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Here's what to know about Maunaloa, the largest active volcano in the world

FILE - A gaseous cloud rises from the crater of Maunaloa, center, on the Big Island, April 4, 1984. (AP Photo/John Swart, File)
John Swart/AP
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AP
FILE - A gaseous cloud rises from the crater of Maunaloa, center, on the Big Island, April 4, 1984. (AP Photo/John Swart, File)

The ground is shaking and swelling at Maunaloa, the largest active volcano in the world, indicating that it could erupt. Scientists say they don't expect that to happen right away but officials on the Big Island are telling residents to be prepared in case it does erupt soon.

Here are some things to know about the volcano.

Where is Maunaloa?

It is one of five volcanoes that together make up the Big Island. It's not the tallest (that title goes to Maunakea) but it's the largest and makes up about half of the island's land mass.

It sits immediately north of Kīlauea volcano, which is currently erupting from its summit crater. Kīlauea is well-known for a 2018 eruption that destroyed 700 homes and sent rivers of lava spreading across farms and into the ocean.

FILE - Lava flows downhill from the crater of Maunaloa, April 5, 1984, on the island of Hawaiʻi. (AP Photo/John Swart, File)
John Swart/AP
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AP
FILE - Lava flows downhill from the crater of Maunaloa, April 5, 1984, on the island of Hawaiʻi. (AP Photo/John Swart, File)

Maunaloa last erupted 38 years ago in 1984. In written history, dating to 1843, it's erupted 33 times.

The Big Island is mostly rural and is home to cattle ranches, coffee farms and beach resorts. It's about 200 miles south of Oʻahu.

Will Maunaloa erupt like Kīlauea?

Maunaloa's eruptions differ from Kīlauea's in part because it is taller. Its greater height gives it steeper slopes, which allow lava to rush down its hillsides faster than Kīlauea's.

Its enormous size may allow it to store more magma, leading to larger lava flows when an eruption occurs.

Frank Trusdell, research geologist at the Hawaiian Volcano Observatory, which is part of the U.S. Geological Survey, said data indicates that Maunaloa has a much larger magma reservoir than Kīlauea, which may allow it to hold more lava and rest longer between eruptions than Kīlauea.

"I would say that right now the signs are pointing to the influx of magma into the volcano. Maunaloa is not a dead volcano. The recent seismicity is reflective of the ingress of magma into the reservoir," Trusdell told HPR. "We're looking at a reawakening of Maunaloa, although an eruption is not imminent."

When asked whether he would be more surprised if Maunaloa erupted this year or if it went another two decades without erupting, Trusdell said "either scenario could be equally likely at this point in time."

Where will Maunaloa erupt from?

Scientists won't know until the eruption begins. Each eruption since 1843 started at the summit. Half the time, the volcano later also began erupting from vents at lower elevations. The other half of the time it only erupted in the summit caldera.

USGS

Scientists can't tell far in advance when and where Maunaloa will open new vents and erupt.

Vents generally form along the volcano's rift zone. That's where the mountain is splitting apart, the rock is cracked and relatively weak and it's easier for magma to emerge.

An eruption from vents on the southwest rift zone could hit residential communities, coffee farms or coastal villages on the west side of the island. Lava could reach homes in just hours or days.

The west side's most populous town would be protected from any Maunaloa eruption by the presence of another active volcano. The broad flanks of that volcano, Hualālai, sit between Maunaloa's southwest rift zone and Kailua-Kona and would block any lava heading toward the coastal community.

An eruption from the northeast rift zone could send lava toward the county seat of Hilo or other towns in East Hawaiʻi. It could take lava weeks or months to reach populated areas on this side of the mountain.

FILE - Molten rock flows from Maunaloa on March 28, 1984, near Hilo, Hawaiʻi. (AP Photo/Ken Love, File)
Ken Love/AP
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AP
FILE - Molten rock flows from Maunaloa on March 28, 1984, near Hilo, Hawaiʻi. (AP Photo/Ken Love, File)

Scott Rowland, a geologist at the University of Hawaiʻi at Mānoa, said there's no pattern when it comes to where an eruption will occur.

“Just because the last one was on the northeast rift zone does not mean the next one will be down the southwest rift zone,” he said.

Will Maunaloa explode like Mount St. Helens?

Fifty-seven people died when Washington state's Mount St. Helens erupted in 1980 and blasted more than 1,300 feet (400 meters) off the top of the mountain. Steam, rocks and volcanic gas burst upward and outward. A plume of volcanic ash rose over 80,000 feet (24,384 meters) and rained down as far as 250 miles (400 kilometers) away.

Hawaiʻi volcanoes like Maunaloa tend not to have explosion eruptions like this.

That's because their magma is hotter, drier and more fluid, said Hannah Dietterich, a research geophysicist at the U.S. Geological Survey's Alaska Volcano Observatory.

The magma in Mount St. Helens tends to be stickier and traps more gas, making it much more likely to explode when it rises.

The gas in the magma of Hawaiʻi’s volcanoes tends to escape, and so lava flows down the side of their mountains when they erupt.

Hawaiʻi's volcanoes are called shield volcanoes because successive lava flows over hundreds of thousands of years build broad mountains that resemble the shape of a warrior's shield.

Shield volcanos are also found in California and Idaho as well as Iceland and the Galapagos Islands. Alaska's Wrangell-St. Elias National Park has eight shield volcanoes including Mount Wrangell.

Volcanoes like Mount St. Helens are called composite or stratovolcanoes. Their steep, conical slopes are built by the eruption of viscous lava flows and rock, ash and gas. Japan's Mount Fuji is another example of a composite volcano.

From left, Civil Defense Administrator Talmadge Magno, translator Carrie Kaufmann, and Ken Hon, Hawaiian Volcano Observatory scientist-in-charge, speak to a crowd about the potential threat of a Maunaloa eruption at the local gymnasium in Pahala, Hawaiʻi, on Oct. 27, 2022. (AP Photo/Megan Moseley)
Megan Moseley/AP
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FR171936 AP
From left, Civil Defense Administrator Talmadge Magno, translator Carrie Kaufmann, and Ken Hon, Hawaiian Volcano Observatory scientist-in-charge, speak to a crowd about the potential threat of a Maunaloa eruption at the local gymnasium in Pahala, Hawaiʻi, on Oct. 27, 2022. (AP Photo/Megan Moseley)

How do scientists monitor Maunaloa?

The Hawaiian Volcano Observatory has more than 60 GPS stations on Maunaloa taking measurements to estimate the location and the amount of magma accumulating beneath the surface.

Scientists use tiltmeters to track long-term changes in the tilting of the ground, helping them identify when the ground is swelling or deflating. A rapid change in tilt can indicate when an eruption will occur.

There's also a thermal webcam at Maunaloa's summit that will identify the presence of heat. And satellite radar can keep track of ground swelling and deflation.

For Hawaiʻi Island residents, lava inundation maps are available to show how your specific community might be affected. Find them below or on the HVO's website.

"They can identify upslope, what segment will impact them. So if there's an eruption and the flow has happened to go into that geographic sector where people live, then they know based on their own research, that they could be impacted. And hopefully, they will have made some preparation," Trusdell said.

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