It was fought near Dogger Bank in the North Sea on January 24, 1915. Offshore Document Number: F-OFC-CH-001 ... caused or arisin g from reliance upon in formation provid ed herein. England: Shallow marine and paralic facies seen in their sequence stratigraphic context. 3. 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. 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. The researchers’ paper explains “The broader landscape became increasingly fragmented by the formation of estuaries, inlets, and islands. [10], Construction was scheduled to start around 2014 at the earliest, but has been repeatedly postponed. In: Knox, R W O'B and Cordey, W G (eds.). The result was a British victory, and the German navy delayed further significant action against the British fleet for more than a year. Concerns had been raised when a supertrawler had been seen off the Yorkshire coast. Lower Eskdale. It gives its name to the Dogger sea area used in the BBC Radio 4 Shipping Forecast. Young, T P. 1994. The Dogger Bank Creyke Beck project includes the joint development of two 1.2GW offshore wind farms in the North Sea. The Dogger Bank is an extensive sublittoral sandbank in the southern North Sea formed by glacial processes and submergence through sea-level rise. Dogger Bank is set to be the largest wind farm in the world with a combined capacity of 3.6GW. Exposure at the base of the cliff, west of Saltwick Bay [NZ 908 113], south-east of Whitby, North Yorkshire. 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. Research Article A great wave: the Storegga tsunami and the end of Doggerland? 161-233 in Rayner, D H and Hemingway, J E (eds), The geology and mineral resources of Yorkshire. 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 Jurassic Rocks of Britain, Vol.1. The lithofacies variation of the Dogger Formation makes selection of a type section difficult. 50, 129-142. Go SPE Disciplines. 2005. Rastall, R H and Hemingway, J E. 1943. Fox-Strangways, C. 1892. Any in SPE Disciplines (3) Geologic Time. Geological Magazine, Vol.78, 351-370. Lithostratigraphic nomenclature of the UK North Sea. [citation needed]. 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). 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. 357-361). Lithostratigraphical nomenclature of the Middle Jurassic strata of the Yorkshire Basin of north-east England. The Basal Dogger Bank comprises a series of discrete bank-like deposits (Fig. That is a misconception. Green electricity tariffs may not actually be that green, says Which? 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. Battle of Dogger Bank, naval engagement between British and German battle cruisers during World War I. Dogger Field Excursion Guide, No.5; 13th International Sedimentological Congress, Nottingham, UK. 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). Proceedings of the Yorkshire Geological Society, Vol.22, 265-279. Rastall, R H. 1905. British Geological Survey, Nottingham. Lott, G K and Knox, R W O'B. The boundary is less distinctive in the Peak Trough (Knox, 1984) (e.g. Jurassic. 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 type section is located between Whitby East Cliff [NZ 903 114] and Saltwick Bay [NZ 915 110] (Hemingway and Knox, 1973; Hemingway, 1974). 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). [7] Proceedings of the Yorkshire Geological Society, Vol.39, 527-535. [2] The water depth ranges from 15 to 36 metres (50 to 120 ft), about 20 metres (65 ft) shallower than the surrounding sea. 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. elongated, rounded or irregular ‘mound’ shapes) which may arise from horizontal or sloping plains of sandy sediment. Subsurface data. Battle of Dogger Bank, naval engagement between British and German battle cruisers during World War I. Richards, P C, Lott, G K, Johnson, H, 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. 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). 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. 43-53 in Powell, A J and Riding, J B (eds), Recent Developments in Applied Biostratigraphy. Dogger Bank Creyke Beck Environmental Statement Chapter 1 – Introduction Contract No. "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 … 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 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. Upper Eskdale. 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 Dogger Bank is the largest single continuous expanse of shallow sandbank in UK waters. Although the rate of MDAC formation is unknown, examples of leaves and anthropogenic material (industrial slag) partially encrusted in MDAC indicate that formation occurs on a human, rather than a geological, time scale (Andrews, 1988; Judd et al., submitted). The bank is an important fishing area, with cod and herring being caught in large numbers. Collectively they will … 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.’” 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. The broader landscape became increasingly fragmented by the formation of estuaries, inlets and islands (Gearey et al. The Yorkshire Dogger II. 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. Whyte, M A and Romano, M. 2006. 7. (Leeds: Yorkshire Geological Society.). Memoir of the British Geological Survey, Sheet 52 (England and Wales). (-208). 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. 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 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. Highlight matches. The base of the overlying Saltwick Formation is marked by black, carbonaceous clay, passing up to yellow sandstone. Dogger Bank SAC. (Ongar: PSS Group.). The Micropalaeontological Society, Special Publications. Hoofdnavigatie. Status: Designated. Rosedale and Farndale. 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. Data and Information on the Dutch Subsurface. 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. What causes the Earth’s climate to change? About us; Report back; Contact; FAQ; News; Dutch; English 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. Marine Geol., 3 (1965) 245-262 256 H.J. 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). OnePetro (3) Date. 45, 99-108. The Dogger Bank is an extensive sublittoral sandbank in the southern North Sea formed by glacial processes and submergence through sea-level rise. Proceedings of the Yorkshire Geological Society, Vol. Dogger Bank is an important habitat for crabs, brittlestar starfish, jellyfish, clams, plaice, sole and sand eels. 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 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 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… Moreover, grab samples of boulder clay were collected in a few places. 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. 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. “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. 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). 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. Post-Triassic of the Southern North Sea. 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). Quarterly Journal of the Geological Society, London, Vol.61, 441-460. 2). Rastall, R H and Hemingway, J E. 1949. Lower-Middle Jurassic sequences between Whitby and Saltwick. Topmenu. Jurassic of the Central and Northern North Sea. 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]. Geologists' Association Guide, No.34. 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. A history of Whitby and Streoneshalh Abbey. 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]. Earlier than January, 2015 (2) 2017 (1) to. 1994. May be absent, locally, due to erosion prior to deposition of the overlying Saltwick Formation (Ravenscar Group). Clasts in the Dogger Formation include mudstone pebbles, and fragments of ammonites and bivalves derived from the underlying Alum Shale Member. Description Site overview. South of Dogger Bank is the Cleaver Bank. A 12,000 sq km (4,600 sq mile) area … Yorkshire. Lower and Middle Jurassic sediments of the Cleveland Basin N.E. 1993. 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"). Cleveland Basin, North Yorkshire, including the North Yorks Moors, North Yorkshire coast (between Boulby and Gristhorpe Bay) and the Howardian Hills. 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 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. Geological Magazine, Vol.77, 177-197. Dogger Bank Creyke Beck A and B would be built 77 miles (125km) off the Yorkshire coast. 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. Until the middle Pleistocene, Great Britain was a peninsula of Europe, connected by the massive chalk Weald–Artois Anticline across the Straits of Dover. Computer Code: DBNK: Preferred Map Code: notEntered : Status Code: Pending Upgrade : Age range: Marine Isotope Stage 3 (QMIS003) — Marine Isotope Stage 2 (QMIS002) Lithological Description: none recorded or not applicable: Definition of … Hemingway, J E and Knox, R W O'B. The action undertaken by Greenpeace had support from some of those in the fishing trade. 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. Mineralogy. At the time of deposition, clastic sediments above the salt are uncompacted, contain siginficant pore space, and have a lower density than the salt. 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