Back to the Seamount – Site 4
If you are having trouble viewing the interactive Google map above please try switching your browser to Chrome. We are…
If you are having trouble viewing the interactive Google map above please try switching your browser to Chrome. We are…
What is seismic reflection imaging? What is a core-log-seismic integration specialist? Glad you asked. Rebecca Bell explains.
Martin is a micro-paleontologist. He identifies, counts and arranges really small creatures on microscope slides and listens to cricket….
As we mentioned in our last blog, Site U1520 sits at the base of Tūranganui Knoll. This is an isolated…
Click on the location icons to read more. The Google Map may not work in all web browsers – if you…
This video shows the first stage of installing the Te Matatike observatory. Here the team is strapping pressure lines to the outside of…
https://www.youtube.com/watch?v=csW9lq7veRY Geologists see sediment cores as a written history, it’s exciting and fascinating. The samples are studied for years, new…
When earthquakes happen in the ocean, they can displace huge volumes of water and cause tsunamis. This was the case…
One of the things that I get to do on this expedition is get to know the scientists. Their curiosity…