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In the last major glacial epoch, or 'Ice Age', there have been small-scale climate shifts in the Earth's landmass and a recent study assumes that the bedrock below the world's southernmost continent - Antarctica - has been rebounding since.

United statesMatt kingAustralian centre for excellenceUniversity of tasmaniaAmerican geophysical unionIce ageAntarctic scienceProfessor mattCaptures imageMassive seven storyMonster waveMysterious east antarcticaOving mysteryIcy continent