Earthquakes and slow slip events may be influenced by mountains on the ocean floor, or “seamounts”, according to new
research co-authored by GNS Science.
A paper published today in Nature Geoscience magazine found that seamounts can have dramatic effects when they get
pulled into a subduction zone.
Subduction zones are where one tectonic plate dives under another - and where the largest and most damaging earthquakes
The Hikurangi Subduction Zone runs along the East Coast of New Zealand, and this new research could help scientists
better understand how seamounts there could influence behaviour.
The research featured in Nature Geoscience used cutting-edge computer modelling techniques to simulate what happens when
seamounts enter a subduction zone.
“When a seamount sinks into a trench, the ground ahead becomes brittle and prone to earthquakes because the water is
squeezed out,” GNS Science’s Susan Ellis says.
“This brittle rock can be a source for earthquakes.
“But in its wake, the seamount leaves softer, wet sediment, which can help dampen or slow down subduction slip.”
Dr Ellis says the weakened rock could be an important factor in slow-slip events – which are like earthquakes, but
happen silently and slowly over weeks or months.
“Our findings show scientists need to carefully monitor what happens around a subducting seamount, so we can better
understand where future quakes might occur.”
The study suggests that subduction of these undersea mountains could influence where earthquakes and slow-motion
earthquakes (slow slip events) occur on subduction zones.
The predictions from the model agree with the locations of offshore tremors and slow slip events observed on the
Hikurangi Subduction Zone offshore Gisborne, where one of these large undersea mountains is subducting.
This study was undertaken in collaboration with scientists from Pennsylvania State University and the University of
It was funded by the United States National Science Foundation and an MBIE Endeavour funded project led by GNS Science
to understand the seismic and tsunami hazard posed by the Hikurangi Subduction Zone.