It's
like a detective mystery with an explosive climax. Scientists
investigating the Antarctica ice sheet for something else came across a
series of unexplained clues that finally led to the discovery of a brand
new volcano emerging from under a kilometer of ice, according to a Washington University statement.
The discovery of the as yet unnamed volcano was announced in the November 17 online issue of Nature Geoscience.
It all started back in January 2010 when a team of scientists set up two crossing lines of seismographs - instruments that measure vibrations in the Earth's surface, like when an earthquake occurs - across Marie Byrd Land in West Antarctica. The instruments used disturbances created by distant earthquakes to make images of the ice and rock deep within West Antarctica.
The goal, says Doug Wiens, professor of earth and planetary science at Washington University in St. Louis and one of the project's principle investigators, was to weigh the ice sheet to help reconstruct Antarctica's climate history, the statement said. But to do this accurately the scientists had to know how the earth's mantle would respond to an ice burden, and that depended on whether it was hot and fluid or cool and viscous. The seismic data would allow them to map the mantle's properties.
In the meantime, automated-event-detection software was put to work to comb the data for anything unusual. When it found two bursts of seismic events between January 2010 and March 2011, Wiens' PhD student Amanda Lough looked more closely to see what was rattling the continent's bones. Was it rock grinding on rock, ice groaning over ice, or, perhaps, hot gases and liquid rock forcing their way through cracks in a volcanic complex?
The discovery of the as yet unnamed volcano was announced in the November 17 online issue of Nature Geoscience.
It all started back in January 2010 when a team of scientists set up two crossing lines of seismographs - instruments that measure vibrations in the Earth's surface, like when an earthquake occurs - across Marie Byrd Land in West Antarctica. The instruments used disturbances created by distant earthquakes to make images of the ice and rock deep within West Antarctica.
The goal, says Doug Wiens, professor of earth and planetary science at Washington University in St. Louis and one of the project's principle investigators, was to weigh the ice sheet to help reconstruct Antarctica's climate history, the statement said. But to do this accurately the scientists had to know how the earth's mantle would respond to an ice burden, and that depended on whether it was hot and fluid or cool and viscous. The seismic data would allow them to map the mantle's properties.
In the meantime, automated-event-detection software was put to work to comb the data for anything unusual. When it found two bursts of seismic events between January 2010 and March 2011, Wiens' PhD student Amanda Lough looked more closely to see what was rattling the continent's bones. Was it rock grinding on rock, ice groaning over ice, or, perhaps, hot gases and liquid rock forcing their way through cracks in a volcanic complex?