"Over the last few years we have started to see the connection between the shallow parts of geothermal fields and the underlying volcanic systems which provide the heat. Results from Rotorua to date and similar research north of Wairakei have enabled us to start to understand how geothermal systems like Rotorua work from tip to toe - from the surface features down to their volcanic roots," Mr Caldwell said.
"As a Crown Research Institute, our job is to provide baseline information that could then stimulate future development. It's been a tremendous help for us to have the additional support from the regional council for this research," he said.
Regional council strategic development group manager Fiona McTavish said as managers of the resource it was important this type of work was undertaken.
"Geothermal is recognised as an important asset for the Bay of Plenty region offering potential to grow the region's economy and social communities. We want to ensure we are utilising the resource as effectively and efficiently as possible for its long-term sustainability, as well as the future development of the region. "
"This work is part of that goal - to understand more about different geothermal systems, their capabilities and potential. With careful management, the resource has capacity for growth in some areas and will continue to provide geothermal energy indefinitely. However, if too much is taken from a system it could be severely damaged," she said.