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. South of Dogger Bank is the Cleaver Bank. 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 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. 158-164 in Scrutton, C T and Powell, J H (eds), Yorkshire Rocks and Landscapes - A Field Guide, 3rd Edition, Yorkshire Geological Society. The bank is non-vegetated and comprises moderately mobile, clean sandy sediments. 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]. Offshore Document Number: F-OFC-CH-001 ... caused or arisin g from reliance upon in formation provid ed herein. The Dogger Bank is an extensive sublittoral sandbank in the southern North Sea formed by glacial processes and submergence through sea-level rise. It is in the Southern North Sea, approximately 150km north east of the Humber Estuary. The result was a British victory, and the German navy delayed further significant action against the British fleet for more than a year. Collectively they will … Cleveland Basin, North Yorkshire, including the North Yorks Moors, North Yorkshire coast (between Boulby and Gristhorpe Bay) and the Howardian Hills. 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. Geologists' Association Guide, No.34. 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. Post-Triassic of the Southern North Sea. A 12,000 sq km (4,600 sq mile) area … 357-361). Marine Geol., 3 (1965) 245-262 256 H.J. .... [it] is the equivalent to allowing bulldozers to plough through a protected forest. Proceedings of the Yorkshire Geological Society, Vol.39, 527-535. The result was a British victory, and the German navy delayed further significant action against the British fleet for more than a year. 45, 99-108. Battle of Dogger Bank, naval engagement between British and German battle cruisers during World War I. Field Excursion Guide, No.5; 13th International Sedimentological Congress, Nottingham, UK. Geology of the country around Thirsk. Lower-Middle Jurassic sequences between Whitby and Saltwick. 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. (Whitby.). Highly variable and heterolithic with substantial lateral interdigitation and lithofacies changes. Proceedings of the Yorkshire Geological Society, Vol. 66pp. Green electricity tariffs may not actually be that green, says Which? 1993. 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 The Blea Wyke Sandstone Formation (Jurassic, Toarcian) of Rosedale, North Yorkshire, UK. In: Knox, R W O'B and Cordey, W G (eds.) [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. 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). Rastall, R H and Hemingway, J E. 1941. England: Shallow marine and paralic facies seen in their sequence stratigraphic context. The Dogger Bank is the largest single continuous expanse of shallow sandbank in UK waters. [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. Young, G. 1817. 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. Geological Magazine, Vol.80, 209-230. Geological Magazine, Vol.86, 201-225, 265-278. Battle of Dogger Bank, naval engagement between British and German battle cruisers during World War I. 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). Go SPE Disciplines. Data and Information on the Dutch Subsurface. Any in SPE Disciplines (3) Geologic Time. 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. Clasts in the Dogger Formation include mudstone pebbles, and fragments of ammonites and bivalves derived from the underlying Alum Shale Member. Rastall, R H and Hemingway, J E. 1939. 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