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. Medieval Treasure Trove Found in Polish Field, New Findings About Prehistoric Easter Island, Research Explains Why Crocodiles Changed so Little Since Age of Dinosaurs, Hominins of Olduvai Gorge Coped With Ecological Changes, How Earth’s Oddest Mammal Got to be so Bizarre, Leaf Fossils Show Severe End-Cretaceous Plant Extinction, Major Drought in Middle Ages Could Have Parallels to Climate Change Today, The Secret Hellfire Club and the Hellfire Caves. WARP Occasional Paper 12. The Doggerland Project", University of Exeter Department of Archaeology; Patterson, W, "Coastal Catastrophe" (paleoclimate research document), University of Saskatchewan Port Royal, originally named Cagway was an English harbour town and base of operations for buccaneers and privateers (pirates) until the great earthquake of 1692. The part we know today as Dogger Bank may have sunk below waves even before the tsunamis; and the part nearest Britain had been reduced to “essentially a big lump of land” off the eastern coast. In addition, settlements with sunken floors, dugout canoes, fish traps and a number of burials in the Rhine/Meuse delta of the Netherlands, and a skull fragment of a Neanderthal, dated at over 40,000 years old dredged from the Middeldiep off the coast of Zeeland. Monument Types 2.1.2 Dogger Bank Creyke Beck will be the first stage of development of the Dogger Bank Zone, and will It is in honour of his early work that the archaeologist Bryony Coles coined the term ‘Doggerland’ to refer to the land now submerged by the North Sea. Named after the Dogger Bank, which in turn was named after the 17th-century Dutch fishing boats called doggers. To the astonishment of the fisherman, the peat contained an ornate barbed antler point used for harpooning fish that dated from between 10,000-4,000 BC. The transition from the Medieval Warm Period to the Little Ice Age was apparently accompanied by severe droughts between 1302 and 1307 in Europe; this preceded the wet and cold phase of the 1310s and the resulting great famine of 1315-21. Its highest point is the submerged Dogger Bank where prehistoric artefacts are occasionally found by fishermen and geologists. Melvyn Bragg and guests discuss the people, plants and animals once living on land now under the North Sea, now called Doggerland after Dogger Bank, inhabited up to … Doggerská lavice (anglicky Dogger Bank) je rozsáhlá písčina v mělké oblasti Severního moře cca 100 km od východního pobřeží Anglie.Rozkládá se na cca 17 600 km², přičemž zabírá asi 260 km ve východozápadním a 97 km v severojižním směru. Bryony J. Coles: Doggerland, a speculative survey. During that period, the British Isles were certainly not British, nor they were islands. It was still populated by humans and animals until the continental shelf off Norway massively collapsed. Entire peoples found themselves displaced as the sea encroached on a region larger than many European countries. Wessex Archaeology was commissioned by Forewind to undertake an archaeological impact assessment for Creyke Beck Project A and Creyke Beck Project B within Tranche A of the Dogger Bank Zone and export cable corridor. Registered Address: HeritageDaily, 41 Belsize Road, Luton, Bedfordshire, England. Geological surveys have suggested that it stretched from where Great Britain's east coast now is to the present-day Netherlands, western coast of Germany, and peninsula of Jutland. British Atlantis: archaeologists begin exploring lost world of Doggerland. Often considered the world's oddest mammal, Australia's beaver-like, duck-billed platypus exhibits an array of bizarre characteristics: it lays eggs instead of giving birth to live babies, sweats milk, has venomous spurs and is even equipped with 10 sex chromosomes. Subsequently, the Dogger Bank formed an emergent plain during the Holocene with a complex meandering river system, associated tributary or distributary channels and lakes, dominating the region. Collectively they will become the world’s largest offshore wind farm. Teōtīhuacān, named by the Nahuatl-speaking Aztecs, and loosely translated as "birthplace of the gods" is an ancient Mesoamerican city located in the Teotihuacan Valley of the Free and Sovereign State of Mexico, in present-day Mexico. "On the origin of the Dogger Bank, in the North Sea". See for example, (S21) and (S22), the latter of which makes specific reference to the Leman and Ower Bank harpoon. ‘The name Doggerland was coined for Dogger Bank, but it applies to any of several periods when the North Sea was land,’ says Richard Bates of the University of St Andrews. The Dogger Bank character area is an important offshore fishing area and part of larger spawning grounds for herring, sprat and sole in addition to being a nursery ground for sprat and whiting. So far 174 peat samples from a large area c. 100 to 300km off the Yorkshire Coast have been recovered and the plant remains including seeds identified within them are indicative of  a range of Early Holocene environments including Sphagnum moss bogs, wooded fens, Phragmites reed and sedge marshlands and freshwater and coastal aquatic habitats. The uplands, comprising the current Dogger Bank, would probably have been cut off , forming Dogger Island, which survived for approximately another millennium. Somewhat later. The Dogger Bank is a large sand bank located in Danish, German, Dutch and UK waters (Figure 1). Over time, the area was flooded by rising sea levels after the last glacial period around 6,500 to 6,200BC. Nov 18, 2013 - Explore Joan Chapman's board " Doggerland ", followed by 158 people on Pinterest. ‘Around 20,000 years ago, there was a ‘maximum’ – although part of this area would have been covered with ice. Geological magazine 96 (1): 33–34. Doggerland eventually became submerged leaving only Dogger Bank, a possible moraine (accumulation of glacial debris) an island until around 5000BC when Dogger Bank also succumbed to the sea. A research report on ancient offshore peat deposits recovered from the Dogger Bank written by Wessex Archaeology has been published on The Crown Estate website. The geologist Clement Reid first described the ‘moorlog’ in detail in his book Submerged Forests published in 1913. Doggerland (also called Dogger Littoral) was an area of land, now submerged beneath the southern North Sea, that connected Great Britain to continental Europe.It was flooded by rising sea levels around 6500–6200 BC. The Dogger Bank incident occurred on the night of 21/22 October 1904 when the Baltic Fleet of the Imperial Russian Navy mistook a British trawler fleet in the Dogger Bank area for Imperial Japanese Navy torpedo boats and fired on them. A recent theory among archaeologists suggests that much of the remaining coast and low-lying islands was flooded around 6225–6170 BC by a mega-tsunami caused by the Storegga Slide. In: Proceedings of the Prehistoric Society. Archaeology discoveries within the Doggerland region have included the remains of mammoth, rhinoceros and hunting artefacts that have all been dredged up from the sea floor of the North Sea. The red line marks Dogger Bank, which is most likely a moraine formed in the Pleistocene Which brings the story to the last major Ice Age, which was coming to its close roughly 12,000 years ago. (The Storegga slide was a landslide that involved an estimated 180 mile length of coastal shelf in the Norwegian Sea which caused a large tsunami in the North Atlantic Ocean). The water depth ranges from 18 to 63 metres (59 to 206 feet). Archaeologists call that vanished plain Doggerland, after the North Sea sandbank and occasional shipping hazard Dogger Bank. 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