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Active Volcano Discovered Underneath Antarctic

Active Volcano Discovered Underneath Antarctic Ice Sheet, Confirming Long-Held Suspicions

Posted: 11/18/2013 10:26 am EST  |  Updated: 11/18/2013 2:52 pm EST

 
Volcano Under Antarctica

By Becky Oskin, LiveScience Staff Writer:

Earthquakes deep below West Antarctica reveal an active volcano hidden beneath the massive ice sheet, researchers said today (Nov. 17) in a study published in the journal Nature Geoscience.

The discovery finally confirms long-held suspicions of volcanic activity concealed by the vast West Antarctic Ice Sheet. Several volcanoes poke up along the Antarctic coast and its offshore islands, such as Mount Erebus, but this is the first time anyone has caught magma in action far from the coast.

“This is really the golden age of discovery of the Antarctic continent,” said Richard Aster, a co-author of the study and a seismologist at Colorado State University. “I think there’s no question that there are more volcanic surprises beneath the ice.”

The volcano was a lucky find. The research project, called POLENET, was intended to reveal the structure of Earth’s mantle, the layer beneath the crust. In 2010, a team led by scientists from Washington University in St. Louis spent weeks slogging across the snow, pulling sleds laden with earthquake-monitoring equipment. [Images: Trek Across Antarctica]

Right place, right time

Two earthquake swarms struck beneath the researchers’ feet in January 2010 and March 2011, near the Executive Committee Range in the Marie Byrd Land region of the continent. As the researchers later discovered, the tremors — called deep, long-period earthquakes (DLPs) — were nearly identical to DLPs detected under active volcanoes in Alaska and Washington. The swarms were 15 to 25 miles (25 to 40 kilometers) below the surface.

“It’s an exciting story,” said Amanda Lough, the study’s lead author and a graduate student in seismology at Washington University in St. Louis. Though there were no signs of a blast, a 3,200-foot-tall (1,000 meters) bulge under the ice suggests the volcano had blasted out lava in the past, forming a budding peak.

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The POLENET/ANET field team drags equipment to install remote seismic and GPS stations at Mount Sidley, a volcano in Antarctica (seen in background).

“We can say with pretty high confidence that there wasn’t an eruption while we were out there,” Lough told LiveScience’s OurAmazingPlanet. “We had people installing [seismometer] stations and flying airborne radar over the ice. But from the bed topography, we can see there is something building up beneath the ice.”

Scientists think that underground magma and fluids pushing open new paths and fracturing rock cause deep, long-period earthquakes. Many active volcanoes in Alaska’s Aleutian Islands have frequently produced these deep earthquake swarms without any signs of impending eruptions. However, researchers also monitor the tremors because a sudden uptick in shaking was seen before eruptions at Mount Spurr and Mount Redoubt in Alaska.

A volcanic flood

If the volcano in Antarctica did erupt, it would melt the bottom of the ice sheet immediately above the vent. Scientists aren’t sure what would happen next. In Iceland, volcanic eruptions can melt glaciers, causing massive floods calledjökulhlaups. But the ice above the Antarctic volcano is more than a half-mile (1 km) thick.

“How West Antarctic ice streams would react to an eruption a hundred or more kilometers [60 miles] inland from the grounding line is a yet-to-be-answered question,” said Stefan Vogel, a glaciologist with Australian Antarctic Division who was not involved in the study. The grounding line is the spot where glaciers detach from rock and float on water.

“There is certainly a need for more research, both in mapping the distribution and monitoring the activity level of subglacial volcanic activity beneath ice sheets, as well as studying the impact of subglacial volcanic activity on the hydrological system of glaciers and ice sheets,” Vogel said in an email interview.

It would take a super-eruption in the style of Yellowstone’s ancient blowouts to completely melt the ice above the active volcano, Lough and her co-authors calculated. And if the volcano under the ice is similar to ones close by, such as Mount Sidley, there’s no risk of a super-eruption. [Big Blasts: History’s 10 Most Destructive Volcanoes]

Instead, the millions of gallons of meltwater might simply hasten the flow of the nearby MacAyeal Ice Stream toward the sea.

“People hear the word ‘volcano’ and get caught up in the idea that it will change the way the ice sheet works, but this stuff has been going on underneath the ice [for millions of years], and the ice sheet is in balance with it,” Lough said. “Everyday magmatism isn’t enough to cause major problems.”

Hugh Corr, a glaciologist at the British Antarctic Survey who also discovered a buried Antarctic volcano, said an eruption could have a big effect, but it’s difficult to quantify.

“The biggest effect on the West Antarctic Ice Sheet is still climate change — warming the ocean, melting the ice shelves. That’s the most immediate risk, compared to if a volcano might go off,” said Corr, who was not involved in the study.

A geologic puzzle

Signs of active and extinct volcanoes pop up all over Antarctica. Ash layers and lava indicate volcanoes spouted while the continent froze during the past 20 million years or more. (An 8,000-year-old ash layer sits above the newly found volcano, but it comes from Mount Waesche, a nearby peak.)

“The [West] coast of Antarctica is like a ring of fire,” Corr said.

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The Executive Committee Range in West Antarctica is home to a newly discovered active volcano.

The earthquake swarms line up with older volcanoes in the Executive Committee Range, suggesting the volcanic activity there is slowly migrating south by 6 miles (9.6 km) every million years. This migration is perpendicular to the motion of Antarctica’s tectonic plate, so a hotspot or mantle plume is not feeding the volcanoes, Lough said. (A mantle plume should make volcanoes that line up parallel to plate motion, like those of the Hawaiian Islands.)

