FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2616551004> ?p ?o ?g. }

• W2616551004 endingPage "303" @default.
• W2616551004 startingPage "285" @default.
• W2616551004 abstract "Due to the need for a national strategy for offshore wind farms in Norway, a small and preliminary joint archaeological and geological research project was conducted. The aim of the investigation was to determine the possibilities for human occupation in the southernmost parts of the Norwegian sector of the North Sea during the Late Glacial and Preboreal periods. The research was in the shallowest area of the Norwegian sector of the continental shelf, south of the Norwegian Trench. By analysing 3D seismic reflection data, several layers with traces of drainage systems and other landforms could be identified in the sediments. These features were, however, mainly situated deep down below the surface of the seabed, and covered by more than 100 m of younger sediments. Their age is therefore uncertain, even if the depth alone indicates that they are much older than the Last Glacial Maximum (LGM). A sediment core through the shallow sea-bed sediments (0–13 m below present sea floor) was analysed for environmental and chronological data. The youngest observed transition, from glacio-lacustrine to marine sediments, was dated to approximately 14,000 cal. BC or the Older Dryas. This indicates that this part of Doggerland was not dry land after the LGM, but was first covered by an ice-dammed lake and later inundated by saltwater from the Atlantic Ocean. The analysis also indicates that the distance from Doggerland to Norway, in the periods when people began to inhabit southern Scandinavia, was far too long to be crossed by boats or on ice. This makes the western coast of Sweden and Bohuslan the most likely bridgehead in the colonisation of Norway. Humans arrived at the Norwegian shores first when a safe and sheltered passage was created between Bohuslan and the Oslo Fjord area, at approximately 9300 cal. BC." @default.
• W2616551004 created "2017-05-26" @default.
• W2616551004 creator A5035651756 @default.
• W2616551004 creator A5068404712 @default.
• W2616551004 creator A5083169974 @default.
• W2616551004 date "2017-01-01" @default.
• W2616551004 modified "2023-09-25" @default.
• W2616551004 title "The Northern Coasts of Doggerland and the Colonisation of Norway at the End of the Ice Age" @default.
• W2616551004 cites W1579624901 @default.
• W2616551004 cites W1964670061 @default.
• W2616551004 cites W1968597789 @default.
• W2616551004 cites W1974944845 @default.
• W2616551004 cites W1992278048 @default.
• W2616551004 cites W2018747394 @default.
• W2616551004 cites W2030421281 @default.
• W2616551004 cites W2062588604 @default.
• W2616551004 cites W2071403721 @default.
• W2616551004 cites W2081734619 @default.
• W2616551004 cites W2092191883 @default.
• W2616551004 cites W2105691658 @default.
• W2616551004 cites W2110449181 @default.
• W2616551004 cites W2111069348 @default.
• W2616551004 cites W2134943946 @default.
• W2616551004 cites W2135362100 @default.
• W2616551004 cites W2166723842 @default.
• W2616551004 cites W2463623565 @default.
• W2616551004 cites W2945417110 @default.
• W2616551004 cites W2946143450 @default.
• W2616551004 cites W2946341190 @default.
• W2616551004 cites W3171869663 @default.
• W2616551004 doi "https://doi.org/10.1007/978-3-319-53160-1_19" @default.
• W2616551004 hasPublicationYear "2017" @default.
• W2616551004 type Work @default.
• W2616551004 sameAs 2616551004 @default.
• W2616551004 citedByCount "2" @default.
• W2616551004 countsByYear W26165510042020 @default.
• W2616551004 crossrefType "book-chapter" @default.
• W2616551004 hasAuthorship W2616551004A5035651756 @default.
• W2616551004 hasAuthorship W2616551004A5068404712 @default.
• W2616551004 hasAuthorship W2616551004A5083169974 @default.
• W2616551004 hasConcept C100970517 @default.
• W2616551004 hasConcept C111368507 @default.
• W2616551004 hasConcept C114793014 @default.
• W2616551004 hasConcept C127313418 @default.
• W2616551004 hasConcept C140345934 @default.
• W2616551004 hasConcept C15739521 @default.
• W2616551004 hasConcept C180705331 @default.
• W2616551004 hasConcept C184751465 @default.
• W2616551004 hasConcept C188291805 @default.
• W2616551004 hasConcept C205649164 @default.
• W2616551004 hasConcept C26099304 @default.
• W2616551004 hasConcept C2776200160 @default.
• W2616551004 hasConcept C33613203 @default.
• W2616551004 hasConceptScore W2616551004C100970517 @default.
• W2616551004 hasConceptScore W2616551004C111368507 @default.
• W2616551004 hasConceptScore W2616551004C114793014 @default.
• W2616551004 hasConceptScore W2616551004C127313418 @default.
• W2616551004 hasConceptScore W2616551004C140345934 @default.
• W2616551004 hasConceptScore W2616551004C15739521 @default.
• W2616551004 hasConceptScore W2616551004C180705331 @default.
• W2616551004 hasConceptScore W2616551004C184751465 @default.
• W2616551004 hasConceptScore W2616551004C188291805 @default.
• W2616551004 hasConceptScore W2616551004C205649164 @default.
• W2616551004 hasConceptScore W2616551004C26099304 @default.
• W2616551004 hasConceptScore W2616551004C2776200160 @default.
• W2616551004 hasConceptScore W2616551004C33613203 @default.
• W2616551004 hasLocation W26165510041 @default.
• W2616551004 hasOpenAccess W2616551004 @default.
• W2616551004 hasPrimaryLocation W26165510041 @default.
• W2616551004 hasRelatedWork W1945918151 @default.
• W2616551004 hasRelatedWork W1968079677 @default.
• W2616551004 hasRelatedWork W2029890633 @default.
• W2616551004 hasRelatedWork W2083175245 @default.
• W2616551004 hasRelatedWork W2170607960 @default.
• W2616551004 hasRelatedWork W21929386 @default.
• W2616551004 hasRelatedWork W2894573434 @default.
• W2616551004 hasRelatedWork W4205549981 @default.
• W2616551004 hasRelatedWork W4237813568 @default.
• W2616551004 hasRelatedWork W298426793 @default.
• W2616551004 isParatext "false" @default.
• W2616551004 isRetracted "false" @default.
• W2616551004 magId "2616551004" @default.
• W2616551004 workType "book-chapter" @default.