Late Weichselian glaciation history of the northern North Sea
Version of Record online: 16 JAN 2008
Volume 23, Issue 1, pages 1–13, March 1994
How to Cite
SEJRUP, H. P., HAFLIDASON, H., AARSETH, I., KING, E., FORSBERG, C. F., LONG, D. and ROKOENGEN, K. (1994), Late Weichselian glaciation history of the northern North Sea. Boreas, 23: 1–13. doi: 10.1111/j.1502-3885.1994.tb00581.x
- Issue online: 16 JAN 2008
- Version of Record online: 16 JAN 2008
- revised 20th November, 1993.
Based on new data from the Fladen, Sleipner and Troll areas, combined with earlier published results, a glaciation curve for the Late Weichselian in the northern North Sea is constructed. The youngest date on marine sedimentation prior to the late Weichselian maximum ice extent is 29.4 ka BP. At this time the North Sea and probably large parts of southern Norway were deglaciated (corresponding to the Alesund interstadial in western Norway). In a period between 29.4 and c. 22 ka BP, the northern North Sea experienced its maximum Weichselian glaciation with a coalescing British and Scandinavian ice sheet. The first recorded marine inundation is found in the Fladen area where marine sedimentation started close to 22 ka BP. After this the ice fronts receded both to the east and west. The North Sea Plateau, and possibly parts of the Norwegian Trench, were ice-free close to 19.0 ka, and after this a short readvance occurred in this area. This event is correlated with the advance recorded at Dimlington, Yorkshire, and the corresponding climatostratigraphic unit is denoted the Dimlington Stadial (18.5 ka to 15.1 ka). The Norwegian Trench was deglaciated at 15.1 ka in the Troll area. The data from the North Sea, together with the results from Andwa, northern Norway (Vorren et al. 1988; Møller et al. 1992), suggest that the maximum extent of the last glaciation along the NW-European seaboard from the British Isles to northern Norway was prior to c. 22 ka BP.