Ka mua, ka muri – Walking backwards into the future
Looking to the past to inform the future – historical events on the Hikurangi subduction zone New Zealand’s geological setting…
Two observatories give us stereo vision inside the slow slip zone
http:// Click on the location icons to learn more about each site. The Google Map may not work in all…
Seamounts – are they an important piece of the slow slip puzzle?
As we mentioned in our last blog, Site U1520 sits at the base of Tūranganui Knoll. This is an isolated…
The observatory is like a Russian Doll
The stages of installing New Zealand’s first observatory To gain a window into this previously inaccessible environment, we are taking…
Follow our journey to NZ’s largest fault
The Google Map may not work in all web browsers – if you have having trouble use Google Chrome. We…
Live science: first results of ocean drilling 362 expedition
When earthquakes happen in the ocean, they can displace huge volumes of water and cause tsunamis. This was the case…
The Earthquake that Triggered Expedition 362
In 2004, a magnitude 9.2 earthquake struck the northern Sumatra region and triggered a tsunami that inundated the Indian Ocean…