Titlebook: Seismicity and Seismic Risk in the Offshore North Sea Area; Proceedings of the N A. Reinier Ritsema,Aybars Gürpinar Conference proceedings

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Commentaires sur une Carte seismique de la Mer du nord et de la Mer de Norvegemagnitude definition..Apart from the June 7, 1931 earthquake (the most important computed event), the seismicity of the North Sea and Norwegian Sea. is located within a stripe paralleling the coast of Norway..La base de la carte séismique présentée est constituée par un extrait de la carte générale

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Tidal Research and Seismicitybservations. Oceanic tides even may be more important than solid earth tides provided their loading effects. While instrumentation should more and more be set towards real time observations, it should be great if more young scientists could be involved in seismological research in Europe.

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Changes of Relative Mean Sea-Level and of Mean Tidal Amplitude Along the Dutch Coastlocations of these gauges are shown on the map in fig. 8. Figure 9 allows the comparison of the stations concerned. The linear variation (relative sea-level rise) varies between 16 and 22 cm per century and appears to be higher in the southern part of the Dutch coast than in the northern part (table

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Possible Neotectonic Fault Movements in Norwaystigations carried out at Yrkje indicate possible postglacial movements of 6–13m vertically across a NNE-SSE trending fault. In addition, investigations of possible fault movements are being carried out based on geophysical surveys of upper sediments along the Skitfjord pipeline trail.

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Some Problems Concerning the Seismicity of the North Sea Area concept aims to the evaluation of earthquake hazard. After having examined the case of the North Sea it is stated that an isoseismal map of the area is still missing and should be undertaken. The occurrence of seismic seawaves in the North Sea has an extremely low probability. Conclusions and recommendations.

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Changes of Relative Mean Sea-Level and of Mean Tidal Amplitude Along the Dutch Coastlocations of these gauges are shown on the map in fig. 8. Figure 9 allows the comparison of the stations concerned. The linear variation (relative sea-level rise) varies between 16 and 22 cm per century and appears to be higher in the southern part of the Dutch coast than in the northern part (table I).