The big mystery is figuring out why the volcano and its forerunners even exist. “Antarctica is certainly one of the most fascinating and enigmatic of all of Earth’s continents,” Aster said. [Video – Antarctica: Solving Geologic Mysteries]

Let’s set the scene. Antarctica is split by an incredible mountain range. Imagine if Utah’s spectacularly steep Wasatch Mountains cleaved North America from Texas all the way to Canada. That’s what the Transantarctic Mountains are like. In the West, the land dives off into a deep rift valley, where the crust has been tearing apart for about 100 million years. The newly found volcano sits on the other side of this rift, in a higher-elevation region called Marie Byrd Land.

While the torn crust may seem like the best explanation for Antarctica’s many volcanoes, many of the peaks fit no obvious pattern. Rifting and volcanism in Antarctica could be like nowhere else on Earth. “What is going on with the crust in Antarctica is still puzzling,” Lough said.

Email Becky Oskin or follow her @beckyoskin. Follow us @OAPlanetFacebook &Google+Original article on LiveScience’s OurAmazingPlanet.

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Tamu Massif, Earth’s Largest Volcano, Lurks Beneath Pacific Ocean

Tamu Massif, Earth’s Largest Volcano, Lurks Beneath Pacific Ocean

Posted: 09/06/2013 8:34 am EDT  |  Updated: 09/06/2013 10:28 am EDT

The world’s largest volcano lurks beneath the Pacific Ocean, researchers announced today (Sept. 5) in the journal Nature Geoscience.

Called the Tamu Massif, the enormous mound dwarfs the previous record holder, Hawaii’s Mauna Loa, and is only 25 percent smaller than Olympus Mons on Mars, the biggest volcano in Earth’s solar system, said William Sager, lead study author and a geologist at the University of Houston.

“We think this is a class of volcano that hasn’t been recognized before,” Sager said. “The slopes are very shallow. If you were standing on this thing, you would have a difficult time telling which way was downhill.”

Tamu is 400 miles (650 kilometers) wide but only about 2.5 miles (4 km) tall. It erupted for a few million years during the early Cretaceous period, about 144 million years ago, and has been extinct since then, the researchers report. [50 Amazing Volcano Facts]

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A 3D map of Tamu Massif, the world’s biggest volcano. (Click image for larger version.)

Explaining ocean plateaus

Like other massive volcanoes, Tamu Massif seems to have a central cone that spewed lava down its broad, gentle slopes. The evidence comes from seismic surveys and lava samples painstakingly collected over several years of surveys by research ships. The seismic waves show lava flows dipping away from the summit of the volcano. There appears to be a series of calderas at the summit, similar in shape to the elongated and merged craters atop Mauna Loa, Sager said.

Until now, geologists thought Tamu Massif was simply part of an oceanic plateau called Shatsky Rise in the northwest Pacific Ocean. Oceanic plateaus are massive piles of lava whose origins are still a matter of active scientific debate. Some researchers think plumes of magma from deep in the mantle punch through the crust, flooding the surface with lava. Others suggest pre-existing weaknesses in the crust, such as tectonic-plate boundaries, provide passageways for magma from the mantle, the layer beneath the crust. Shatsky Rise formed atop a triple junction, where three plates pulled apart.

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Tamu Massif on Shatsky Rise in the northwest Pacific Ocean, compared in size to Olympus Mons on Mars. (Click image for larger version.)

Tamu Massif’s new status as a single volcano could help constrain models of how oceanic plateaus form, Sager said. “For anyone who wants to explain oceanic plateaus, we have new constraints,” he told LiveScience. “They have to be able to explain this volcano forming in one spot and deliver this kind of magma supply in a short time.”

Geochemist David Peate of the University of Iowa, who was not involved in the study, said he looks forward to new models explaining the pulses of magma that built Shatsky Rise. Tamu Massif is the biggest and oldest volcano, and the cones grow smaller and younger to the northeast of Tamu. Sager and his colleagues suggest that pulses of magma created the volcanic trail.

“It seems that in many oceanic plateaus the melting is continuous, but here you have a big shield volcano,” Peate told LiveScience. “Understanding the source of the volume of that magma, the rate of production of the magma and the time interval between those pulses will help give better constraints to feed into those models,” he said.

Sager said other, bigger volcanoes could be awaiting discovery at other oceanic plateaus, such as Ontong Java Plateau, located north of the Solomon Islands in the southwest Pacific Ocean. “Structures that are under the ocean are really hard to study,” he said.

Floating volcano

Oceanic plateaus are the biggest piles of lava on Earth. The outpourings have been linked to mass extinctions and climate change. The volume of Tamu Massif alone is about 600,000 cubic miles (2.5 million cubic km). The entire volcano is bigger than the British Isles or New Mexico.

Despite Tamu’s huge size, the ship surveys showed little evidence the volcano’s top ever poked above the sea. The world’s biggest volcano has been hidden because it sits on thin oceanic crust (or lithosphere), which can’t support its weight. Its top is about 6,500 feet (1,980 meters) below the ocean surface today.

“In the case of Shatsky Rise, it formed on virtually zero thickness lithosphere, so it’s in isostatic balance,” Sager said. “It’s basically floating all the time, so the bulk of Tamu Massif is down in the mantle. The Hawaiian volcanoes erupted onto thick lithosphere, so it’s like they have a raft to hold on to. They get up on top and push it down. And with Olympus Mons, it’s like it formed on a two-by-four.”

Sager and his colleagues have studied Shatsky Rise for decades, seeking to solve the puzzle of oceanic plateaus. About 20 years ago, they named Tamu Massif after Texas A&M University, Sager’s former employer, he said.

Email Becky Oskin or follow her @beckyoskin. Follow us @OAPlanetFacebook &Google+. Original article on LiveScience’s OurAmazingPlanet.

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