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A map showing Viking-Bergen island to the north of Doggerland 10,000 BCE. From approximately 15,500 to 13,600 years before present (BP), sea levels in the region were lower by 100 to 110 metres (330 to 360 ft), and possibly more than 140 metres (460 ft). [1] At this time, Viking-Bergen would have been an island surrounded by a shallow sea.
Printable version; In other projects Wikidata item; Appearance. ... Viking-Bergen Banks This page was last edited on 17 December 2016, at 00:42 (UTC). ...
Print/export Download as PDF; Printable version; ... Viking-Bergen Banks; W. Walters Shoals This page was last edited on 19 December 2017, at 22:11 ...
Map of Doggerland at its near maximum extent c. 10,000 years Before Present (~8,000 BCE) (top left) and its subsequent disintegration by 7,000 BP (~5,000 BCE). Doggerland was an area of land in Northern Europe, now submerged beneath the southern North Sea.
Printable version; Page information; ... Changed colours to uniform all the palaeogeographic maps: 00:52, 22 February 2009 ... Viking-Bergen Banks;
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The Dogger Bank. The seabed is separated into three bathymetric areas, the Norwegian Trench and the north and south North Sea separated by the Dogger Bank. [3] For the most part, the sea lies on the European continental shelf. The only exception is the Norwegian trench, which reaches from the Stad peninsula in Sogn og Fjordane to the Oslofjord.