Scientists have confirmed for the first time that radical changes of one volcano in southern Japan was the direct result of an erupting volcano 22 kilometres (13.7 miles) away.
The observations from the two volcanos–Aira caldera and Kirishima–show that the two were connected through a common subterranean magma source in the months leading up to the 2011 eruption of Kirishima.
The Japanese cities of Kirishima and Kagoshima lie directly on the border of the Aira caldera, one of the most active, hazardous, and closely monitored volcanoes in southern Japan. Identifying how volcanoes interact is critical to determine if and how an eruption can influence the activity of a distant volcano or raise the threat of a new strong explosive event.
The research team from the University of Miami’s (UM) Rosenstiel School of Marine and Atmospheric Science and Florida International University analyzed deformation data from 32 permanent GPS stations in the region to identify the existence of a common magma reservoir that connected the two volcanoes.
Leading up to the eruption of Kirishima, which is located in the densely-populated Kagoshima region, the Aira caldera stopped inflating, which experts took as a sign that the volcano was at rest. The results from this new study, however, indicated that the opposite was happening–the magma chamber inside Aira began to deflate temporarily while Kirishima was erupting and resumed shortly after the activity at Kirishima stopped.
“We observed a radical change in the behaviour of Aira before and after the eruption of its neighbour Kirishima,” said Elodie Brothelande, a postdoctoral researcher at the UM Rosenstiel School and lead author of the study. “The only way to explain this interaction is the existence of a connection between the two plumbing systems of the volcanoes at depth.”
Prior to this new study, scientists had geological records of volcanoes erupting or collapsing at the same time, but this is the first example of an unambiguous connection between volcanoes that allowed scientists to study the underlying mechanisms involved. The findings confirm that volcanoes with no distinct connection at the surface can be part of a giant magmatic system at depth.
“To what extend magmatic systems are connected is an important question in terms of the hazards,” said Falk Amelung, professor of geophysics at the UM Rosenstiel School and coauthor of the study. “Is there a lot of magma underground and can one eruption trigger another volcano? Up until now, there was little or no evidence of distinct connections.”
“Eruption forecasting is crucial, especially in densely populated volcanic areas,” said Brothelande. “Now, we know that a change in behaviour can be the direct consequence of the activity of its neighbour Kirishima.”
The findings also illustrate that large volcanic systems such as Aira caldera can respond to smaller eruptions at nearby volcanoes if fed from a common deep reservoir but not all the time, since magma pathways open and close periodically.
“Now, we have to look whether this connection is particular for these volcanoes in southeastern Japan or are widespread and occur around the world,” said Amelung.
Header Image – Kirishima Volcanic Field – Credit: Robert Simmon – NASA Earth Observatory
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