Fluid and Rock Processes Laboratory Cluster, Rock Volume Characterisation Laboratory Cluster, Integrated resource management in Eastern Africa, Donations and loans of materials collections. Yes (1) Source. Dogger Bank is an important habitat for crabs, brittlestar starfish, jellyfish, clams, plaice, sole and sand eels. The oldest of these formations is the Dogger Bank Formation that comprises massive clays, sands and diamicts of glacial origin (Cotterill et al., 2017a), subdivided informally in this study into the Lower and Upper Dogger Bank sub-units. 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. Many explainations of salt domes suggest that the lower density of salt, compared to the density of overlying rock units, is the driving force of salt dome formation. 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. [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. 66pp. Lower-Middle Jurassic sequences between Whitby and Saltwick. 1992. and Riding, J B. 43-53 in Powell, A J and Riding, J B (eds), Recent Developments in Applied Biostratigraphy. The bank was part of a large landmass, now known as Doggerland, which connected Britain to the European mainland until it was flooded some time after the end of the last glacial period. Rastall, R H and Hemingway, J E. 1949. That is a misconception. "[4], Geologically, the feature is most likely a moraine, formed during the Pleistocene. Battle of Dogger Bank, naval engagement between British and German battle cruisers during World War I. Data and Information on the Dutch Subsurface. These indicate that the substratum of the Dogger Bank consists of moraine ridges belonging presumably to the Weichsel glaciation, the last Pleistocene glaciation. The Ravenscar Group: a coeval analogue for the Middle Jurassic reservoirs of the North Sea and offshore Mid-Norway. Collectively they will … [7] 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. 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. 1993. Description Site overview. Memoir of the Geological Survey of the United Kingdom. The action undertaken by Greenpeace had support from some of those in the fishing trade. 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. Rosedale and Farndale. In: Knox, R W O'B and Cordey, W G (eds.) 2nd Edition, 117pp. 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 … Data and Information on the Dutch Subsurface. May be absent, locally, due to erosion prior to deposition of the overlying Saltwick Formation (Ravenscar Group). Lithostratigraphic nomenclature of the UK North Sea. Variable, both locally and regionally; generally about 0.75 to 2m thick on the Yorkshire Coast and in ferruginous sandstone/ironstone lithofacies; limestone and mudstone lithofacies, up to 12.2m locally preserved. Yorkshire. 357-361). Field Excursion Guide, No.5; 13th International Sedimentological Congress, Nottingham, UK. Rawson, P F and Wright, J K (eds). Rastall, R H. 1905. 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. Explanation At the lower boundary, sand-filled burrows extend downwards from the Dogger Formation to the underlying mudstone. Highlight matches. 7. Geological Magazine, Vol.78, 351-370. Green electricity tariffs may not actually be that green, says Which? Any in Geologic Time (1) Journal. Young, G. 1817. Mineralogy. England: Shallow marine and paralic facies seen in their sequence stratigraphic context. 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]. 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. Dogger Bank Formation. The result was a British victory, and the German navy delayed further significant action against the British fleet for more than a year. Black oolites in the Dogger of north-east Yorkshire. [2] At differing times during the last glacial period it was either joined to the mainland or an island. 1973. Hemingway, J E and Knox, R W O'B. 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. Dogger Bank Creyke Beck Environmental Statement Chapter 1 – Introduction Contract No. 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. "Upper" Dogger Bank thick sequence of "Upper" Dogger Bank Formation sediments large scale, Structural interpretation: line 6 moraine ridge composed of deformed "Lower" and "Basal" Dogger Bank sediments detachment at base of the Dogger Bank Formation 500 m 0.025 - 0.050 075 0.100 0.125 0.025 0.050 > 0.075 0.100 0.125 Lower Eskdale. Geological Magazine, Vol.76, 225-233 (273-281). 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