Researchers from Kobe University, working with the Japan Agency for Marine-Earth Science and Technology (JAMSTEC), used airgun arrays to send seismic pulses through the crust beneath the seafloor around the mostly underwater Kikai caldera, recording the waves with ocean-bottom seismometers. Because seismic waves travel differently through solid rock and molten material, the measurements allowed the team to map structures that cannot be observed directly.
The survey revealed a substantial region containing a high proportion of magma directly beneath the site of Kikai's giant eruption roughly 7,300 years ago. 'Due to its extent and location it is clear that this is in fact the same magma reservoir as in the previous eruption,' said Nobukazu Seama, a Kobe University geophysicist.
The magma now stored there does not appear to be leftover material from that ancient blast. A new lava dome has been developing near the centre of the caldera over approximately the past 3,900 years, and chemical analyses show that material from the dome and other recent activity differs in composition from the giant eruption's output. 'This means that the magma that is now present in the magma reservoir under the lava dome is likely newly injected magma,' Seama said.
The findings, published in Communications Earth & Environment, suggest the reservoir is being recharged by new injections of molten rock from deeper within the crust or mantle. Kikai's underwater location aided the work. 'The underwater location allows us to implement systematic, large-scale surveys,' Seama said.
The recharge process does not mean another catastrophic eruption is imminent, the researchers stress. Rather, it shows how a giant volcanic system can gradually rebuild its magma supply over thousands of years, a step toward understanding how such eruptions become possible. 'We must understand how such large quantities of magma can accumulate to understand how giant caldera eruptions occur,' Seama said.
The team says the re-injection model is consistent with the existence of large shallow magma reservoirs beneath other giant calderas, including Yellowstone in the United States and Toba in Indonesia, and hopes to refine its seismic techniques to track magma movement in greater detail. 'Our ultimate goal is to become better able to monitor the crucial indicators of future giant eruptions.'
