It was fought near Dogger Bank in the North Sea on January 24, 1915. The result was a British victory, and the German navy delayed further significant action against the British fleet for more than a year. Sedimentation of the Aalenian rocks of Yorkshire. A 12,000 sq km (4,600 sq mile) area … 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 type section is located between Whitby East Cliff [NZ 903 114] and Saltwick Bay [NZ 915 110] (Hemingway and Knox, 1973; Hemingway, 1974). Richards, P C, Lott, G K, Johnson, H, Knox, R W O'B. The Dogger Bank is an extensive sublittoral sandbank in the southern North Sea formed by glacial processes and submergence through sea-level rise. Concerns had been raised when a supertrawler had been seen off the Yorkshire coast. The bank is an important fishing area, with cod and herring being caught in large numbers. Geologists' Association Guide, No.34. May be absent, locally, due to erosion prior to deposition of the overlying Saltwick Formation (Ravenscar Group). Hoofdnavigatie. 3. 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. Exposure at the base of the cliff, west of Saltwick Bay [NZ 908 113], south-east of Whitby, North Yorkshire. 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). 161-233 in Rayner, D H and Hemingway, J E (eds), The geology and mineral resources of Yorkshire. 2005. 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. 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). Highly variable and heterolithic with substantial lateral interdigitation and lithofacies changes. 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). 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… Dogger Bank Peer Reviewed. Offshore Document Number: F-OFC-CH-001 ... caused or arisin g from reliance upon in formation provid ed herein. Fluid and Rock Processes Laboratory Cluster, Rock Volume Characterisation Laboratory Cluster, Integrated resource management in Eastern Africa, Donations and loans of materials collections. Quarterly Journal of the Geological Society, London, Vol.61, 441-460. 50, 129-142. 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. Worms burrow into the sand and then become a food source for larger animals, … The upper boundary is unconformable or disconformable, sharp. Knox, R W O B. Clasts in the Dogger Formation include mudstone pebbles, and fragments of ammonites and bivalves derived from the underlying Alum Shale Member. British Geological Survey, Nottingham. Lithostratigraphical nomenclature of the Middle Jurassic strata of the Yorkshire Basin of north-east England. Field Excursion Guide, No.5; 13th International Sedimentological Congress, Nottingham, UK. 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. A sediment survey carried out on board H.M.S. Read more. Battle of Dogger Bank, naval engagement between British and German battle cruisers during World War I. A history of Whitby and Streoneshalh Abbey. British Geological Survey, Nottingham. 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. On the higher grounds, the Dogger Bank and Cleaver Bank (Fig.2), are patches covered with pebbles. 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. These indicate that the substratum of the Dogger Bank consists of moraine ridges belonging presumably to the Weichsel glaciation, the last Pleistocene glaciation. [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. 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. At the lower boundary, sand-filled burrows extend downwards from the Dogger Formation to the underlying mudstone. The Micropalaeontological Society, Special Publications. Dogger Bank Special Area of Conservation shown in red. The researchers’ paper explains “The broader landscape became increasingly fragmented by the formation of estuaries, inlets, and islands. Dogger Bank Creyke Beck A and B would be built 77 miles (125km) off the Yorkshire coast. 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. It was fought near Dogger Bank in the North Sea on January 24, 1915. 158-164 in Scrutton, C T and Powell, J H (eds), Yorkshire Rocks and Landscapes - A Field Guide, 3rd Edition, Yorkshire Geological Society. 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). 1984. In: Knox, R W O'B and Cordey, W G (eds.). Dogger Bank SAC. 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. Rawson, P F and Wright, J K (eds). 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 Basal Dogger Bank comprises a series of discrete bank-like deposits (Fig. 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. The habitat comprises distinct banks (i.e. Yorkshire. Green electricity tariffs may not actually be that green, says Which? It gives its name to the Dogger sea area used in the BBC Radio 4 Shipping Forecast. 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]. Memoir of the British Geological Survey, Sheet 52 (England and Wales). Until the middle Pleistocene, Great Britain was a peninsula of Europe, connected by the massive chalk Weald–Artois Anticline across the Straits of Dover. 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. Explanation Black oolites in the Dogger of north-east Yorkshire. 1990. 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. 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