In the graphic you can see how the set up works. The boat tows the seismic source (either the low frequency 'boomer' or the higher frequency 'CHIRP'). This sends sound waves down through the water and into the rocks below. These signals get reflected back up from the different rock layers and are received by the hydrophones in the cable floating behind the boat. Lower frequency sound waves can penetrate deeper into the rocks, whilst higher frequencies give shallower penetration, but provide more detail.
During our survey we are using the boomer to give an overall view of the lake floor first. We are then using CHIRP to go over specific locations that we want to observe in more detail, such as the sites of any terraces and particular volcanic structures.
On this map of the lake floor, you can see how the seismic lines criss cross the lake back and forth to give overall coverage. This is the planning map, but sometimes the scientists change their plans during the survey, depending on the time they have available, and how well things are progressing.
There has been a great deal of media interest in our investigation of Lake Rotomahana. In the last photo Cornel de Ronde is being interviewed by John Hudson with cameraman Clint Bruce for TV1's Sunday programme.
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