Antarctic Orca Submarine Volcano Blasted by Swarm of 85,000 Earthquakes


Carlini Base on King George Island, Antarctica

The Carlini base on King George Island, hosting the seismometer located closest to the seismic region, and the Bransfield Strait. Credit: Milton Percy Plasencia Linares

In a remote area, a mix of geophysical methods identifies magma transfer below the seafloor as the cause.

Even off the coast of Antarctica, volcanoes can be found. A sequence of more than 85,000 earthquakes was recorded in 2020 at the deep-sea volcano Orca, which has been inactive for a long time, a swarm quake that reached proportions not previously observed for this region. The fact that such events can be studied and described in remarkable detail even in such remote, and therefore poorly instrumented areas, is now shown by the study of an international team published in the journal Communications Earth and Environment.

Researchers from Germany, Italy, Poland, and the United States were involved in the study, which was led by Simone Cesca of the German Research Centre for Geosciences (GFZ) Potsdam. They were able to combine seismological, geodetic, and remote sensing techniques to determine how the rapid transfer of magma from the Earth’s mantle near the crust-mantle boundary to almost the surface caused the swarm quake.

The Orca volcano between the tip of South America and Antarctica

Swarm quakes mainly occur in volcanically active regions. The movement of fluids in the Earth’s crust is therefore suspected as the cause. Orca seamount is a large submarine shield volcano with a height of about 900 meters above the seafloor and a base diameter of about 11 kilometers. It is located in the Bransfield Strait, an ocean channel between the Antarctic Peninsula and the South Shetland Islands, southwest of the southern tip of Argentina.

Seismically Active Zone off Antactica

Illustration of the seismically active zone off Antactica. Credit: Cesca et al. 2022; nature Commun Earth Environ 3, 89 (2022); doi.org/10.1038/s43247-022-00418-5 (CC BY 4.0)

“In the past, seismicity in this region was moderate. However, in August 2020, an intense seismic swarm began there, with more than 85,000 earthquakes within half a year. It represents the largest seismic unrest ever recorded there,” reports Simone Cesca, a scientist in GFZ’s Section 2.1 Earthquake and Volcano Physics and lead author of the now published study. At the same time as the swarm, a lateral ground displacement of more than ten centimeters and a small uplift of about one centimeter was recorded on neighboring King George Island.

Challenges of research in a remote area

Cesca studied these events with colleagues from the National Institute of Oceanography and Applied Geophysics — OGS and the University of Bologna (Italy), the Polish Academy of Sciences, Leibniz University Hannover, the German Aerospace Centre (DLR) and the University of Potsdam. The challenge was that there are few conventional seismological instruments in the remote area, namely only two seismic and two GNSS stations (ground stations of the Global Navigation Satellite System which measure ground displacement). In order to reconstruct the chronology and development of the unrest and to determine its cause, the team therefore additionally analyzed data from farther seismic stations and data from InSAR…



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