Evaluating earthquake hazards using liquefied volcanic-ash layers in lakes
The Tephra Seismites team at Waikato held a half-day meeting today to present progress on different aspects of the project, and discuss next steps. Josh presented preliminary results from paleoseismic trenching and geomorphology of the Te Puninga Fault segment, Hamilton lowlands. Richard, in his talk on ‘Soft sediment deformation structures (SSDS) in Rotoroa/Hamilton Lake’, presented observations … Continue reading Tephra Seismites group seminars
A short newsletter on research progress was recently emailed to partners, supporters and stakeholders, and can also be viewed below. If you’d like to receive any future updates directly, please feel free to contact us.
At the start of June, the team met at Hamilton Gardens for a wānanga led by Wiremu Puke (Ngāti Wairere, Ngāti Porou). This began with an introduction to mātauranga Māori in geosciences research – particularly as it relates to Ngāti Wairere, as mana whenua for much of the area in which we are working. Wiremu … Continue reading Wānanga with Wiremu Puke and CT scanning update
Liquefied volcanic-ash layers (‘tephra seismites’) preserved in lake sediments have never been reported. In northern New Zealand we have identified at least four such seismites in tephra-bearing lakes aged ~20,000 years in the Hamilton Basin. Our aim is to use this unique opportunity to develop a novel methodology to evaluate the frequency, possible magnitude, and likely locations of major earthquakes for the past 20,000 years in the basin. Click here to continue