Scientists have shed more light on a newly identified fault system north of Gisborne – with implications for the region's risk from earthquakes and tsunami.
A new study, led by Dr Nicola Litchfield of GNS Science, suggests that distinctive marine terraces were caused by earthquakes on multiple offshore upper-plate faults.
The team used radiocarbon and other methods to date the ages of marine terraces at two North Island sites, Puatai Beach and the Pakarae River mouth.
Previously, scientists thought the youngest terraces were created at the same time by a rupture in the Hikurangi subduction zone – a major fault area along the boundary of the Pacific and Australian plates- or a single-fault earthquake in the upper plate.
But radiocarbon dating of beach shells and layers of volcanic ash showed the uplift happened at different times.