Underwater Antarctic volcano triggers 85,000 earthquakes

Along-dormant underwater volcano near Antarctica has woken up, triggering a swarm of 85,000 earthquakes. The swarm, which began in August 2020 and subsided by November of that year, is the strongest earthquake activity ever recorded in the region. The quakes were likely caused by a ‘finger’ of hot magma poking into the crust, according to recent research. “There have been similar intrusions in other places on Earth, but this is the first time we have observed it there,” said Simone Cesca, a seismologist at the GFZ German Research Centre for Geosciences in Potsdam. “Normally, these processes occur over geologic time scales” as opposed to over the course of a human life span.

The swarm occurred around the Orca Seamount, an inactive volcano that rises 900 metres from the seafloor in the Bransfield Strait, a narrow passage between the South Shetland Islands and the northwestern tip of Antarctica. In this region, the Phoenix tectonic plate is diving beneath the continental Antarctic plate, creating a network of fault zones, stretching some portions of the crust and opening rifts in other places. Scientists at the research stations on King George Island, one of the South Shetland Islands, were the first to feel the rumblings of small quakes. The team wanted to understand what was going on, but King George Island is remote, with just two seismic stations nearby.

Researchers used data from those seismic stations, as well as data from two ground stations for the global satellite navigation system, to measure ground displacement. They also looked at data from more far-flung seismic stations and from satellites circling Earth that use radar to measure shifting at ground level. The nearby stations are rather simple, but they were good for detecting the tiniest quakes. By piecing these data together, the team was able to create a picture of the underlying geology that triggered this massive earthquake swarm.

The two largest earthquakes in the series were a magnitude 5.9 quake in October 2020 and a magnitude 6.0 quake in November. After the November quake, seismic activity waned.

The quakes seemed to move the ground on

King George Island around 11 centimetres. Only four per cent of that displacement could be directly explained by the tremor; the scientists suspect the movement of magma into the crust largely accounts for the ground shift. “We think the magnitude 6.0 created some fractures and reduced the pressure of the magma dike,” Cesca said. If there was an underwater eruption at the seamount, it likely happened at that time. But as of yet, there is no direct evidence for an eruption; to confirm that the massive shield volcano blew its top, scientists would have to send a mission to the strait to measure the bathymetry, or seafloor depth, and compare it to historical maps.