By Sarah Sloat
on
East Antarctica is the coldest place on Earth.
It is permanently covered in ice; there are no trees or shrubs, just
bits of lichens, moss, and clinging algae. The idea that humans may not
want to kick it there — or even think about it — is pardonable. But by
avoiding the Earth’s icebox, a team of researchers argue a new Nature Geoscience paper, we’ve also ignored the massive continent’s terrifying geology: The frozen wasteland, they write, has earthquakes — and lots of them.
Until recently, they explain in their paper,
the geologic structure and tectonic activity of East Antartica were
relatively unknown. The first earthquake there was recorded in 1982, and
only eight earthquakes have been reported since. Scientists had
accepted the theory that East Antarctica just didn’t really experience
earthquakes because its seismic activity was suppressed by the weight of
the region’s thick ice. But that assumption, lead author and Drexel
University professor Amanda Lough, Ph.D., explains to Inverse, isn’t true.
“East Antarctica shows comparable levels of seismicity as other stable
cratons,” she says, referring to the geological term for the chunk of
the Earth’s crust that makes up a continent’s backbone. “So at least for
the East Antarctic Ice Sheet, the presence of a several-kilometer-thick
ice sheet is not suppressing seismicity.”



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