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dogger bank formation

[citation needed]. Geological Magazine, Vol.76, 225-233 (273-281). About us; Report back; Contact; FAQ; News; Dutch; English Lott, G K and Knox, R W O'B. 357-361). Battle of Dogger Bank, naval engagement between British and German battle cruisers during World War I. The Dogger Bank Wind Farm will be the largest offshore wind farm in the world, once all three phases are complete in 2026. 1993. The Jurassic Rocks of Britain, Vol.1. 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. The Basal Dogger Bank comprises a series of discrete bank-like deposits (Fig. 2nd Edition, 117pp. A sediment survey carried out on board H.M.S. On the higher grounds, the Dogger Bank and Cleaver Bank (Fig.2), are patches covered with pebbles. 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"). The uplands, comprising the current Dogger Bank, would probably have been cut off , forming Dogger Island, which survived for approximately another millennium. A large part of the southern area of the bank is covered by water seldom deeper than 20 m below chart datum. At the time of deposition, clastic sediments above the salt are uncompacted, contain siginficant pore space, and have a lower density than the salt. England: Shallow marine and paralic facies seen in their sequence stratigraphic context. Young, T P. 1994. Until the middle Pleistocene, Great Britain was a peninsula of Europe, connected by the massive chalk Weald–Artois Anticline across the Straits of Dover. Dogger Bank Special Area of Conservation shown in red. Lithostratigraphical nomenclature of the Middle Jurassic strata of the Yorkshire Basin of north-east England. Dogger Bank is an important habitat for crabs, brittlestar starfish, jellyfish, clams, plaice, sole and sand eels. Yes (1) Source. Fluid and Rock Processes Laboratory Cluster, Rock Volume Characterisation Laboratory Cluster, Integrated resource management in Eastern Africa, Donations and loans of materials collections. The Yorkshire Coast. Topmenu. and Riding, J B. 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. 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. 3. The bank is an important fishing area, with cod and herring being caught in large numbers. 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. (Leeds: Yorkshire Geological Society.). 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. Knox, R W O'B, Howard, A S, Powell, J H and van Buchem, F S P. 1991. 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. Clasts in the Dogger Formation include mudstone pebbles, and fragments of ammonites and bivalves derived from the underlying Alum Shale Member. Any in SPE Disciplines (3) Geologic Time. The type section is located between Whitby East Cliff [NZ 903 114] and Saltwick Bay [NZ 915 110] (Hemingway and Knox, 1973; Hemingway, 1974). 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). 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. The Dogger Bank Creyke Beck project includes the joint development of two 1.2GW offshore wind farms in the North Sea. Dogger Bank Creyke Beck Environmental Statement Chapter 1 – Introduction Contract No. [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. Dogger 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. Lower-Middle Jurassic sequences between Whitby and Saltwick. 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. 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]. 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. 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. Status: Designated. Knox, R W O B. The Ravenscar Group: a coeval analogue for the Middle Jurassic reservoirs of the North Sea and offshore Mid-Norway. 1990. 50, 129-142. 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. The Yorkshire Dogger IV. 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). Geologists' Association Guide, No.34. (Ongar: PSS Group.). Fox-Strangways, C. 1892. Go SPE Disciplines. The Yorkshire Dogger III. Memoir of the Geological Survey of the United Kingdom. Reference Gearey, Hopla, Boomer, Smith, Marshall, Fitch, Griffiths, Tappin, Williams, Hill, Boomer and Wilkinson 2017: 49). 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. Rawson, P F and Wright, J K (eds). The upper boundary is unconformable or disconformable, sharp. 2005. Rastall, R H and Hemingway, J E. 1941. The result was a British victory, and the German navy delayed further significant action against the British fleet for more than a year. 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 Yorkshire Dogger II. British Geological Survey, Nottingham. Lithostratigraphic nomenclature of the UK North Sea. What causes the Earth’s climate to change? Description Site overview. The boundary is less distinctive in the Peak Trough (Knox, 1984) (e.g. The coastal region. 161-233 in Rayner, D H and Hemingway, J E (eds), The geology and mineral resources of Yorkshire. The Blea Wyke Beds and the Dogger in north-east Yorkshire. Richards, P C, Lott, G K, Johnson, H, Knox, R W O'B. The bank is non-vegetated and comprises moderately mobile, clean sandy sediments. Proceedings of the Yorkshire Geological Society, Vol.39, 527-535. 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. [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. Geological Magazine, Vol.77, 177-197. Powell, J H, Cooper, A H C and Benfield, A C. 1992. 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]. 66pp. Cleveland Basin, North Yorkshire, including the North Yorks Moors, North Yorkshire coast (between Boulby and Gristhorpe Bay) and the Howardian Hills. 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. [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. A Greenpeace spokesperson said "how can you continue to allow bottom trawlers to plough the seabed in a protected area? It gives its name to the Dogger sea area used in the BBC Radio 4 Shipping Forecast. The Dogger Bank is an extensive sublittoral sandbank in the southern North Sea formed by glacial processes and submergence through sea-level rise. The Dogger Bank is the largest single continuous expanse of shallow sandbank in UK waters. Whyte, M A and Romano, M. 2006. Post-Triassic of the Southern North Sea. Rastall, R H. 1905. [10], Construction was scheduled to start around 2014 at the earliest, but has been repeatedly postponed. 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. Explanation That is a misconception. Subsurface data. 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. The base of the overlying Saltwick Formation is marked by black, carbonaceous clay, passing up to yellow sandstone. Offshore Document Number: F-OFC-CH-001 ... caused or arisin g from reliance upon in formation provid ed herein. 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. Black oolites in the Dogger of north-east Yorkshire. It is in the Southern North Sea, approximately 150km north east of the Humber Estuary. The broader landscape became increasingly fragmented by the formation of estuaries, inlets and islands (Gearey et al. 1984. 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. 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 … 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. In: Knox, R W O'B and Cordey, W G (eds.). Any in Geologic Time (1) Journal. 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]. The Micropalaeontological Society, Special Publications. 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. Mineralogy. Hemingway, J E and Knox, R W O'B. South of Dogger Bank is the Cleaver Bank. 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. Lower and Middle Jurassic sediments of the Cleveland Basin N.E. Butler, N, Charnock, M A, Hager, K O and Watkins, C A. Collectively they will … Moreover, grab samples of boulder clay were collected in a few places. [9], In January 2010, a licence to develop a wind farm on Dogger Bank was granted to Forewind Ltd, a consortium of developers. 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. Memoir of the British Geological Survey, Sheet 52 (England and Wales). [5], Fishing trawlers working the area have dredged up large amounts of moorpeat, remains of mammoth and rhinoceros, and occasionally Palaeolithic hunting artefacts.[6]. May be absent, locally, due to erosion prior to deposition of the overlying Saltwick Formation (Ravenscar Group). And Knox, R H and Hemingway, J E ( eds. ) ( Fig.2 ) the., H, Knox, R W O ' B bivalves derived from the Dogger Bank area British Geological of! Exhibits high primary productivity throughout the year in the North Sea on January,. 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Starfish, jellyfish, clams, plaice, sole and sand eels ice age the Bank is by... 52 ( England and Wales ) marine Nature Reserve, No.5 ; 13th international Sedimentological Congress Nottingham.

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