[10], Construction was scheduled to start around 2014 at the earliest, but has been repeatedly postponed. The base of the overlying Saltwick Formation is marked by black, carbonaceous clay, passing up to yellow sandstone. It gives its name to the Dogger sea area used in the BBC Radio 4 Shipping Forecast. Highlight matches. Young, G. 1817. Powell, J H, Cooper, A H C and Benfield, A C. 1992. 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 is set to be the largest wind farm in the world with a combined capacity of 3.6GW. 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 habitat comprises distinct banks (i.e. 2). Description Site overview. During the last ice age the bank was part of a large landmass connecting Europe and the British Isles, now known as Doggerland. Moreover, grab samples of boulder clay were collected in a few places. Young, T P. 1994. .... [it] is the equivalent to allowing bulldozers to plough through a protected forest. The lithofacies variation of the Dogger Formation makes selection of a type section difficult. Any in SPE Disciplines (3) Geologic Time. elongated, rounded or irregular ‘mound’ shapes) which may arise from horizontal or sloping plains of sandy sediment. 1990. 45, 99-108. Dogger
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. 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. Dogger Bank Formation. The upper boundary is unconformable or disconformable, sharp. [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. Fox-Strangways, C. 1892. 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). Dogger Bank Creyke Beck Environmental Statement Chapter 1 – Introduction Contract No. Earlier than January, 2015 (2) 2017 (1) to. Lower Eskdale. 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. The broader landscape became increasingly fragmented by the formation of estuaries, inlets and islands (Gearey et al. Offshore Document Number: F-OFC-CH-001 ... caused or arisin g from reliance upon in formation provid ed herein. However, the best exposed and familiar sections are those in the ferruginous sandstone and ironstone lithofacies located near Whitby on 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]. Post-Triassic of the Southern North Sea. 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. Lithostratigraphy and depositional history of the late Toarcian sequence at Ravenscar, Yorkshire. 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. Knox, R W O'B, Howard, A S, Powell, J H and van Buchem, F S P. 1991. 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. 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. Any in Geologic Time (1) Journal. 2005. The Dogger Bank is an extensive sublittoral sandbank in the southern North Sea formed by glacial processes and submergence through sea-level rise. [citation needed]. Whyte, M A and Romano, M. 2006. 50, 129-142. Geologists' Association Guide, No.34. Richards, P C, Lott, G K, Johnson, H, Knox, R W O'B. 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). Lower-Middle Jurassic sequences between Whitby and Saltwick. 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… 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. The Ravenscar Group: a coeval analogue for the Middle Jurassic reservoirs of the North Sea and offshore Mid-Norway. Explanation; Quickstart; Subsurface models. In: Knox, R W O'B and Cordey, W G (eds.). [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 Dogger Bank Wind Farm will be the largest offshore wind farm in the world, once all three phases are complete in 2026. and Riding, J B. (Whitby.). The boundary is less distinctive in the Peak Trough (Knox, 1984) (e.g. [9], In January 2010, a licence to develop a wind farm on Dogger Bank was granted to Forewind Ltd, a consortium of developers. Dogger Bank has been identified as an oceanic environment that exhibits high primary productivity throughout the year in the form of phytoplankton. A 12,000 sq km (4,600 sq mile) area … The Micropalaeontological Society, Special Publications. It is in the Southern North Sea, approximately 150km north east of the Humber Estuary. In: Knox, R W O'B and Cordey, W G (eds.) 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. 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. 1973. 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. Go SPE Disciplines. Battle of Dogger Bank, naval engagement between British and German battle cruisers during World War I. Flooded, Sea level rise was as much as 1-2 meters ( 3-6 feet ) century... The Humber Estuary sections are those in the North Sea and offshore Mid-Norway Journal of and. Caught in large numbers fishing trade was as much as 1-2 meters ( feet. 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