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The 2015 Eruption

Category: General Article

Back to Axial Seamount Eruption Response

Sunday, August 16, 2015
Submitted by Bill Chadwick

Summary: The Jason and Sentry Groups completed their overnight preparations to begin an investigation of the marine volcano using underwater robots.

This morning the Jason (our remotely operated underwater vehicle) and Sentry (our autonomous underwater vehicle) Groups completed their overnight navigational calibration north of Axial Seamount’s caldera. We transited to the North Rift Zone and launched AUV Sentry just after lunch. Medea was launched for the Jason Group to test a new winch cable and the rest of the evening was spent in preparation for our first ROV Jason dive, due at midnight tonight!

An exciting part of this expedition is that we are heading out to explore and sample new lava flows at Axial Seamount that are less than 4 months old. How do we know that Axial recently erupted? Because it is now a “wired volcano.” Over the last several years the National Science Foundation has funded the Ocean Observatories Initiative (OOI), which is enabling new ways to study, observe, and understand our oceans. One component of the OOI is a fiber-optic cable network that extends from the Oregon Coast to areas offshore, including Axial Seamount. About a year ago, the University of Washington finished deploying most of the monitoring instruments on this Cabled Array and it started sending data back to shore. On April 24, nearly 8,000 earthquakes were suddenly detected and the seafloor dropped by 2.4 meters (almost 8 feet), signaling that something big was happening at Axial Seamount.

Axial Seamount has two previous known eruptions in 1998 and 2011. What was different this time was that the OOI Cabled Array enabled a community of scientific researchers from many different disciplines to look at the data coming in and debate what it meant, each contributing their own valuable perspectives and interpretations. Often scientists work alone or in small groups, but in this case a diverse group came together in a collaborative way to discuss the event and try to figure out what was happening as it was unfolding. It was exciting!

From the drop in seafloor, it was clear that magma had moved from beneath the summit of the volcano, but it wasn’t obvious at first whether or not it had reached the seafloor to erupt as lava. But over the next few weeks, explosion-like seismic signals were recorded from Axial’s north rift zone, and unusual temperature increases began to be recorded at several of the OOI monitoring instruments in the summit caldera. Both of these were seen as a “smoking gun” for an eruption, but exactly what was causing them was unclear. More conclusive evidence for an eruption was collected just a few weeks ago by our colleagues at University of Washington. During an expedition to Axial Seamount to do maintenance work on the OOI Cabled Array, they were able to remap the summit and north rift zone with multibeam sonar, which revealed depth changes up to 127 m (417 feet), and a short ROV dive on one of these areas confirmed that they were due to thick new lava flows. Since then, more detailed analysis of the new bathymetry and comparison to previous surveys by colleagues at the Monterey Bay Aquarium Research Institute (MBARI) has revealed additional thinner lava flows, both on the NE caldera floor and on the northern caldera rim. There may also be other thin lava flows that are still undetected that we may find on this expedition.

On this cruise, we’ll be exploring and sampling the new lava flows in more detail. We plan to collect high-resolution bathymetry over the eruption sites with the AUV Sentry to better understand how the lava was emplaced. We’ll make dives with ROV Jason to collect samples of the new lava that will be analyzed later for precise dating and chemical analysis. Since the lava flows are probably still warm and cooling, we expect to find new hydrothermal vents to sample. These could include “snowblower vents” that have such high densities of microbes that they look like snow coming out of the seafloor. We’ll be looking for evidence of explosive activity during the eruption, which would leave small particles of ash on the surface of the new lavas. In short, we still have lots of questions about what happened during the eruption. We’re a bit like detectives trying solving a mystery by looking for clues that will help us better understand what happened. It’s fun and that’s what science is all about!

Photos and video courtesy of Axial 2015 Team.

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A Cooperative Program

The Axial Seamount Eruption Response is a program of the National Oceanic and Atmospheric Administration and the National Science Foundation in cooperation with Oregon State University, Hatfield Marine Science Center, the Oceanscape Network and others.

How Is Axial Seamount A "Wired Volcano?"

Download this schmatic to better understand how scientists have used a sophisticated underwater monitoring system to "watch" the volcano. Can you find the home of the Oceanscape Network on this map, too?

Do You Have Questions?

During the duration of this expedition, the science team will answer your questions. Return to the main Axial Seamount Eruption Response page to find the online form for this activity.