Source: GNS Science
New research detailing the risk of a major earthquake at the southern end of the Hikurangi Subduction Zone could help Marlborough and lower North Island residents prepare for “the big one”.
A new study, led by Charlotte Pizer of Victoria University of Wellington, used prehistorical tsunami deposits at Lake Grassmere/Kapara Te Hau to get insight into past earthquakes. This project is a joint study between GNS Science, Durham University and Victoria University of Wellington.
This data, combined with tsunami modelling techniques, shows the probability of an earthquake of at least magnitude 8 on the southern end of the Hikurangi Subduction Zone (HSZ) in the next 50 years is about 26 per cent.
GNS Science’s Kate Clark co-authored the study and says this is the first-time scientists have been able to come up with a probability for large earthquakes for the HSZ.
“Geological records like this are essential for assessing the risk of earthquakes and tsunami, but they’re difficult to obtain at transitional plate boundaries like this,”
The evidence shows that large earthquakes on the subduction zone generate large tsunamis that are likely to impact the lower North Island and upper South Island.
“This research helps us better understand these large fault systems and the likelihood of tsunamis produced by the faults – and the more information we have, the better we can inform local communities about how to be prepared and resilient.”
Victoria University of Wellington’s Dr Jamie Howarth also co-authored the study.
“Knowing more about the risk is a really good thing because it provides the opportunity to better prepare our communities and infrastructure which should now be a priority,” Dr Howarth says.
The paper was published in The Seismic Record, a journal of the Seismological Society of America this week.
Core samples of the sediment layers at Lake Grassmere / Kapara Te Hau showed unusual shell layers, indicating deposits from several large-scale tsunamis, which were caused by large subduction earthquakes in the last 2000 years.
The lake sits on the transitional plate boundary between the Marlborough Fault System and the HSZ. The subduction interface lies 25km below the site, with active faults in close proximity.
“Geological records like this are essential for assessing the risk of earthquakes and tsunami, but they’re difficult to obtain at transitional plate boundaries like this,” Ms Pizer says.
“This is a rare opportunity to gain knowledge from past earthquakes and tsunami sequences – helping us to best prepare for the future.”