No two volcanic eruptions are exactly alike, but scientists think a series of explosive eruptions at Kฤซlauea volcano fit into a whole new category.

By analyzing the dynamics of 12 back-to-back explosions that happened in 2018, researchers describe a new type of volcanic eruption mechanism. The explosions were driven by sudden pressure increases as the ground collapsed, which blasted plumes of rock fragments and hot gas into the air, much like a classic stomp-rocket toy.

Researchers from the University of Oregon, United States Geological Survey and Chinaโ€™s Sichuan University report their findings in a paper published May 27 in Nature Geoscience.



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The particular string of explosions at the summit of Kฤซlauea was part of a sequence of events that included lava flows erupting from lower on the flank of the volcano. Those lava flows destroyed thousands of homes and displaced residents on the Island of Hawaiโ€™i for months.

Understanding exactly what happened in past volcanic eruptions, colloquially called โ€œhindcasting,โ€ allows volcanologists to make better forecasts about future eruptions and give more accurate warnings to people in an eruptionโ€™s path.

For the most part, explosive volcanic eruptions are either primarily driven by rising magma, vaporized groundwater, or some combination of the two, according to Josh Crozier, who did this research as a doctoral student at the UO. But these eruptions didnโ€™t quite fit the mold.


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โ€œThese eruptions are quite interesting in that they donโ€™t really seem to involve either of those,โ€ Crozier said. โ€œThe eruptive material contained very little that looked like fresh magma that was blasted out, but thereโ€™s no evidence for significant groundwater being involved, either.โ€

The Hawaiian Volcano Observatory, part of the U.S. Geological Survey, keeps close tabs on Kฤซlauea. The volcano is covered with scientific instruments, from ground sensors that measure the shaking of the earth to tools that analyze the gases released from the volcano.

โ€œA cool thing about these eruptions is that there were a bunch of them in sequence that were remarkably similar; thatโ€™s relatively unusual,โ€ said Leif Karlstrom, a volcanologist at the UO. โ€œTypically, volcanic eruptions donโ€™t happen with as much regularity.โ€

So the team had more data than usual to work with, and they could dig deeper into the specific dynamics of the eruptions.

Putting all that data into a variety of atmospheric and subsurface models, the scientists pieced together a new story about what happened on Kฤซlauea during the string of events in 2018.

Before each explosion at the summit, magma was slowly draining from an underground reservoir. (This magma was feeding lava flows 40 kilometers away, on the eastern flank of the volcano.) As the reservoir depleted, the ground above it โ€” the crater within the caldera at the volcanoโ€™s summit โ€” suddenly collapsed.

That quickly increased the pressure in the reservoir. And because there was a pocket of accumulated magmatic gas sitting at the top of this reservoir, the pressure increase squeezed the magmatic gas and bits of rubble through a conduit and blasted them out of a vent in Kฤซlaueaโ€™s crater.

The researchers compare the eruption dynamic to a stomp-rocket toy, where stepping on an air bag connected to a hose launches a projectile into the air.

โ€œThe โ€˜stompโ€™ is this whole kilometer-thick chunk of rock dropping down, pressurizing the pocket, and then forcing material directly up,โ€ Crozier said. And the โ€˜rocketโ€™ is, of course, the gas and rocks erupting from the volcano.

Caldera collapse is fairly common, Crozier notes. So while this is the first time scientists have specifically spelled out this specific stomp-rocket mechanism, itโ€™s probably not the only time itโ€™s occurred.

The study was able to link geophysical observations to the properties of the volcanic plume in the atmosphere.

โ€œThis link is very rare,โ€ said Joe Dufek, a volcanologist at the UO. โ€œIt points to new ways for us to observe eruptions and to combine sensor measurements with computer simulations to better assess hazards from eruptions.โ€

The fact that this was a series of smaller eruptions may have made it easier to see the underlying mechanism, Dufek said. Other complex processes werenโ€™t overshadowing the stomp-rocket component.

But thatโ€™s not to say that Kฤซlauea is simple. A typical textbook drawing of a volcano shows magma moving upwards through chambers at different depths. But itโ€™s rarely that straightforward, and a volcano like Kฤซlauea, decked out in scientific instruments, provides an opportunity to dig into the details.  

โ€œThis is an example, and thereโ€™s an increasing number of these, where the pathways of magma ascent are quite geometrically complex,โ€ Karlstrom said. โ€œIt gives us a much more nuanced picture of what volcanic plumbing systems look like.โ€


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