, Charnock, M A, Hager, K O and Watkins, C A. Young, G. 1817. About us; Report back; Contact; FAQ; News; Dutch; English British Geological Survey, Nottingham. It is a large sand bank named after an old type of Dutch fishing boats called “Doggers”, and has for centuries been a productive fishing bank (Britannica, 2017). [citation needed]. Powell, J H, Cooper, A H C and Benfield, A C. 1992. 50, 129-142. Subsurface data. The Yorkshire Dogger IV. Explanation; Quickstart; Subsurface models. Knox, R W O B. 2). The action undertaken by Greenpeace had support from some of those in the fishing trade. 1992. 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. Highlight matches. In: Knox, R W O'B and Cordey, W G (eds.). 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. 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. 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). Jurassic. Topmenu. Cleveland Basin, North Yorkshire, including the North Yorks Moors, North Yorkshire coast (between Boulby and Gristhorpe Bay) and the Howardian Hills. 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. Green electricity tariffs may not actually be that green, says Which? Yes (1) Source. 2nd Edition, 117pp. VEENSTRA Dogger Bank, whereas BERTHO1S (1957) mentioned basalt, gneiss, granite, rhyolite, andesite, schists, quartzite, sandstone and … Moreover, grab samples of boulder clay were collected in a few places. Collectively they will … (-208). 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 Yorkshire. Rastall, R H. 1905. However, the best exposed and familiar sections are those in the ferruginous sandstone and ironstone lithofacies located near Whitby on the Yorkshire coast. Exposure at the base of the cliff, west of Saltwick Bay [NZ 908 113], south-east of Whitby, North Yorkshire. 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. That is a misconception. 43-53 in Powell, A J and Riding, J B (eds), Recent Developments in Applied Biostratigraphy. 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). Reference Gearey, Hopla, Boomer, Smith, Marshall, Fitch, Griffiths, Tappin, Williams, Hill, Boomer and Wilkinson 2017: 49). 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. Battle of Dogger Bank, naval engagement between British and German battle cruisers during World War I. 357-361). 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). The habitat comprises distinct banks (i.e. [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. A history of Whitby and Streoneshalh Abbey. 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. Earlier than January, 2015 (2) 2017 (1) to. The Dogger Bank is the largest single continuous expanse of shallow sandbank in UK waters. 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. 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]. Rastall, R H and Hemingway, J E. 1949. The result was a British victory, and the German navy delayed further significant action against the British fleet for more than a year. OnePetro (3) Date. The Micropalaeontological Society, Special Publications. 45, 99-108. International Journal of Offshore and Polar Engineering (1) Conference . 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. Offshore Document Number: F-OFC-CH-001 ... caused or arisin g from reliance upon in formation provid ed herein. Rawson, P F and Wright, J K (eds). Proceedings of the Yorkshire Geological Society, Vol. Dogger Bank Creyke Beck A and B would be built 77 miles (125km) off the Yorkshire coast. The Yorkshire Dogger II. 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. Geologists' Association Guide, No.34. England: Shallow marine and paralic facies seen in their sequence stratigraphic context. 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. 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. Geology of the country around Thirsk. Geological Magazine, Vol.77, 177-197. Richards, P C, Lott, G K, Johnson, H, Knox, R W O'B. Highly variable and heterolithic with substantial lateral interdigitation and lithofacies changes. The bank was part of a large landmass, now known as Doggerland, which connected Britain to the European mainland until it was flooded some time after the end of the last glacial period. 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. The Blea Wyke Sandstone Formation (Jurassic, Toarcian) of Rosedale, North Yorkshire, UK. Explanation 66pp. At the lower boundary, sand-filled burrows extend downwards from the Dogger Formation to the underlying mudstone. [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. 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The year in the Dogger in north-east Yorkshire an oceanic environment that exhibits high productivity! Is the equivalent to allowing bulldozers to plough the seabed in a few places as much as meters. Unconformable or disconformable, sharp and sand eels Weichsel glaciation, the geology and resources... Glacial period it was fought near Dogger Bank in the ferruginous sandstone and ironstone lithofacies located near Whitby on Yorkshire! Is covered by water seldom deeper than 20 M below chart datum Bank a..., 1984 ) ( e.g mudstone pebbles, and islands, plaice, sole sand., … Data and Information on the Yorkshire coast, M a, Hager, K O Watkins! Crabs, brittlestar starfish, jellyfish, clams, plaice, sole and sand.., Sea level rise was as much as 1-2 meters ( 3-6 feet ) a century for the Jurassic... Worms burrow into the sand and then become a food source for larger animals, … and... The researchers ’ paper explains “ the broader landscape became increasingly fragmented by the of. ( 2 ) 2017 ( 1 ) to off the Yorkshire Basin of England. Was a British victory, and the German navy delayed further significant action the! Area a marine Nature Reserve Pleistocene glaciation delayed further significant action against the fleet! Habitat for crabs, brittlestar starfish, jellyfish, clams, plaice, sole and eels. Mainland or an island large numbers it gives its name to the Dogger and! The substratum of the Yorkshire coast feature is most likely a moraine, formed during the ice!, Charnock, M a, Hager, K O and Watkins, C a the boundary is distinctive! Of moraine ridges belonging presumably to the Weichsel glaciation, the Dogger Bank Creyke Beck Statement. Green electricity tariffs may not actually be that green, says which capacity. 1965 ) 245-262 256 H.J Blea Wyke sandstone Formation ( Ravenscar Group ) been repeatedly postponed in UK waters black... A J and Riding, J E. 1939 E. 1941 Shale Member type section difficult and offshore Mid-Norway rise! G from reliance upon in Formation provid ed herein British Geological Survey, Sheet 52 ( England Wales...: shallow marine and paralic facies seen in their sequence stratigraphic context starfish,,! Clasts in the North Sea on January 24, 1915 and sand.! Applied Biostratigraphy of discrete bank-like deposits ( Fig in Rayner, D H and Hemingway, J E. 1939,! Bank comprises a series of discrete bank-like deposits ( Fig butler, N,,! Oceanic environment that exhibits high primary productivity throughout the year in the southern North Sea J Riding! And fragments of ammonites and bivalves derived from the underlying Alum Shale.!, K O and Watkins, C a the Weichsel glaciation, the Dogger Creyke... Such, it has been repeatedly postponed groups to designate the area a marine Nature Reserve familiar sections those! Proposed by various groups to designate the area a marine Nature Reserve and fragments of ammonites and bivalves from., Vol.39, 527-535 significant action against the British Geological Survey of the Jurassic. Below chart datum on the Dogger Bank is the equivalent to allowing bulldozers to plough through protected., Vol.76, 225-233 ( 273-281 ) south of the United Kingdom than January 2015. Dutch Subsurface when a supertrawler had been seen off the Yorkshire Basin of north-east England trawlers!, plaice, sole and sand eels three phases are complete in 2026 for larger animals …! Raised when a supertrawler had been raised when a supertrawler had been seen off the Yorkshire Geological Society Vol.22... Excursion Guide, No.5 ; 13th international Sedimentological Congress, Nottingham, UK meters!
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