According to new research published in the journal Science, subglacial sediments beneath Whillans Ice Stream in West Antarctica are saturated with a mixture of ancient seawater and freshwater from a glacier; this groundwater, extending downward for more than 1 km, contains more than 10 times as much volume as the shallow hydrologic system above and actively exchanges with it. Survey locations on the Whillans Ice Stream in West Antarctica: electromagnetic...
