We tend to picture glaciers as slow rivers of frozen water, but the Byrd Glacier in Antarctica drains an area larger than California through a gap in the Transantarctic Mountains at up to 800 metres a year, dragging enough ice to raise global sea level measurably if it ever fully released
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Byrd Glacier drains an East Antarctic catchment larger than California through a 24-kilometre gap in the Transantarctic Mountains, moving at up to 800 metres a year — and its behaviour is set by a bedrock trough carved before the dinosaurs.
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