A team of scientists studying last years eruption of Axial Seamount now says that the undersea volcano some 250 miles off the Oregon coast gave off clear signals hours before the eruption.
The findings, plus those from scientists who mapped the lava flow, are published this week in three separate articles in the journal Nature Geoscience.
“Our data suggest that access to real-time seismic data, projected to be available in the near future, might facilitate short-term forecasting and provide sufficient lead time to prepare… instrumentation before future intrusion and eruption events,” one of the published reports states. David Butterfield, an oceanographer with the Joint Institute for the Study of the Atmosphere and Ocean at UW, is a co-author of the paper and Bob Dziak, Oregon State University, is the lead author.
The researchers also collected valuable information about the 2011 eruption — precisely mapping the extent and thickness of the lava flows, calculating the volume of lava and identifying eruptive fissures — by comparing data collected before and after the eruption.
“One of the most surprising discoveries was that of numerous ‘snow blowers’ at the summit of the volcano,” said Deborah Kelley, a UW oceanographer who led the expedition that mapped the eruption with UW oceanographer John Delaney. Kelley and Alden Denny, a graduate student in the UW School of Oceanography and the leader of the mapping effort, are co-authors of one of the papers. David Caress, Monterey Bay Aquarium Research Institute, is lead author.
So-called snow blower vents release microorganisms that are believed to bloom in the subseafloor after an eruption and which are then released into the overlying ocean where they look like gently falling snow.
The researchers found that the flow extended nearly two miles across the summit of Axial Seamount and over five miles in length. It reached a thickness of 450 feet in some places on the flanks of the volcano.
By examining the ground deformation throughout the eruption cycle, researchers who wrote the third paper conclude that the next eruption could occur as early as 2018. Butterfield and UW oceanographer Marv Lilley are co-authors on the paper, with Bill Chadwick, OSU, as lead author.
The eruption was discovered during an expedition that was part of the New Millennium Observatory, a National Oceanic and Atmospheric Administration and Pacific Marine Environmental Laboratory project, which has monitored Axial Seamount since 1997. Butterfield, Chadwick and Lilley noticed that the seafloor had changed in well-known locations, and found instruments partially covered by new lava flows. They alerted a Monterey Bay Aquarium Research Institute ship working in the area, as well as Delaney and Kelley so that the whole community would have the chance to document this decadal event.
Delaney, Kelley and many others at UW are charged with designing and building the U.S.’s first regional cabled ocean observatory off the coast of Oregon that encompasses the Axial Seamount. This submarine network will bring real-time data to the Internet, 24/7. It is part of the National Science Foundations Ocean Observatories Initiative.
The research published this week was funded by the National Science Foundation, the National Oceanic and Atmospheric Administration and the Monterey Bay Aquarium Research Institute.