
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.
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.