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Scientists have just mapped the volcanic lower region of Hawaii in amazing detail

Scientists have just mapped the volcanic lower region of Hawaii in amazing detail

 


“We were terrified,” says John Wilding, a graduate researcher at Caltech and lead author of a new study describing geological features in science. “Nobody has ever directly observed magma activity of this magnitude before.”

The researchers used machine learning algorithms to search for earthquakes in seismic data from the network of sensors at the Hawaii Volcano Observatory, picking out tremors so small that previous methods missed. The result is a stunningly detailed picture of Hawaii’s fiery underworld, which promises to help scientists sort out the geological processes that drive the island’s volcanism.

“This is potentially the future for volcanoscience,” says Matt Burgess, a former Hawaiian seismologist who has studied deep earthquakes below Pahala.

A mysterious rumble from the depths

The Pahala earthquake swarm has been roaring since at least 1970. Earthquakes occur in the mantle, the layer of our planet between the crust and core, and most are too small and deep to move the surface with much force. Instead, the tremor feels more like the rolling or swaying of the ground. Sometimes, Ka’u Coffee’s Daniele realizes something isn’t right because ripples appear on the surface of his coffee. But in recent years, the rattles under Pahala have become relentless.

“The seismic activity has been continuing to rise,” says Ninfa Pennington, a volcanic seismologist at the USGS Volcano Observatory in Hawaii, who has been tracking the recent spike in activity.

Pahala is believed to sit atop a scorching rock column, called a hotspot, that built the Hawaiian Islands. As the Pacific Plate moves across the stationary hotspot, new volcanoes – and eventually new islands – are born. The 15 volcanoes of the Hawaiian Islands are the youngest in a chain of more than 129 created by the hotspot, most of which have gone silent and are now hidden beneath the waves.

Previous studies have identified potential sources of magma below the earthquake swarm and suggested that an upward pulse of magma could be driving the deep crackles. Other studies have detailed shallow volcanic plumbing. But exactly how molten rock flows out from the depths of the mantle is unknown.

“We’re basically missing out on this big hunk,” says Pennington.

The earthquake swarm had an opportunity to get a closer look at the fiery bottom of the island. While earthquakes can come from many sources, magma or fluids moving through cracks generates the telltale seismic rumble. As the molten rock shifts, it can pressurize nearby ground, causing it to crack and shift, which the scientists can also detect in the earthquake data.

By plotting all of these earthquakes in three dimensions—a bit like a geologic raster—scientists have now mapped a network of subterranean structures where magma might flow toward the surface, charging volcanic eruptions.

Seismic treasure trove

Amid increased earthquake activity in Hawaii, Wilding joined geophysicist Zachary Ross’s research group at Caltech. Ross has been developing methods for detecting earthquakes using machine learning algorithms, which can pick up surprisingly small earthquakes and give stunning spider-web views of fault zones underground.

The team applied these methods to 3.5 years of seismic data in Hawaii, recorded between 2019 and 2022. The system identified nearly 200,000 earthquakes from the swarm, illuminating sill structures stacked in the upper mantle. Even the extreme detail has allowed scientists to track magma as it flows into a sill, triggering a series of earthquakes.

When Ross first saw the details of geological structures on a computer screen, he was dumbfounded. “He was kind of like, ‘Oh my God, what are we looking at here?'” He says. “It’s just shocking.”

He describes the thresholds complex as a “gateway to the system,” providing a means for moving magma horizontally away from the region below Pahala. These underground features do not contain empty space, and instead represent a weak area in the rock where magma has intruded and spread out as a molten plate. The complex is associated with an area of ​​fractures leading to Kilauea as well as an area the team believes is associated with Mauna Loa.

There may be more than one path that the molten rock follows to the surface, Ross says. The sills are expected to be part of a broader layer of sub-island structures transporting magma to the various volcanic peaks.

Sources

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2/ https://www.nationalgeographic.co.uk/science-and-technology/2022/12/scientists-just-mapped-hawaiis-volcanic-underbelly-in-stunning-detail

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