Researchers have confirmed a subglacial river system channeling water more than 1,500 feet beneath the Antarctic ice sheet, where episodic surges flush into the ocean cavity under the Ross Ice Shelf.
Craig Stevens receives funding from the NZ Ministry for Business, Innovation and Employment and its Strategic Science Investment Fund, and the Antarctica New Zealand Antarctic Science Platform. He is ...
Deep beneath Antarctica’s ice, scientists have uncovered a geological archive that could reshape predictions of future ...