“One of the potential scenarios suggested by past experience, and which seismologists have argued is likely in the near future, is an earthquake in the eastern part of the Reykjanes peninsula, possibly of similar magnitude size as the two South Iceland earthquakes in June 2000 and the Ölfus earthquake in May 2008. An event like this could significantly impact the Reykjavík area, although the distance from expected epicentre and fault rupture to the outskirts of the capital would be much greater than the distance to the built environment in South Iceland when earthquakes strike there. Findings from the SERICE project help us to assess seismic risk in the Reykjavík area and other areas of Iceland which could be affected by larger earthquakes,” says Bjarni Bessason, professor of civil and environmental engineering. Together with his colleagues, Bjarni has been working on an extensive research project aimed at developing new tools and models for assessing seismic risk in Iceland.
Icelanders are all too familiar with the potential impact of major earthquakes. The three earthquakes in South Iceland which occurred in 2000 and 2008 caused serious damage to various buildings and infrastructure, as did the earthquakes connected to the volcanic activity in Grindavík in November 2023. In South Iceland, intense ground shaking caused the damage, while in Grindavík it was primarily the openings and differential movements of faults beneath buildings and infrastructure that led to damage. There is a lot to be gained if we can reduce the impact that seismic activity has on infrastructure, which is one of the aims of the project led by Bjarni and his colleagues, professors Rajesh Ruphakety and Sigurður Erlingsson.
Project inspired by the South Iceland earthquakes
The project, entitled Seismic Risk in Iceland (SERICE), began before the recent seismic activity on the Reykjanes peninsula and was inspired by the three South Iceland earthquakes in 2000 and 2008. “The South Iceland Seismic Zone is an area known for seismic activity and is monitored with various measuring equipment. A range of important data was recorded by the Icelandic Meteorological Office during these events. Seismic acceleration time series data was also recorded by the University of Iceland Earthquake Engineering Research Centre,” says Bjarni, explaining that the time series data describes either the ground motion or the seismic responses of selected buildings and bridges during the earthquakes.